Pole star project/Equatorials
The equatorials are a collection of land masses currently or formerly above sea level that may contain archaeological artifacts differentiating between here on Earth versus in heaven at or near the North Pole star.
- 1 Togo
- 2 Benin
- 3 Annobón
- 4 Ilhéu das Rolas
- 5 São Tomé
- 6 Príncipe
- 7 Bioko
- 8 Corisco
- 9 Equatorial Guinea
- 10 Cameroon
- 11 Gabon
- 12 Republic of the Congo
- 13 Democratic Republic of the Congo
- 14 Idjwi
- 15 Uganda
- 16 Ssese Islands
- 17 Bugala
- 18 Ukerewe
- 19 Tanzania
- 20 Kenya
- 21 Zanzibar
- 22 Somalia
- 23 Maldives
- 24 Alifushi
- 25 Simeulue
- 26 Nias
- 27 Pini
- 28 Sumatera Island
- 29 Singapore
- 30 Christmas Island
- 31 Matak
- 32 Borneo
- 33 Sapudi
- 34 Sebuku
- 35 Sangeang
- 36 Taiwan
- 37 Togian
- 38 Indonesia
- 39 Timor
- 40 Tidore
- 41 Ngulu
- 42 Fais
- 43 New Guinea
- 44 Eauripik
- 45 Elato
- 46 Romanum
- 47 Etal
- 48 Kapingamarangi
- 49 Nukuoro
- 50 Pohnpei
- 51 Kosrae
- 52 Nauru
- 53 Banaba
- 54 Butaritari
- 55 Makin
- 56 Abaiang
- 57 Maiana
- 58 Tarawa
- 59 Marakei
- 60 Kuria
- 61 Aranuka
- 62 Abemama
- 63 Nonouti
- 64 Tabiteuea
- 65 Onotoa
- 66 Beru
- 67 Tamana
- 68 Nikunau
- 69 Arorae
- 70 Howland Island
- 71 Baker Island
- 72 Winslow Reef
- 73 Nikumaroro
- 74 McKean Island
- 75 Carondelet Reef
- 76 Kiribati
- 77 Orona
- 78 Kanton Island
- 79 Birnie Island
- 80 Manra
- 81 Enderbury Island
- 82 Rawaki
- 83 Jarvis Island
- 84 Kiritimati
- 85 Malden
- 86 Darwin
- 87 Isabela
- 88 Galápagos Islands
- 89 Ecuador
- 90 Colombia
- 91 Suriname
- 92 Brazil
- 93 Caviana
- 94 Marajó
- 95 Mosqueiro
- 96 Rocas Atoll
- 97 Fernando de Noronha
- 98 Ascension
- 99 Bobowasi
- 100 See also
- 101 References
- 102 External links
Togo is located at 6°8'N 1°13'E.
Archaeological finds indicate that ancient tribes were able to produce pottery and process iron. The name Togo is translated from the Ewe language as "land where lagoons lie". Not much is known of the period before arrival of the Portuguese in 1490. During the period from the 11th century to the 16th century, various tribes entered the region from all directions: the Ewé from the west, and the Mina and Gun from the east.
There are signs of Ewe settlement for several centuries before the Portuguese arrival.
Benin is located at 6°28'N 2°36'E.
Before 1700, there were a few important city-states along the coast (primarily of the Aja ethnic group, but also including Yoruba and Gbe peoples) and a mass of tribal regions inland (composed of Bariba, Mahi, Gedevi, and Kabye peoples). The Oyo Empire, located primarily to the east of modern Benin, was the most significant large-scale military force in the region. It regularly conducted raids and exacted tribute from the coastal kingdoms and the tribal regions. The situation changed in the 1600s and early 1700s as the Kingdom of Dahomey, consisting mostly of Fon people, was founded on the Abomey plateau and began taking over areas along the coast. By 1727, king Agaja of the Kingdom of Dahomey had conquered the coastal cities of Allada and Whydah, but it had become a tributary of the Oyo empire and did not directly attack the Oyo allied city-state of Porto-Novo. The rise of the kingdom of Dahomey, the rivalry between the kingdom and the city of Porto-Novo, and the continued tribal politics of the northern region, persisted into the colonial and post-colonial periods.
The Dahomey Kingdom was known for its culture and traditions. Young boys were often apprenticed to older soldiers, and taught the kingdom's military customs until they were old enough to join the army. Dahomey was also famous for instituting an elite female soldier corps, called Ahosi, i.e. the king's wives, or Mino, "our mothers" in the Fon language Fongbe, and known by many Europeans as the Dahomean Amazons. This emphasis on military preparation and achievement earned Dahomey the nickname of "black Sparta" from European observers and 19th-century explorers such as Sir Richard Burton.
Annobón is at 1°25'S 5°38'E.
Annobón is an extinct volcano about 220 miles (350 km) west of Cape Lopez in Gabon and 110 miles (180 km) southwest of São Tomé Island. The main island measures about 4 miles (6.4 km) long by 2 miles (3.2 km) wide, with an area of about 6 3⁄4 square miles (17 km2), but a number of small rocky islets surround it, including Santarém to the south. Its central crater lake is named Lago A Pot and its highest peak is Quioveo, which rises 598 meters (1,962 ft). The island is characterized by a succession of lush valleys and steep mountains, covered with rich woods and luxuriant vegetation.
Annobón is often described as being "in the Gulf of Guinea", for example, by the Encyclopædia Britannica Eleventh Edition. like the neighboring islands of São Tomé and Príncipe, but the formal boundary line for the Gulf of Guinea established by the International Hydrographic Organization actually runs north of it. From the 1953 Limits of Oceans and Seas: "(34) A line running south-eastwards from Cape Palmas in Liberia to Cape Lopez [in Gabon] (0°38' S, 8°42' E)."
Ilhéu das Rolas
Ilhéu das Rolas is located at 0°00'14"S 6°31'21"E.
The independent nation of São Tomé and Príncipe has an equatorial marker shown on the right in São Tomé. São Tomé is located at 0°14'N 6°36'E. It is located 2 km (1¼ miles) north of the equator. The island is surrounded by a number of small islands, including Ilhéu das Rolas, Ilhéu das Cabras and Ilhéu Gabado. The youngest dated rock on the island is about 100,000 years old, but numerous more recent cinder cones are found on the southeast side of the island.
The islands of São Tomé and Príncipe were uninhabited at the time of the arrival of the Portuguese sometime between 1469 and 1471.
Príncipe is located at 1°37'N 7°24'E.
Príncipe is the smaller, northern major island of the country of São Tomé and Príncipe lying off the west coast of Africa in the Gulf of Guinea. It has an area of 142 square kilometres (55 sq mi) (including offshore islets) and a population of 7,324 at the 2012 Census; the latest official estimate (at May 2018) was 8,420. The island is a heavily eroded volcano speculated to be over three million years old, surrounded by smaller islands including Ilheu Bom Bom, Ilhéu Caroço, Tinhosa Grande and Tinhosa Pequena. Part of the Cameroon Line archipelago, Príncipe rises in the south to 947 metres at Pico do Príncipe.
Bioko is located at 3°30'N 8°41'E.
The island is located off Cameroon, in the Bight of Bonny portion of the Gulf of Guinea. Its geology is volcanic; its highest peak is Pico Basile at 3,012 m (9,882 ft).
Bioko used to be the end of a peninsula attached to the mainland in what is now Cameroon, but it was cut off when sea levels rose 10,000 years ago at the end of the last ice age.
The topographic image on the left shows Bioko as the last green island off Cameroon connected by gray continental shelf to Africa.
One perspective offers that the Bubi were once enslaved by a single continental African tribe, likely another Bantu ethnic group that once occupied areas along the shores of West Africa.
The Bubi people are subdivided into a number of tribes and subtribes that go back centuries. Indigenous Bubi folklore indicate that the tribe immigrated to Bioko Island some 3,000 years ago as a means of escaping servitude.
The map on the right shows the location of Bonga Field off Nigeria where colors browns to gray approximately represent areas near or above sea level during the last ice age (currently 1,000 meters up to sea level).
Corisco is located at 0°55'N 9°19'E.
During the Iron Age (50 BC - 1400 AD) and before the arrival of the Portuguese, the island was densely settled. The most important evidence of human occupation comes from the area of Nandá, near the eastern coast, where dozens of prehistoric burials have been excavated. These burials belong to two different periods: Early Iron Age (50 BC - 450 AD) and Middle Iron Age (1000-1150 AD). During the first period, the islanders deposited bundles of human bones and iron implements (axes, bracelets, spears, spoons, iron currency) in shallow pits dug in the sand. During the second period, tombs have been documented where the corpses (not preserved) lied down surrounded by pots, probably containing food and alcoholic beverages. The deceased were interred with their adornments (collars, bracelets and anklets) and a few personal possessions (knives and adzes).
Equatorial Guinea is located at 1°30'N 10°00'E.
Equatorial Guinea consists of two parts, an insular and a mainland region. The Islands of Equatorial Guinea, the insular region, consists of the islands of Bioko (formerly Fernando Pó) in the Gulf of Guinea and Annobón, a small volcanic island which is the only part of the country south of the equator. Bioko Island is the northernmost part of Equatorial Guinea. The island nation of São Tomé and Príncipe is located between Bioko and Annobón. The mainland region, Río Muni, is bordered by Cameroon on the north and Gabon on the south and east. Rio Muni includes several small offshore islands, such as Corisco, Elobey Grande, and Elobey Chico.
Pygmy peoples probably once lived in the continental region that is now Equatorial Guinea, but are today found only in isolated pockets in southern Río Muni. Bantu migrations between the 18th and 19th centuries from between south-east Nigeria and north-west Cameroon (the Grassfields). brought coastal ethno-linguistic groups as well as the Fang people. They must have settled continental Equatorial Guinea around 500 BCE at the latest. Elements of the latter may have generated the Bubi people, who migrated from Cameroon to Río Muni and Bioko in several waves and succeeded former Neolithic populations. The Annobonese Creole population, originally native to Angola, was introduced by the Portuguese via São Tomé island.
Cameroon is located at 6°N 12°E.
The territory of present-day Cameroon was first settled during the Neolithic Era. The longest continuous inhabitants are groups such as the Baka (Pygmies). From here, Bantu migrations into eastern, southern, and central Africa are believed to have originated about 2,000 years ago. The Sao culture arose around Lake Chad, c. 500 AD, and gave way to the Kanem and its successor state, the Bornu Empire. Kingdoms, fondoms, and chiefdoms arose in the west.
On the right is an image of a sign announcing the equator in Gabon in Libreville.
Gabon is located at 1°S 12°E.
The earliest inhabitants of the area were Pygmy peoples. They were largely replaced and absorbed by Bantu tribes as they migrated.
The African Pygmies (or Congo Pygmies, variously also "Central African foragers", "African rainforest hunter-gatherers" (RHG) or "Forest People of Central Africa") are a group of tribal ethnicities, traditionally subsisting in a forager and hunter-gatherer lifestyle, native to Central Africa, mostly the Congo Basin.
The African Pygmies are divided into three roughly geographic groups:
- the western Bambenga or Mbenga (Cameroon, Gabon, Republic of the Congo, Central African Republic),
- the eastern Bambuti or Mbuti of the Congo basin (Democratic Republic of the Congo (DRC))
- the central and southern Batwa or Twa (Rwanda, Burundi, Democratic Republic of the Congo (DRC), Tanzania, Uganda, Zambia, Angola and Namibia). The more widely scattered (and more variable in physiology and lifestyle) Southern Twa are also grouped under the term Pygmoid.
They are notable for, and named for, their short stature (described as "pygmyism" in anthropological literature). They are assumed to be descended from the original Middle Stone Age expansion of anatomically modern humans to Central Africa, albeit substantially affected by later migrations from West Africa, from their first appearance in the historical record in the 19th century limited to a comparative small area within Central Africa, greatly decimated by the prehistoric Bantu expansion, and to the present time widely affected by enslavement and cannibalism at the hand of neighboring Bantu groups.
Gabon was settled from the 14th century by Bantu peoples. Little is known of tribal life before European contact, but tribal art suggests a rich cultural heritage.
Republic of the Congo
The equator passes through the Republic of the Congo as shown in the map on the right.
Republic of the Congo is located at 1.44°S 15.556°E.
Bantu-speaking peoples who founded tribes during the Bantu expansions largely displaced and absorbed the earliest inhabitants of the region, the Pygmy people, about 1500 BC. The Bakongo, a Bantu ethnic group that also occupied parts of present-day Angola, Gabon, and the Democratic Republic of the Congo, formed the basis for ethnic affinities and rivalries among those countries. Several Bantu kingdoms—notably those of the Kongo, the Loango, and the Teke—built trade links leading into the Congo River basin.
Democratic Republic of the Congo
The map on the right shows the equator passing through the Democratic Republic of the Congo.
Democratic Republic of the Congo is located at 3°S 24°E.
The geographical area now known as the Democratic Republic of the Congo was populated as early as 90,000 years ago, as shown by the 1988 discovery of the Semliki harpoon at Katanda, one of the oldest barbed harpoons ever found, believed to have been used to catch giant river catfish.
Idjwi is located at 2°9'57"S 29°3'22"E.
At 70 km (43 mi) in length and with an area of 340 km2 (131 sq mi), it is the second largest inland island in Africa, and the tenth largest in the world.
Historically a clan-based Bahavu society, Idjwi island became a kingdom in the late 18th century (roughly between 1780 and 1840).
Uganda is located at 1°N 32°E.
Near the city of Masaka, Uganda, is this equatorial monument in the image on the right.
The map on the left shows approximately where the equator passes through Uganda.
Paleolithic evidence of human activity in Uganda goes back to at least 50,000 years, and perhaps as far as 100,000 years, as shown by the Acheulean stone tools recovered from the former environs of Lake Victoria, which were exposed along the Kagera River valley, chiefly around Nsonezi. Rock art in Uganda, particularly in the eastern part of the country, attests to occupation during the Later Stone Age as well.
Ssese Islands are located at 00°26'00"S 32°15'00"E.
Bugala is located at 00°25'8"S 32°15'00"E.
Ukerewe is located at 2°1'45"S 33°0'35"E.
Ukerewe is the fifth-largest lake island in the world. With an area of 530 km2 (200 sq mi), it is also the largest island in Lake Victoria and the largest lake island in Africa. Ukerewe Island is situated in the Ukerewe District of Tanzania, 45 km (28 mi) north of Mwanza to which it is linked by ferry.
Ukerewe is known for having a large population of Africans with albinism. Many of the first of them to live there were taken to and abandoned on the island by their families as children. Despite comprising an exceptionally high percentage of the island's population, they are still, as throughout Tanzania, an oppressed minority on the island, though it appears to have avoided the killings of albinos, who are "harvested" for black magic rituals, that regularly occurs in Tanzania.
Tanzania is located at 6°S 35°E.
Many important hominid fossils have been found in Tanzania, such as 6 million year-old Pliocene hominid fossils. The genus Australopithecus ranged all over Africa 4-2 million years ago; and the oldest remains of the Homo genus are found near Lake Olduvai. Following the rise of Homo erectus 1.8 million years ago, mankind spread all over the Old World, and later in the New World and Australia under the species Homo sapiens. Homo sapiens also overtook Africa and absorbed the older archaic species and subspecies of humanity. One of the oldest known ethnic groups still existing, the Hadzabe, appears to have originated in Tanzania, and their oral history recalls ancestors who were tall and were the first to use fire, medicine, and lived in caves, much like Homo erectus or Homo heidelbergensis who lived in the same region before them.
Later in the Stone and Bronze Age, prehistoric migrations into Tanzania included Southern Cushitic speakers who moved south from present-day Ethiopia; Eastern Cushitic people who moved into Tanzania from north of Lake Turkana about 2,000 and 4,000 years ago; and the Southern Nilotes, including the Datoog, who originated from the present-day South Sudan–Ethiopia border region between 2,900 and 2,400 years ago. These movements took place at about the same time as the settlement of the Mashariki Bantu from West Africa in the Lake Victoria and Lake Tanganyika areas. They subsequently migrated across the rest of Tanzania between 2,300 and 1,700 years ago.
Kenya is located at 1°N 38°E.
The Kikuyu belong to the Northeast Bantu languages. Their language is most closely related to that of the Embu people and Mbeere people. Geographically, they are concentrated in the vicinity of Mount Kenya.
The exact place that the Northeast Bantu speakers migrated from after the initial Bantu expansion is uncertain. Some authorities suggest that the Kikuyu arrived in their present Mount Kenya area of habitation from earlier settlements further to the north and east, while others argue that the Kikuyu, along with their closely related Eastern Bantu neighbors the Embu people, Meru people, Mbeere people, and Kamba people moved into Kenya from points further north.
From archaeological evidence, their arrival at the northern side of Mt. Kenya dates to around the 3rd century, as part of the larger group known as Thagicu.
By the 6th century, there was a community of Agikuyu newly established at Gatunganga, or Gatuang'ang'a in Nyeri County. The Agikuyu established themselves in their current homeland of Mt.Kenya region by the 13th century.
On the right is a sign posted on the equator in Kenya.
The equator passes through Kenya as shown in the map on the left.
Ngai – The Supreme Creator
The Gĩkũyũ were – and still are – monotheists believing in an omnipotent God whom they refer to as Ngai. All of the Gĩkũyũ, Embu, and Kamba use this name. Ngai was also known as Mũrungu by the Meru and Embu tribes, or Mũlungu (a variant of a word meaning God which is found as far south as the Zambezi of Zambia). The title Mwathani or Mwathi (the greatest ruler) comes from the word gwatha meaning to rule or reign with authority, was and is still used. All sacrifices to Ngai were performed under a Ficus sycomorus (sycamore tree) (Mũkũyũ) and if one was not available, a fig tree (Mũgumo) would be used. The olive tree (Mũtamaiyũ) was a sacred tree for women.
Zanzibar is located at 6°08'S 39°19'E.
The presence of microliths suggests that Zanzibar has been home to humans for at least 20,000 years, which was the beginning of the Later Stone Age.
Somalia is located at 10°N 49°E.
Somalia has been inhabited since at least the Paleolithic. During the Stone Age, the Doian and Hargeisan cultures flourished here. The oldest evidence of burial customs in the Horn of Africa comes from cemeteries in Somalia dating back to the 4th millennium BCE. The stone implements from the Jalelo site in the north were also characterized in 1909 as important artefacts demonstrating the archaeological universality during the Paleolithic between the East and the West.
According to linguists, the first Afroasiatic-speaking populations arrived in the region during the ensuing Neolithic period from the family's proposed urheimat ("original homeland") in the Nile Valley, or the Near East.
The Laas Geel complex on the outskirts of Hargeisa in northwestern Somalia dates back approximately 5,000 years, and has rock art depicting both wild animals and decorated cows. Other cave paintings are found in the northern Dhambalin region, which feature one of the earliest known depictions of a hunter on horseback. The rock art is in the distinctive Ethiopian-Arabian style, dated to 1,000 to 3,000 BCE. Additionally, between the towns of Las Khorey and El Ayo in northern Somalia lies Karinhegane, the site of numerous cave paintings of real and mythical animals. Each painting has an inscription below it, which collectively have been estimated to be around 2,500 years old.
North and South Malosmadulu Atols are in the Maldives, an island republic in the northern Indian Ocean, southwest of India. Maldives is made up of a chain of 1192 small coral islands that are grouped into clusters of atolls. It has a total area of 298 sq km and a population of about 330,000. The capital and largest city is Male, with a population of about 80,000. Arguably the lowest-lying country in the world, the average elevation is 1 m above sea level. Waves triggered by the great tsunami of December 2004 spilled over sea walls to flood Male with sand-clouded water and then swept out just as suddenly. Residents fear this was a foreboding of disasters to come from sea-level rise due to global warming. The simulated natural color ASTER image was acquired 22 December 2002, covers an area of 50.8 x 90.4 km, and is centered near 5.3 degrees north latitude, 73.9 degrees west longitude.
Raa Atoll is located at 5°38'N 72°55'E.
The first Maldivians did not leave any archaeological artifacts. Their buildings were probably built of wood, palm fronds and other perishable materials, which would have quickly decayed in the salt and wind of the tropical climate. Moreover, chiefs or headmen did not reside in elaborate stone palaces, nor did their religion require the construction of large temples or compounds.
Comparative studies of Maldivian oral, linguistic and cultural traditions and customs confirm that the first settlers were people from the southern shores of the neighboring Indian subcontinent, including the Giraavaru people mentioned in ancient legends and local folklore about the establishment of the capital and kingly rule in Malé.
A strong underlying layer of Dravidian population and culture survives in Maldivian society, with a clear Tamil-Malayalam substratum in the language, which also appears in place names, kinship terms, poetry, dance, and religious beliefs. Malabari seafaring culture led to the settlement of the Islands by Malayali seafarers.
The earliest written history of the Maldives was marked by the arrival of Sinhalese people in Sri Lanka and the Maldives (Mahiladvipika) circa 543 to 483 BC, as reported in the Mahavansa. Their settlement marks a significant change in demographics and the development of the Indo-Aryan language Dhivehi language.
Physical location of the equirectangular projection: 7.5°N, 1.2°S, 71.9°E, 74.7°E.
Alifushi is located at 5°58'00"N 72°57'15"E, left upper atoll before angled atolls.
Simeulue is located at 2°35'N 96°05'E.
From the ethnic point of view the inhabitants of Simeulue are similar to the people of neighboring Nias Island. Two languages and a number of dialects are spoken on the island: Devayan and Sigulai, which are different from the languages spoken in the north of Sumatra.
Nias is located at 1°6'N 97°32'E.
Customary law of the Nias people is generally referred to as fondrakö, which regulates all aspects of life from birth to death. Historical evidence of megalithic structures and carvings of stones that are found in the interior of the island proved that ancient Nias people practiced megalith culture. The caste system is also recognized in Nias society, whereby the highest level out of the 12 levels in the Nias caste system is Balugu.
According to the people of Nias, one of the mythical origins of Nias tribe comes from a tree of life called Tora Sigaru'a which is located at a place called Tetehöli Ana'a. According to the myth, it is said that the arrival of the first human on Nias island began in the days of King Sirao, whose nine sons had been banished out of Tetehöli Ana'a for fighting over the throne. Hence the nine sons of King Sirao were considered as the first people to set foot on the island of Nias.
The observations found that there has been human habitation on Nias island since 12,000 years ago through migration from Asia to Nias island during the Paleolithic period. In fact there are indications of migration as far as 30,000 years ago. During that period the Hòa Bình, Vietnam civilization was similar to that in Nias island. Therefore, it was presumed that the origins of the Nias people came from an area in mainland Asia that is in modern-day Vietnam.
New genetic research has found that the Nias people of North Sumatra came from the Austronesian peoples. The ancestors of the Nias people are also thought to have come from Taiwan through the Philippines 4,000 to 5,000 years ago.
Research that lasted for 10 years with blood samples of 440 Nias people in 11 villages in Nias island has shown the Y-chromosome and DNA mitochondria of the Nias people are very identical to the Taiwanese aborigines and Filipino peoples. The observation has also found that the genes in today's Nias people no longer carry any traces of the ancient Nias people, as of those whose remains were found in the Togi Ndrawa cave, Central Nias. Archaeological findings of the stone tools found showed that humans living in the cave are 12,000 years old. The genetic diversity of the Nias people are very low compared to other people groups, especially with regard to the Y-chromosome. This indicates that there was once a "bottle neck" population in the past history of Nias. Studies have also found that the Nias people do not share any genes with ethnicities living in the Andaman-Nicobar islands in the Indian ocean, which are geographically considered as neighbours. Although it is known that there was a migration of the Austronesian peoples between Taiwan and the Indonesian archipelago including Nias, it is still uncertain if the migration started from Taiwan to Nias or vice versa.
Nias villages often possess impressive stone monuments and large houses which stood on earthquake-resistant timber pylons. Most of these villages have lost its old houses because of their deterioration and difficulties in maintaining the ancient wooden structures from rot, insects and wear, and hence replaced by other more generic structures. Other reasons why not so many old horses were rebuilt because of the over-harvesting of the forests.
In the past, Nias villages, especially those of South Nias, were strategically built on top of a ridge or hill and were surrounded by ramparts and security gates. Entry into this village was provided by only two gates via steep staircases. The gates lead to a straight paved avenue which run through the village center, with row of traditional houses on the sides of the avenue. Close to the main square of the village was the house of the village founders, the omo sebua. In Nias villages, the space in front of each houses was the property of the inhabitants. This "front courtyard" was used for mundane activities e.g. drying harvests before storing.
Villages in Central Nias was usually smaller than its southern counterpart. The houses are also positioned farther away from the main avenue.
The people of Nias placed great value on wooden figures or adu. The sole purpose of the Nias figures was to fulfil ritual needs, whether it is to ensure wealth or to perform specific beneficial rite. Niassan figures vary in size, from as small as 20 centimetres (7.9 in) in height to more than 2 metres (6.6 ft) tall.
When an elderly person died, the family would make a wooden statue known as adu zatua. The statue was unveiled on the fourth day after the death of the person. The shape of the wooden statue reflects the status of the person who used them: the more powerful the owner, the more impressive the statue will be made. Nias people believed that the deceased person's spirits reside in the statue, so all events that occurred in the family were shared with the ancestor statues through prayers. Ancestor figures were believed to ensure fertility for the family, livestock and agricultural land. Sacrifices were made to the ancestor statues especially on important events e.g. births, marriages and deaths. Ancestor statues were placed in the main room of the house, sometimes more than a hundred. A missionary work in 1930 had recorded the removal of 'over 2000 "idols" from a house of new northern convert.' Some missionary even recorded collapsing houses under the weight of these ancestor figures. Small adu zatua were bound together horizontally using a rattan and pegs.
In North Nias, large impressive ancestor figure is known as adu suraha salawa (Nias language for "portraits of honored ancestors"). The adu suraha salawa represents the first known ancestor of a family, often the founder of the village. The adu suraha salawa were usually placed upon a wall or on an altar (daro-daro). Another large ancestor statues are the adu hörö. Adu hörö ancestor statues are large, elongated, armless and wear high, forked headdresses. These statues are generally found in Central Nias, and rarely in South Nias.v
Other wooden figures do not represent the ancestors. These wooden figures were created to heal specific illnesses, to protect villages, or to invoke supernatural beings to aid through rituals. These statues were generally crudely made, as opposed to the finely carved ancestor figures. Joachim von Brenner-Felsach classified more than 60 types of non-ancestor wooden figures.
Many ancestor figures were destroyed in 1916 by a religious movement which seen them as an old blasphemous religion symbol. Some were sold to collectors and can be found in museum or private collections around the world.
The Nias produced one of the most impressive megalith culture in Indonesia, especially the Center and South Nias. Stones were used to construct different objects and structures. Nias village features impressive stoneworks e.g. large staircases and broad paved streets. Ritual objects e.g. the behu (vertical column), standing columns, jumping stones, obelisks, altars, and sarcophagi are among the many stone objects produced by Nias people.
Stone monuments were central in the owasa festival, a kind of feast to raise the rank of a person. Dedicating stone monuments publicly is considered as one of the several requirements that must be done by a person to proof that he had fulfilled the right to claim a higher rank and to receive honorary titles.
The behu is a type of megalith in the form of vertical column. Behu were erected in front of the house of the host to commemorate former great celebrations held by the host. The more behu displayed in front of the host's house, the more powerful his position are in the village. Noblemen display behu that is larger in size and more abundant in numbers than the commoners. A behu with anthropomorphic form is known as the osa-osa. The osa-osa is depicted as wearing traditional Nias attire e.g. the kalabubu necklace and pendant earrings (fondulu or saro dalinga). The osa-osa's head is that of the various beasts, usually a lasara, a hornbill, a stag, or a multi-headed mixture of all. Before displaying the osa-osa in front of houses, they were paraded around the village with the host seated, or even standing on top of the osa-osa.
The Nias people used a variety of material for the creation of their weaponry: leather, cord or woven fibres, precious metal, iron and brass. The Nias used spears, swords and blades as their weapon. The Nias spear (toto'a doho in the south, toho in the north) was mainly used for hunting; the shaft is made of dark hardwood of Oncosperma tigillarium nibung palm wrapped with rattan. Other type of spears are the burusa, with a triangle-shaped head. The Nias sword (gari) is a combat weapon; both the sword and its sheath have simple undecorated form. The most well-known of the Nias weapon is the balato or tolögu, a steel sword with a protective amulet believed to possess magical power. The balato has a hilt made of brass. The sheath of the balato contains a spherical bundle of rattan (ragö balatu) which performed as a protective amulet. This protective amulet is usually attached with a variety of objects e.g. animal fangs which is formed so that it looks like the jaw of the mythical lasara. The balato is only reserved for the highest nobles as a kind of proof of the authority and the social rank of its owner.
Some prominent chiefs covered their armor with sheets of gold. Helmets can be made of iron or tightly woven palm fibers. The oval-shaped shield is known as the baluse in South Nias, while the North Nias produced a hexagonal-shaped shield known as the dange.
Deterioration in Niassan culture already happened since the end of the 19th-century. Missionary works had contribute to the decline of original Nias culture. Missionary works in Nias such as those performed by the German Protestant Rhenish Missionary Society as well as the Roman Catholics had been responsible to the destruction of Niassan wooden statues as well the suppression of unique culture of Nias society e.g. ancestor worship, magical practices, the Owasa festivals (noblemen rank-elevation festivals) headhunting and slave trading.
Pini is located at 0.10°N 98.70°E.
Sumatera is Indonesian for Sumatra. Sumatera is located at 00°N 102°E.
Sumatra was known in ancient times by the Sanskrit names of Swarnadwīpa ("Island of Gold") and Swarnabhūmi ("Land of Gold"), because of the gold deposits in the island's highlands. The first mention of the name of Sumatra was in the name of Srivijayan Haji (king) Sumatrabhumi ("King of the land of Sumatra"), who sent an envoy to China in 1017. Arab geographers referred to the island as Lamri (Lamuri, Lambri or Ramni) in the tenth through thirteenth centuries, in reference to a kingdom near modern-day Banda Aceh which was the first landfall for traders. The island is also known by other names namely, Andalas  or Percha Island.
Singapore is located at 1.3°N 103.8°E.
Singapore is an island city-state in Southeast Asia that lies one degree (137 kilometres or 85 miles) north of the equator, at the southern tip of the Malay Peninsula, with Indonesia's Riau Islands to the south and Peninsular Malaysia to the north. Singapore's territory consists of Pulau Ujong (main island) along with 62 other islets.
Christmas Island is located at 10°29'S 105°38'E.
The island is about 19 kilometres (12 mi) in greatest length and 14.5 km (9.0 mi) in breadth. The total land area is 135 square kilometres (52 sq mi), with 138.9 km (86.3 mi) of coastline. The island is the flat summit of an underwater mountain more than 4,500 metres (14,800 ft) high, which rises from about 4,200 m (13,780 ft) below the sea and only about 300 m (984 ft) above it.
The mountain was originally a volcano, and some basalt is exposed in places such as The Dales and Dolly Beach, but most of the surface rock is limestone accumulated from coral growth. The karst terrain supports numerous anchialine caves. The summit of this mountain peak is formed by a succession of Tertiary limestones ranging in age from the Eocene or Oligocene up to recent reef deposits, with intercalations of volcanic rock in the older beds.
Steep cliffs along much of the coast rise abruptly to a central plateau. Elevation ranges from sea level to 361 m (1,184 ft) at Murray Hill. The island is mainly tropical rainforest, 63% of which is national parkland. The narrow fringing reef surrounding the island poses a maritime hazard.
Christmas Island lies 2,600 kilometres (1,600 mi) northwest of Perth, Western Australia, 350 km (220 mi) south of Indonesia, 975 km (606 mi) ENE of the Cocos (Keeling) Islands, and 2,748 km (1,708 mi) west of Darwin, Northern Territory. Its closest point to the Australian mainland is 1,560 km (970 mi) from the town of Exmouth, Western Australia.
Matak is located at 3.33°N 106.29°E in the South China Sea.
The equatorial monument at Pontianak, Borneo, Indonesia, has Google Earth Latitude: 0° 8'35.40"N Longitude: 109°15'26.78"E.
Sapudi is located at 7.15°S 114.35°E.
Sebuku is located at 3.50°S 116.35°E.
Sangeang is located at 8.20°S 119.05°E.
Taiwan is located at 25°02'N 121°38'E.
Togian is located at 0.39°S 121.94°E.
Indonesia lies between latitudes 11th parallel south (11°S) and 6th parallel north (6°N), and longitudes 95th meridian east (95°E) and 141st meridian east (141°E). It is the largest archipelagic country in the world, extending 5,120 kilometres (3,181 mi) from east to west and 1,760 kilometres (1,094 mi) from north to south. According to a geospatial survey conducted between 2007 and 2010 by the Badan Informasi Geospasial (National Mapping Agency), Indonesia has 13,466 islands, scattered over both sides of the equator, and with about 6,000 of them are inhabited. The largest are Java, Sumatra, Borneo (shared with Brunei and Malaysia), Sulawesi, and New Guinea (shared with Papua New Guinea). Indonesia shares land borders with Malaysia on Borneo, Papua New Guinea on the island of New Guinea, and East Timor on the island of Timor. Indonesia shares maritime borders across narrow straits with Singapore, Malaysia, Vietnam, the Philippines, and Palau to the north, and Australia to the south.
Fossils and the remains of tools show that the archipelago was inhabited by Homo erectus, known as "Java Man", between 1.5 million years ago and 35,000 years ago. Homo sapiens reached the region around 45,000 years ago. Austronesian peoples, who form the majority of the modern population, migrated to Southeast Asia from present-day Taiwan. They arrived around 2,000 BCE, and as they spread through the archipelago, confined the indigenous Melanesian peoples to the far eastern regions. Ideal agricultural conditions and the mastering of wet-field rice cultivation as early as the 8th century BCE allowed villages, towns, and small kingdoms to flourish by the first century CE. Indonesia's strategic sea-lane position fostered inter-island and international trade, including links with Indian kingdoms and Chinese dynasties, which were established several centuries BCE. Trade has since fundamentally shaped Indonesian history.
Timor is located at 9°14'S 124°56'E.
Anthropologists identify eleven distinct ethno-linguistic groups in Timor. The largest are the Atoni of western Timor, and the Tetum of central and eastern Timor. Most indigenous Timorese languages belong to the Timor–Babar branch of the Austronesian languages spoken throughout the Indonesian archipelago. Although lexical evidence is lacking, the non-Austronesian languages of Timor are thought to be related to languages spoken on Halmahera and in Western New Guinea.
Tidore is located at 0.67°N 127.42°E.
Ngulu is located at 8.50°N 137.50°E.
Fais is located 9.75°N 140.52°E.
New Guinea is located at 5°30'S 141°00'E.
The Duna are an indigenous people of Papua New Guinea (also known as Yuna) who live in the north-western area of the Southern Highlands Province and number approximately 11,000 (1991)
Eauripik is located at 6.70°N 143.07°E.
Elato is located at 7.45°N 146.15°E.
Romanum is located at 7°26'29"N 151°40'9"E.
Etal is located at 5.41°N 153.51°E.
Kapingamarangi is located at 0.57°N 154.71°E.
Nukuoro is located at 3.88°N 154.95°E.
Pohnpei is located at 6°53'N 158°14'E.
Kosrae, or Kusaie, is located 5.11°N 162.88°E.
Nauru is located at 0°32'S 166°55'E.
Fifty-eight percent of people in Nauru are ethnically Nauruan, 26 percent are other Pacific Islander, 8 percent are European, and 8 percent are Han Chinese. Nauruans are descended from Polynesian and Micronesian seafarers. Two of the 12 original tribal groups became extinct in the 20th century.
Nauru is a 21-square-kilometre (8.1 sq mi), oval-shaped island in the southwestern Pacific Ocean, 55.95 kilometres (34.77 mi) south of the equator. The island is surrounded by a coral reef, which is exposed at low tide and dotted with pinnacles. The presence of the reef has prevented the establishment of a seaport, although channels in the reef allow small boats access to the island. A fertile coastal strip 150 to 300 metres (490 to 980 ft) wide lies inland from the beach.
Coral cliffs surround Nauru's central plateau. The highest point of the plateau, called the Command Ridge, is 71 metres (233 ft) above sea level.
The only fertile areas on Nauru are on the narrow coastal belt where coconut palms flourish. The land around Buada Lagoon supports bananas, pineapples, vegetables, Pandanus tectorius (pandanus trees), and indigenous hardwoods, such as the Calophyllum inophyllum (tomano tree).
Banaba is located at 0°51'34"S 169°32'13"E.
It has an area of 6.0 km2, and the highest point on the island is also the highest point in Kiribati, at 81 metres (266 ft) high. Along with Nauru and Makatea (French Polynesia), it is one of the important elevated phosphate-rich islands of the Pacific.
According to "Te Rii Ni Banaba—The Backbone of Banaba" by Raobeia Ken Sigrah, Banaban oral history supports the claim that the people of the Te Aka clan, which originated in Melanesia, were the original inhabitants of Banaba (Ocean Island), having arrived before the arrival of later migrations from the East Indies and Kiribati.
Banabans are ethnically distinct from other I-Kiribati. The Banabans were assimilated only through forced migrations and the impact of the discovery of phosphate in 1900. Prior to the relocation of its inhabitants at the end of World War II, there were four villages on the island - Ooma (Uma), Tabiang, Tapiwa (Tabwewa), and Buakonikai.
A three-year drought starting in 1873 killed over three quarters of the population and wiped out almost all the trees; many of those who survived left the island on passing ships to escape the drought, and only some were able to return, often years later.
Butaritari is located at 3°10'04"N 172°49'33"E.
The lagoon is deep and can accommodate large ships, though the entrance passages are relatively narrow.
The south and southeast portion of the atoll comprises a nearly continuous islet, broken only by a single, broad section of interislet reef. These islets are mostly between 0.2 km (0.1 mi) and 0.5 km (0.3 mi) across, but widen in the areas where the reef changes directions. Mangrove swamps appear well developed in these latter areas as well as all along the southern lagoon shore. (Narrow islets are somewhat characteristic of Kiribati atolls running east-west.)
Bikati and Bikatieta islets occupy a corner of the reef at the extreme northwest tip of the atoll, bordering a small lagoon to the north of the main lagoon. There is a village on the larger Bikati (2 by 0.5 km).
An important legend in the culture of Butaritari is that spirits who lived in a tree in Samoa migrated northward carrying branches from the tree, Te Kaintikuaba, which translates as the tree of life. It was these spirits, together with Nareau the Wise who created the islands of Tungaru (the Gilbert Islands).
Makin is located at 3°23'00"N 173°00'00"E.
Makin is the northernmost of the Gilbert Islands, with a population (in 2010) of 1,798.
Kiebu, the second largest islet, has an even smaller, completely landlocked lagoon on its eastern side, with about 80 m in diameter (making an area of about 0.005 km² or 0.5 hectares) and at distance of 60 m to the open sea.
|Makin: Population and Land Area|
|Islet/Village||Population 2010||Land area (usable)||Density||Area not available for use|
|Little Makin||1,364||1,541.5 acres (624 ha)||0.9 people per acre||Enclosed lagoon 84.7 acres|
|Bikin Eitei||8 acres (3 ha)|
|Aonibike||30.9 acres (13 ha)|
|Tebua Tarawa||5 acres (2 ha)|
|Kiebu||434||242.2 acres (98 ha)||1.8 people per acre|
|Onne||122.6 acres (50 ha)|
|Makin Total||1,798||1,950.2 acres (789 ha)||0.9 people per acre||Enclosed lagoon 84.7 acres|
An important legend in the culture of Makin is that spirits who lived in a tree in Samoa migrated northward carrying branches from the tree, Te Kaintikuaba, which translates as the tree of life.
Nakaa Beach is located at the northern tip of Makin Atoll is an important site in the traditional mythology of the island group, being the departing point for the spirits of the dead heading to the underworld. Nakaa is the legendary guardian of the gateway to the place of the dead.
Abaiang is located at 1°50'N 172°57'E.
The atoll has a lagoon 16 by 5 miles (25.7 by 8.0 km) that provides sheltered anchorage.
The channel is between the biggest island of Abaiang (in the east) and a very little island in the southwest of Abaiang called Teirio.
|Abaiang: Population and Land Area|
|Census Area||Population 2010||Land area by islet||Density (people per acre)|
|Nuotaea||559||330.9 acres (133.9 ha)||1.7|
|Ribono||341||219.3 acres (88.7 ha)||1.6|
|Takarano||348||3,552.6 acres (1,437.7 ha)||1.2|
|Uninhabited islets||0||215.5 acres (87.2 ha)||0|
|Abaiang total||5,502||4,318.3 acres (1,747.6 ha)||1.3|
By tradition, the first inhabitants of Abaiang Island were known to be spirits, some of them created in Samoa and some in Abaiang. Years passed by and then Pacific Islanders came along.
Maiana is located at 0°55'N 173°00'E.
The atoll is 14 kilometres (8.7 mi) long and is very narrow, with an average width of less than 1 kilometre (0.62 mi) and a total land area (including uninhabited islets) of 16.72 square kilometres (6.46 sq mi).
|Maiana: Population and Land Area|
|Census Area||Population 2010||Land area by islet||Density (people per acre)|
|Tebikerai||93||61.2 acres (25 ha)||1.5|
|Tebiauea||211||3,805.6 acres (1,540 ha)||0.5|
|Uninhabited islets||0||263.5 acres (107 ha)||0|
|Maiana total||2,027||4,130.3 acres (1,671 ha)||0.5|
Like all of the atolls of Kiribati, Maiana is at serious risk from sea level rise, as even small changes in sea level can cause accelerated erosion and threaten infrastructure, agriculture and water supplies.
There are different stories told as to the creation of Maiana and the other islands in the Gilberts. An important legend in the culture of Maiana is that spirits who lived in a tree in Samoa migrated northward carrying branches from the tree, Te Kaintikuaba, which translates as the tree of life. It was these spirits, together with Nareau the Wise who created the islands of Tungaru (the Gilbert Islands).
The islets are separated in places by wide channels that are best crossed at low tide, and there is a ferry service between Buota and Abatao.
On South Tarawa, the construction of causeways has now created a single strip of land from Betio in the west to Tanaea in the northeast.
In Kiribati mythology, Tarawa was the earth when the land, ocean and sky had not been cleaved yet by Nareau the spider. Thus after calling the sky karawa and the ocean marawa, he called the piece of rock that Riiki (another god that Nareau found) had stood upon when he lifted up the sky as, Tarawa. Nareau then created the rest of the islands in Kiribati and also Samoa.
People arrived on these islands thousands of years ago, and there have been migrations to and from Kiribati since antiquity.
Evidence from a range of sources, including carbon dating and DNA analyses, confirms that the exploration of the Pacific included settlement of the Gilbert Islands by around 200 BC. The people of Kiribati are still excellent seafarers, capable of making ocean crossings in locally made vessels using traditional navigation techniques.
Marakei is located at 2°00'N 173°17'E.
Two narrow channels, which are not navigable at low tide, link the lagoon with the sea; these are called Baretoa Pass and Raweta Pass.
The construction of causeways have also resulted to significant reduction in the flushing of the lagoon that has resulted in low levels of oxygen in the lagoon, which has resulted in the water becoming stagnant so that fish no longer found in the lagoon. The erosion and accretion that are occurring along the shoreline is identified as being linked to aggregate mining, land reclamation and the construction of causeways that has been thought to change the currents along the shoreline.
There are different stories told as to the creation of Marakei and the other islands in the Southern Gilberts. An important legend in the culture of Marakei is that spirits who lived in a tree in Samoa migrated northward carrying branches from the tree, Te Kaintikuaba, which translates as the tree of life. It was these spirits, together with Nareau the Wise who created the islands of Tungaru (the Gilbert Islands).
The "katabwanin" is a tradition unique to Marakei; first time visitors need to pay their respects to the four ghosts of Marakei, travelling anticlockwise, before any other activities. Offerings of tobacco, sweets or money at the shrines of Nei Reei, Nei Rotebenua, Nei Tangangau and Nei Nantekimam will secure a happy stay in Marakei.
This shrine in the image on the left is at the northern tip of the island, near the airport.
Kuria is located at 0°13'N 173°24'E.
Aranuka is located at 0°09'N 173°35'E.
Aranuka is by tradition the island in the middle of Kiribati and the location for the formation and separation of all the islands of Kiribati which was first started by the God of our Ancestors, Nareau. That is why Aranuka was formerly named and known as Ananuka – the middle of it.
Abemama is located at 0°24'N 173°50'E.
Abemama (Apamama) is an atoll, one of the Gilberts group in Kiribati, and is located 152 kilometres (94 miles) southeast of Tarawa and just north of the Equator. Abemama has an area of 27.37 square kilometres (10.57 square miles) and a population of 3,299 2015. The islets surround a deep lagoon. The eastern part of the atoll of Abemama is linked together by causeways making automobile traffic possible between the different islets. The outlying islands of Abatiku and Biike are situated on the southwestern side of the atoll.
Most of the important food crops in Kiribati such as coconut, giant taro, pandanus and breadfruit grow well in Abemama.
Nonouti is located at 0°40'S 174°20E.
The eastern area of the atoll consists of tiny islets and islands which form a continuous line.
Tabiteuea is located at 1°21'S 174°48'E.
The islanders have customary fishing practices related to the lagoon and the open ocean.
Tabiteuea North has a land area of 26 km2 (10 sq mi) and a population of 3,600 as of 2005, distributed among twelve villages (capital Utiroa)
Tabiteuea South has a land area of 12 km2 (4.6 sq mi) and a population of 1,299, distributed among six villages (capital Buariki).
Howland Island is located at 0°48'25.85"N 176°36'59.48"W.
For statistical purposes, Howland is grouped as one of the United States Minor Outlying Islands. The island has an elongated banana-shape on a north–south axis, and covers 2.6 square kilometres (640 acres).
The island is visited every two years by the U.S. Fish and Wildlife Service.
Sparse remnants of trails and other artifacts indicate a sporadic early Polynesian presence. A canoe, a blue bead, pieces of bamboo, and other relics of early settlers have been found.
"Howland's Island, although naturally uninhabitable, gave various indications of early visitors, probably natives drifting from windward islands, whose traces were still visible in the remains of a canoe, a blue bead, pieces of bamboo, and other distinctly characteristic belongings." The island's prehistoric settlement may have begun about 1000 BC when eastern Melanesians traveled north and may have extended down to Rawaki Island, Kanton Island, Manra Island and Orona of the Phoenix Islands, 500 to 700 km southeast. K.P. Emery, an ethnologist for Honolulu's Bernice P. Bishop Museum, indicated that settlers on Manra Island were apparently of two distinct groups, one Polynesian and the other Micronesian, hence the same might have been true on Howland Island, though no proof of this has been found.
The difficult life on these isolated islands along with unreliable fresh water supplies may have led to the dereliction or extinction of the settlements, much the same as other islands in the area (such as Kiritimati and Pitcairn Islands) were abandoned.
Baker Island is at 00°13'N 176°28'W.
Winslow Reef is a submerged coral reef located at 01°36'S 174°57'W.
"We had one particularity: coming down on Winslow Reef, p. d. (position doubtful): two positions in the directory, a third (if you cared to count that) on the chart; heavy sea running, and the night due. The boats were cleared, bread put on board, and we made up our packets for a boat voyage of four or five hundred miles, and turned in, expectant of a crash. Needless to say, it did not come, and no doubt we were far to leeward."
Gardner Island is located at 04°40'S 174°31'W.
The International Group for Historic Aircraft Recovery (TIGHAR) made several expeditions to Nikumaroro during the 1990s and first decade of the 21st century, finding possible evidence, but no conclusive proof, of this theory. Investigation and expeditions to the island continue.
McKean Island is located at 03°36'S 174°08'W.
Actively worked for guano in the mid-19th century, it was abandoned by 1870, and no further use has been made of it.
Carondelet Reef is located at 05°34'S 173°51'W.
Carondelet Reef is a horseshoe-shaped reef of the Phoenix Islands, also known as the Rawaki Islands, in the Republic of Kiribati, is located 106 km southeast of Nikumaroro, and has a least depth of 1.8 meters, reported to be approximately 1.5 km in length.
Carondelet Reef was named after the vessel which reported it in about 1899.
Kiribati is located at 1°25'N 173°00'W. It's one of those volcanic peaks in the central Pacific as shown on this map of the Pacific Ocean basin.
Kiribati consists of 32 atolls and one solitary island (Banaba), extending into the eastern and western hemispheres, as well as the northern and southern hemispheres. It is the only country that is situated within all four hemispheres. The groups of islands are:
- Banaba: an isolated island between Nauru and the Gilbert Islands
- Gilbert Islands: 16 atolls located some 1,500 kilometres (932 mi) north of Fiji
- Phoenix Islands: 8 atolls and coral islands located some 1,800 kilometres (1,118 mi) southeast of the Gilberts
- Line Islands: 8 atolls and one reef, located about 3,300 kilometres (2,051 mi) east of the Gilberts
Banaba (or Ocean Island) is a raised-coral island. It was once a rich source of phosphates, but was exhausted in mining before independence. The rest of the land in Kiribati consists of the sand and reef rock islets of atolls or coral islands, which rise only one or two metres above sea level.
The soil is thin and calcareous. It has a low water-holding capacity and low organic matter and nutrient content—except for calcium, sodium, and magnesium. Banaba is one of the least suitable places for agriculture in the world.
Kiritimati (Christmas Island) in the Line Islands is the world's largest atoll. Based on a 1995 realignment of the International Date Line, the Line Islands were the first area to enter into a new year, including year 2000. For that reason, Caroline Island has been renamed Millennium Island.
Hull Island is located at 04°30'S 172°10'W.
An ancient stone marae stands on the eastern tip of the island, together with ruins of shelters, graves and other platforms.
Kanton Island is located at 02°48'38"S 171°40'32"W.
Kanton has been described as being shaped like a large pork chop. From its northwest to southeast points is a distance of 14.5 km (9.0 mi), while the land rim varies in width from 50–600 m (160–2,000 ft) and 1.5–7 m (5–25 ft) in elevation. The southeast corner of the island is known as "Pyramid Point." The sole entrances to the lagoon are on the west side, with the main channel exhibiting currents of 6–8 knots (3–4 m/s). The lagoon itself is filled with marine life, holding 153 different species of fish, including tuna, sharks, stingrays and eels. An unpaved road runs around the island, though its current state of repair is uncertain. Canton Island Airport Airport codes CIS PCIS lies at the northwest corner of the island, but it currently lacks any commercial scheduled service. The World Port Index number of Kanton Island is 56025.
Birnie Island is located at 03°35'S 171°33'W.
There is no anchorage, but landing can be made on the lee beach.
Sydney Island is located at 04°27'S 171°15'W.
Two groups of people were present on Manra, one from eastern Polynesia, the other from Micronesia, where wells and pits from these early inhabitants were found.
Enderbury Island is located at 3°08'S 171°05'W.
Phoenix Island is located at 03°43'S 170°43'W.
Rawaki does have several freshwater pools, the only known freshwater wetlands in the Phoenix Islands. Worked for guano from 1859 to 1871, Rawaki was abandoned and no human use seems to have been made of it thereafter.
Jarvis Island, formerly known as Bunker Island, or Bunker's Shoal is located at 0°22'S 160°01'W in the South Pacific Ocean.
It is an unincorporated, unorganized territory of the United States, administered by the United States Fish and Wildlife Service of the United States Department of the Interior as part of the National Wildlife Refuge system.
The indigenous people who inhabit the islands of Polynesia are termed Polynesians, and share many similar traits including language family, culture, and beliefs.
Christmas Island is located at 1°53'N 157°24'W.
Archaeologists have since identified remains of coral marae platforms and/or village complexes on Kiritmati dateable as far back as the 14th century, and show that the inhabitants of the Line Islands were more than just castaways.
Malden is located at 4°1'S 154°56'W.
The island is chiefly notable for its mysterious prehistoric ruins.
In 1924, the Malden ruins were examined by an archaeologist from the Bishop Museum in Honolulu, Kenneth Emory, who concluded that they were the creation of a small Polynesian population which had resided there for perhaps several generations some centuries earlier.
The ancient stone structures are located around the beach ridges, principally on the north and south sides. A total of 21 archaeological sites have been discovered, three of which (on the island's northwest side) are larger than the others. These sites include temple platforms, called marae, house sites, and graves. Comparisons with stone structures on Tuamotu atolls show that a population of between 100 and 200 natives could have produced all of the Malden structures. Maraes of a similar type are found on Raivavae, one of the Austral Islands. Various wells used by these ancients were found by later settlers to be dry or brackish.
Darwin is located at 1.678°N 92.003°W in the Galápagos Islands.
Isabela is located at 00°30'S 91°04'W in the Galápagos Islands.
The islands are found at the coordinates 1°40'N–1°36'S, 89°16'–92°01'W. Straddling the equator, islands in the chain are located in both the northern and southern hemispheres, with Volcán Wolf and Volcán Ecuador on Isla Isabela being directly on the equator.
According to a 1952 study by Thor Heyerdahl and Arne Skjølsvold, potsherds and other artifacts from several sites on the islands suggest visitation by South American peoples in pre-Columbian era. The group located an Inca flute and shards from more than 130 pieces of ceramics, which were later identified as pre-Incan. However, no remains of graves, ceremonial vessels and constructions have ever been found, suggesting no permanent settlement occurred before the Spanish arrived in the 16th century. It is not clear who the first visitors to the islands were, but they were probably sailors blown off course or people on hapless fishing boats blown out to sea. Most of them were likely unimpressed by the lack of fresh water on the islands. Whether the Incas ever made it here is disputed; in 1572, Spanish chronicler Pedro Sarmiento de Gamboa claimed that Topa Inca Yupanqui, the second Sapa Inca of the Inca Empire had visited the archipelago, but there is little evidence for this, and many experts consider it a far-fetched legend, especially since the Incas were not seafaring people.
The volcano Cayambe is located at 0.029°0′0″N 77.986°0′0″W. It is the only permanent snow (glacier) capped peak along the equator.
An equatorial marker in Cayambe, Ecuador, is shown on the right.
Another equatorial marker in Ecuador is Mitad del Mundo, Quito, second image down on the right.
Ecuador is located at 2°00'S 77°30'W.
The archeological evidence suggests that the Paleo-Indians' first dispersal into the Americas occurred near the end of the last glacial period, around 16,500–13,000 years ago.
Colombia is located at 4°N 72°W.
Owing to its location, the present territory of Colombia was a corridor of early human civilization from Mesoamerica and the Caribbean to the Andes and Amazon basin. The oldest archaeological finds are from the Pubenza and El Totumo sites in the Magdalena Valley 100 kilometres (62 mi) southwest of Bogotá. These sites date from the Paleoindian period (18,000–8000 BCE). At Puerto Hormiga and other sites, traces from the Archaic Period (~8000–2000 BCE) have been found. Vestiges indicate that there was also early occupation in the regions of El Abra and Tequendama in Cundinamarca. The oldest pottery discovered in the Americas, found at [San Jacinto, dates to 5000–4000 BCE.
Indigenous people inhabited the territory that is now Colombia by 12,500 BCE. Nomadic hunter-gatherer tribes at the El Abra, Tibitó and Tequendama sites near present-day Bogotá traded with one another and with other cultures from the Magdalena River Valley. Between 5000 and 1000 BCE, hunter-gatherer tribes transitioned to agrarian societies; fixed settlements were established, and pottery appeared. Beginning in the 1st millennium BCE, groups of Amerindians including the Muisca, Zenú, Quimbaya, and Tairona developed the political system of cacicazgos with a pyramidal structure of power headed by caciques. The Muisca inhabited mainly the area of what is now the Departments of Boyacá and Cundinamarca high plateau (Altiplano Cundiboyacense) where they formed the Muisca Confederation. They farmed maize, potato, quinoa and cotton, and traded gold, emeralds, blankets, ceramic handicrafts, coca and especially rock salt with neighboring nations. The Tairona inhabited northern Colombia in the isolated mountain range of Sierra Nevada de Santa Marta. The Quimbaya inhabited regions of the Cauca River Valley between the Western and Central Ranges of the Colombian Andes. Most of the Amerindians practiced agriculture and the social structure of each indigenous community was different. Some groups of indigenous people such as the Caribs lived in a state of permanent war, but others had less bellicose attitudes. The Incas expanded their empire onto the southwest part of the country.
Suriname is located at 4°N 56°W.
The early history of Suriname dates from 3000 BCE when Native Americans first inhabited the area. The largest nations at the time of colonialization were the Arawaks, a nomadic coastal tribe that lived from hunting and fishing, and the Caribs. The Caribs conquered the Arawaks along much of the coast, and into the Caribbean, using sailing ships. They settled in Galibi (Kupali Yumï, meaning "tree of the forefathers") on the mouth of the Marowijne river. While the Arawak and Carib lived off the coast and savanna, smaller groups of indigenous peoples lived in the rainforest inland, such as the Akurio, Trió, Warrau, and Wayana.
On the right is the equatorial marker in Macapá, Brazil.
Brazil is located at 10°S 52°W.
Some of the earliest human remains found in the Americas, Luzia Woman, were found in the area of Pedro Leopoldo, Minas Gerais and provide evidence of human habitation going back at least 11,000 years.
The earliest pottery ever found in the Western Hemisphere was excavated in the Amazon basin of Brazil and radiocarbon dated to 8,000 years ago (6000 BC). The pottery was found near Santarém and provides evidence that the tropical forest region supported a complex prehistoric culture. The Marajoara culture flourished on Marajó in the Amazon delta from 800 CE to 1400 CE, developing sophisticated pottery, social stratification, large populations, mound building, and complex social formations such as chiefdoms.
Around the time of the Portuguese arrival, the territory of current day Brazil had an estimated indigenous population of 7 million people, mostly semi-nomadic who subsisted on hunting, fishing, gathering, and migrant agriculture. The indigenous population of Brazil comprised several large indigenous ethnic groups (e.g. the Tupis, Guaranis, Gês and Arawaks). The Tupí people were subdivided into the Tupiniquins and Tupinambás, and there were also many subdivisions of the other groups.
Before the arrival of the Europeans, the boundaries between these groups and their subgroups were marked by wars that arose from differences in culture, language and moral beliefs. These wars also involved large-scale military actions on land and water, with cannibalistic rituals on prisoners of war. While heredity had some weight, leadership status was more subdued over time, than allocated in succession ceremonies and conventions. Slaver among the Indians had a different meaning than it had for Europeans, since it originated from a diverse socioeconomic organization, in which asymmetries were translated into kinship relations.
Caviana is located at 0°10'N 50°00'W.
Marajó is located at 0°59'S 49°35'W in the delta of the Amazon River.
The island was the site of an advanced pre-Columbian society, the Marajoara culture, which existed from approximately 400 BC to 1600 AD. The island has been a center of archaeological exploration and scholarship since the 19th century. Scholars from the 1980s forward have divided the pre-Columbian period into the Ananatuba phase (c. 1100–c. 200 BC), the Mangueiras phase (c. 1000 BC–c. 100 AD), the Formiga phase (c. 100-400 AD), the Marajoará phase (c. 400-1200 AD), and the Aruã phase (1200-1500 AD).
Since the 1990s, there has been debate over the origins and sophistication of Marajó's pre-Columbian society. Based on fieldwork in the 1940s and 1950s, the archaeologist Betty Meggers initially argued that the Marajoara culture had been founded by emigrants from the Andes, and that the society steadily declined until its final collapse in around 1400 AD, due to the Marajó's poor soil fertility and other environmental factors. Megger's hypotheses subsequently became associated with environmental determinism. However, her claims has since been rejected by the archaeologist Anna Curtenius Roosevelt, who re-excavated Marajó in the 1980s. According to Roosevelt, the Marajoara culture developed independently within the Amazon, and featured both intensive subsistence agriculture and major public works.
Roosevelt estimated that Marajó had a population of possibly over 100,000 people at its peak. The population lived in homes with tamped earth floors, organized themselves into matrilineal clans, and divided tasks by sex, age, and skill level.
Mosqueiro is located at 1.1°S 48.4°W.
The atoll is of volcanic origin and coralline formation.
Rocas Atoll is located at 03°52'S 33°49'W.
Fernando de Noronha
Fernando de Noronha is located at 3°51'13.71"S 32°25'25.63"W.
Ascension Island is located at 7°56'S 14°22'W.
Although volcanic activity is mainly associated with the Mid-Atlantic Ridge plate boundary 80 km to the west, Ascension also displays some features which are commonly associated with hotspot volcanism. This appears to be the result of a smaller mantle plume that originally formed under the Mid-Atlantic Ridge, before the African plate, along with the Mid-Atlantic Ridge itself, drifted eastward – leaving the (stationary) plume at its current location west of the ridge. Its last eruption may have occurred in the sixteenth century. Due to its short above-water history, its soil consists mostly of clinker.
The island consists of a wide range of alkaline rocks atypical for oceanic islands, ranging from basalt through trachyandesite and trachyte to rhyolite.
Bobowasi Island is located at 04°52'N 02°15'W.
- "Cool Planet | Oxfam Education". Oxfam.org.uk. Archived from the original on 2012-02-06. Retrieved 2013-10-31.
- Bay, Edna (1998). Wives of the Leopard: Gender, Politics, and Culture in the Kingdom of Dahomey. University of Virginia Press.
- Akinjogbin, I.A. (1967). Dahomey and Its Neighbors: 1708–1818. Cambridge University Press. OCLC 469476592.
- Law, Robin (1986). "Dahomey and the Slave Trade: Reflections on the Historiography of the Rise of Dahomey". The Journal of African History 27 (2): 237–267. doi:10.1017/s0021853700036665.
- Creevey, Lucy; Ngomo, Paul; Vengroff, Richard (2005). "Party Politics and Different Paths to Democratic Transitions: A Comparison of Benin and Senegal". Party Politics 11 (4): 471–493. doi:10.1177/1354068805053213.
- Harms, Robert W. (2002). The Diligent: A Voyage Through the Worlds of the Slave Trade. Basic Books. p. 172. ISBN 978-0-465-02872-6. Archived from the original on 9 May 2016. Retrieved 12 October 2015.
- Alpern, Stanley B. (1998). Amazons of Black Sparta: The Women Warriors of Dahomey. C. Hurst & Co. Publishers. p. 37. ISBN 978-1-85065-362-2. Archived from the original on 6 May 2016. Retrieved 12 October 2015.
- Chisholm (1911).
- EB (1878).
- "Limits of Oceans and Seas, 3rd ed." (PDF). International Hydrographic Organization. 1953. Retrieved 7 February 2010..
- "Satellite View and Map of São Tomé and Príncipe" Nations Online. Retrieved 2014-9-26.
- Projecção a nível distrital 2012 - 2020, Instituto Nacional de Estatística
- Instituto Nacional de Estatística.
- Sailing Directions (Enroute), Pub. 123: Southwest Coast of Africa (PDF). Sailing Directions. United States National Geospatial-Intelligence Agency. 2017. p. 74.
- McNeil Jr, Donald G. (16 September 2010). "Precursor to H.I.V. Was in Monkeys for Millenniums, Study Says". The New York Times.
- Aymemí, R.P Antonio (1942). The History of the Bubis on Fernando Po. Colleen Truelsen (trans.). Imprenta de Galo Saez. Chapter 1.
- Digital.CSIC: Arqueología en el Estuario del Muni (Guinea Ecuatorial)
- Bostoen (K.), Clist (B.), Doumenge (C.), Grollemund (R.), Hombert (J.-M.), Koni Muluwa (J.) & Maley (J.), 2015, Middle to Late Holocene Paleoclimatic Change and the Early Bantu Expansion in the Rain Forests of Western Central Africa, Current Anthropology, 56 (3), pp.354-384.
- Clist (B.). 1990, Des derniers chasseurs aux premiers métallurgistes : sédentarisation et débuts de la métallurgie du fer (Cameroun, Gabon, Guinée-Equatoriale). In Lanfranchi (R.) & Schwartz (D.) éds. Paysages quaternaires de l'Afrique Centrale Atlantique. Paris : ORSTOM, Collection didactiques : 458-478
- Clist (B.). 1998. Nouvelles données archéologiques sur l'histoire ancienne de la Guinée-Equatoriale. L'Anthropologie 102 (2) : 213-217
- DeLancey and DeLancey 2.
- "Cameroon". US Department of State. 25 August 2011. Retrieved 24 September 2011.
- Njung, GN, Lucas Tazanu Mangula, and Emmanuel Nfor Nkwiyir (2003). Introduction to History: Cameroon. ANUCAM, pp. 5–6.
- "Central African foragers" is used (in some cases alongside "pygmies") in e.g.: Susan Kent, Cultural Diversity Among Twentieth-Century Foragers: An African Perspective (2006); Richard Bradshaw, Juan Fandos-Rius, Historical Dictionary of the Central African Republic (2016), p. 11; Schlebusch et al. (2017). "[African] rainforest hunter-gatherers" is used in population genetics from c. 2015, Fagny, Maud; Patin, Etienne; MacIsaac, Julia L; Rotival, Maxime; Flutre, Timothée; Jones, Meaghan J; Siddle, Katherine J; Quach, Hélène et al. (2015). "The epigenomic landscape of African rainforest hunter-gatherers and farmers". Nature Communications 6: 10047. doi:10.1038/ncomms10047. PMID 26616214. PMC 4674682. //www.ncbi.nlm.nih.gov/pmc/articles/PMC4674682/. The alternative "Forest People [of Central Africa]" sees limited use in the early 2000s, e.g. Racism Against Indigenous Peoples, International Work Group for Indigenous Affairs (2001), p. 312. Thomas Widlok, Wolde Gossa Tadesse (eds.), Property and Equality vol. 2 (2005), p. 104.
- Thomas, Katie (March 12, 2007). "Congo's Pygmies live as slaves". The News & Observer. Archived from the original on 2009-02-28. Kristof, Nicholas D. (June 16, 1997). "As the World Intrudes, Pygmies Feel Endangered". New York Times.
- "Background Note: Republic of the Congo". Department of State. March 2009. Retrieved 25 June 2017.
- "Katanda Bone Harpoon Point | The Smithsonian Institution's Human Origins Program". Humanorigins.si.ed. Archived from the original on 2 March 2015. Retrieved 10 March 2015.
- Yellen, John E. (1 September 1998). "Barbed Bone Points: Tradition and Continuity in Saharan and Sub-Saharan Africa". African Archaeological Review 15 (3): 173–98. doi:10.1023/A:1021659928822.
- Retrieved 4 June 2007. Ukerewe Island in neighbouring Lake Victoria is considerably bigger than Idjwi, at 530 km2 (205 sq mi).
- Newbury, David S. (1991). Kings and Clans: Ijwi Island and the Lake Kivu Rift, 1780-1840. Univ of Wisconsin Press. p. 239. ISBN 9780299128944.
- East Africa Living Encyclopedia
- World Atlas website: Islands of the World: Largest Lake Islands. Retrieved 4 June 2007.
- Mwanza Guide: Ukerewe.
- Howden, Daniel (2008-12-08). "Albinos slaughtered for body parts by black magic witchdoctors". Belfast Telegraph. Retrieved 2019-06-03.
- Tishkoff, S. A.; Reed, F. A.; Friedlaender, F. R.; Ehret, C.; Ranciaro, A.; Froment, A.; Hirbo, J. B.; Awomoyi, A. A. et al. (2009). "The Genetic Structure and History of Africans and African Americans". Science 324 (5930): 1035–44. doi:10.1126/science.1172257. PMID 19407144. PMC 2947357. //www.ncbi.nlm.nih.gov/pmc/articles/PMC2947357/.
- Christopher Ehret (2001). An African Classical Age: Eastern and Southern Africa in World History, 1000 B.C. to A.D. 400. University Press of Virginia. ISBN 978-0-8139-2057-3.
- Joseph Bindloss, Tom Parkinson, Matt Fletcher, Lonely Planet Kenya, (Lonely Planet: 2003), p.35.
- (PDF). 13 August 2011 https://web.archive.org/web/20110813010018/http://www.kenyacommunities.org/articles%26downloads/KENYA.pdf. Missing or empty
- Arnold Curtis, Kenya: a visitor's guide, (Evans Brothers: 1985), p.7.
- Peak Revision K.C.S.E. History & Government. East African Publishers.
- Iron Working In The Upper Tana pg 3,July 2013 (PDF).
- John & Mbiti 1990
- Hashim, Nadra O. (2009). Language and Collective Mobilization: The Story of Zanzibar. Lexington Books. p. xi. ISBN 978-0-7391-3708-6.
- Peter Robertshaw (1990). A History of African Archaeology. J. Currey. p. 105. ISBN 978-0-435-08041-9.
- Brandt, S. A. (1988). "Early Holocene Mortuary Practices and Hunter-Gatherer Adaptations in Southern Somalia". World Archaeology 20 (1): 40–56. doi:10.1080/00438243.1988.9980055. PMID 16470993.
- H. W. Seton-Karr (1909). Prehistoric Implements From Somaliland. 9. Man. pp. 182–183. https://archive.org/stream/mananth9a10royauoft/mananth9a10royauoft_djvu.txt. Retrieved 30 January 2011.
- Zarins, Juris (1990), "Early Pastoral Nomadism and the Settlement of Lower Mesopotamia", (Bulletin of the American Schools of Oriental Research)
- Diamond J, Bellwood P (2003) "Farmers and Their Languages: The First Expansions" Science 300, doi:10.1126/science.1078208
- Bakano, Otto (24 April 2011). "Grotto galleries show early Somali life". Agence France-Presse. Archived from the original on 21 September 2013. Retrieved 11 May 2013.
- Mire, Sada (2008). "The Discovery of Dhambalin Rock Art Site, Somaliland". African Archaeological Review 25 (3–4): 153–168. doi:10.1007/s10437-008-9032-2. Archived from the original on 27 June 2013. https://web.archive.org/web/20130627100400/http://www.mbali.info/doc494.htm. Retrieved 22 June 2013.
- Alberge, Dalya (17 September 2010). "UK archaeologist finds cave paintings at 100 new African sites". The Guardian. Retrieved 25 June 2013.
- Hodd, Michael (1994). East African Handbook. Trade & Travel Publications. p. 640. ISBN 0-8442-8983-3.
- Ali, Ismail Mohamed (1970). Somalia Today: General Information. Ministry of Information and National Guidance, Somali Democratic Republic. p. 295.
- Kalpana Ram (1993). Mukkuvar Women. Macquarie University.
- Xavier Romero-Frias, The Maldive Islanders, A Study of the Popular Culture of an Ancient Ocean Kingdom
- Ellis, Royston (2008). Maldives. Bradt Travel Guides. ISBN 9781841622668.
- Maloney, Clarence. "Maldives People". International Institute for Asian Studies. Retrieved 22 June 2008.
- BPS Kabupaten Simeulue (2003). Simeulue Dalam Angka 2012. BadanPusatStatistik.Com. ISBN 978-0-0100-0021-4.
- Suhadi Hadiwinoto (2008). Nias, dari masa lalu ke masa depan. Badan Pelestarian Pusaka Indonesia. ISBN 9791801916.
- Österreichische Leo-Gesellschaft, Görres-Gesellschaft, Anthropos Institute (1984). Anthropos, Volume 79. Zaunrith'sche Buch-, Kunst- und Steindruckerei.CS1 maint: Multiple names: authors list (link)
- "Native People of Nias Island". Pleasure Surf Camp. 18 October 2014. Retrieved 2016-12-14.
- Papers, Issues 41-46. Kroeber Anthropological Society. 1969.
- "Jejak Manusia Pertama Sumatera Utara Ada Di Pulau Nias". Tempo.Co. Retrieved 12 July 2014.
- "Unexpected island Effects At An Extreme: Reduced Y-Chromosome And Mitochondrial DNA Diversity In Nias". Oxford Journals. Retrieved 12 July 2014.
- "Asal-Usul Orang Nias Ditemukan". Kompas.Com. Retrieved 12 July 2014.
- "Merunut Asal-Usul Orang Nias Berdasarkan DNA/Gen". Nias Online. Retrieved 12 July 2014.
- "MTidak Ada Kepentingan Komersial dan Tidak Ada Hak Paten Yang Akan Diajukan". Nias Online. Retrieved 12 July 2014.
- Gavin W. Jones, Chee Heng Leng & Maznah Mohamad (2009). Muslim-Non-Muslim Marriage: Political and Cultural Contestations in Southeast Asia. Institute of Southeast Asian Studies. ISBN 98-123-0874-1.
- Asian Development Bank (2010). Complaint Handling in the Rehabilitation of Aceh and Nias: Experiences of the Asian Development Bank and Other Organizations. Asian Development Bank. ISBN 92-925-4734-8.
- Sibeth, Achim; Carpenter, Bruce W.; Meyers, Koen (2013). Nias Sculpture: Mandala Collection. Red & White Publishing. ISBN 9789791008723.
- "Nias Customs". Nias Heritage Museum. Yayasan Pusaka Nias. 2017. Retrieved June 20, 2018.
- Lase, Apolonius (2011). Kamus Liniha Nias - Indonesia. Penerbit Buku Kompas. ISBN 9789797095413.
- Volkenkundig Museum Nusantara (1990). Nias: tribal treasures: cosmic reflections in stone, wood, and gold. Delft: Volkenkundig Museum Nusantara. ISBN 9789071423055.
- Drakard, Jane (1999). A Kingdom of Words: Language and Power in Sumatra. Oxford University Press. ISBN 983-56-0035-X.
- Munoz. Early Kingdoms. p. 175.
- Marsden, William (1783). The history of Sumatra. Dutch: Longman. p. 5.
- Cribb, Robert (2013). Historical Atlas of Indonesia. Routledge. p. 249.
- "Submission on Development Potential No. 37" (PDF). Northern Australia Land and Water Taskforce. 16 August 2007. Archived from the original (PDF) on 20 May 2009. Retrieved 26 April 2009.
- "Christmas island". World Factbook. CIA. 23 April 2009. Retrieved 26 April 2009.
- "Christmas Islands Hidden Secret". Advanced Diver Magazine. 2016. http://www.advanceddivermagazine.com/articles/christmasisland.html. Retrieved 2016-01-02.
- II.—A Monograph of Christmas Island (Indian Ocean: Physical Features and Geology). By C. W. Andrews. With descriptions of the fauna and flora by numerous contributors. 8vo; pp. xiii, 337, 22 plates, 1 map, text illustrated.(London : printed by order of the Trustees of the British Museum, 1900.)
- Geoscience Australia. "Remote Offshore Territories". Retrieved 20 January 2018.
- Kuoni – Far East, A world of difference. Kuoni Travel & JPM Publications. 1999.
- Hidayat, Rafki (7 June 2017). Indonesia counts its islands to protect territory and resources. BBC. Retrieved 5 July 2017.
- The World Factbook: Indonesia. Central Intelligence Agency. 12 December 2017. Retrieved 19 December 2017.
- Choi, Kildo; Driwantoro, Dubel (2007). "Shell tool use by early members of Homo erectus in Sangiran, central Java, Indonesia: cut mark evidence". Journal of Archaeological Science 34: 48. doi:10.1016/j.jas.2006.03.013.
- Finding showing human ancestor older than previously thought offers new insights into evolution. TerraDaily. 5 July 2011. Retrieved 29 January 2012.
- Pope, G.G. (1988). "Recent advances in far eastern paleoanthropology". Annual Review of Anthropology 17: 43–77. doi:10.1146/annurev.an.17.100188.000355. cited in Whitten, T.; Soeriaatmadja, R.E.; Suraya, A.A. (1996). The Ecology of Java and Bali. Hong Kong: Periplus Editions. pp. 309–412.; Pope, G.G. (1983). "Evidence on the age of the Asian Hominidae". Proceedings of the National Academy of Sciences of the United States of America 80 (16): 4988–4992. doi:10.1073/pnas.80.16.4988. PMID 6410399. PMC 384173. //www.ncbi.nlm.nih.gov/pmc/articles/PMC384173/. ; de Vos, J.P.; Sondaar, P.Y. (1994). "Dating hominid sites in Indonesia". Science 266 (16): 4988–4992. doi:10.1126/science.7992059.
- Gugliotta, Guy (July 2008). The Great Human Migration. Smithsonian Maganize. Retrieved 21 August 2011.
- Taylor 2003, pp. 5–7.
- Taylor 2003, pp. 8–9.
- Taylor 2003, pp. 15–18.
- Taylor 2003, pp. 3, 9–11, 13–5, 18–20, 22–3.
- Vickers 2005, pp. 18–20, 60, 133–4.
- Taylor, Jean Gelman (2003). Indonesia: Peoples and Histories. New Haven and London: Yale University Press. p. 378. ISBN 978-0-300-10518-6.
- Gary Holton; Laura C. Robinson (2014). "The linguistic position of the Timor-Alor-Pantar languages". In Klamer, Marian (ed.). The Alor-Pantar languages.
- Lewis, M. Paul; Gary F. Simons; Charles D. Fennig, eds. (2015). Ethnologue: Languages of the World (18th ed.). Dallas, Texas: SIL International.CS1 maint: Uses editors parameter (link)
- Central Intelligence Agency (2015). "Nauru". The World Factbook. Archived from the original on 17 September 2008. Retrieved 8 June 2015. 
- "U.S. Relations With Nauru".
- Google Map Developers. "Distance Finder". Archived from the original on 22 August 2017. Retrieved 9 April 2017.
- Thaman, RR; Hassall, DC. "Nauru: National Environmental Management Strategy and National Environmental Action Plan" (PDF). South Pacific Regional Environment Programme. p. 234. Archived (PDF) from the original on 11 May 2012. Retrieved 18 June 2012.
- Jacobson, Gerry; Hill, Peter J; Ghassemi, Fereidoun (1997). "24: Geology and Hydrogeology of Nauru Island". In Vacher, H Leonard; Quinn, Terrence M (eds.). Geology and hydrogeology of carbonate islands. Elsevier. p. 716. ISBN 978-0-444-81520-0.
- Dahl, Arthur (July 12, 1988). "Islands of Kiribati". Island Directory. UN System-Wide Earthwatch Web Site. Retrieved April 14, 2012.
- "19. Banaba" (PDF). Office of Te Beretitent - Republic of Kiribati Island Report Series. 2012. Retrieved 28 April 2015.
- C.Michael Hogan. 2011. Phosphate. Encyclopedia of Earth. Topic ed. Andy Jorgensen. Ed.-in-Chief C.J.Cleveland. National Council for Science and the Environment. Washington DC |url=https://web.archive.org/web/20121025180158/http://www.eoearth.org/article/Phosphate?topic=49557 |date=October 25, 2012 }}
- Sigrah, Raobeia Ken, and Stacey M. King (2001). Te rii ni Banaba.. Institute of Pacific Studies, University of the South Pacific, Suva, Fiji. ISBN 982-02-0322-8.
- "Banaba: The island Australia ate". Radio National. 2019-05-30. Retrieved 2019-06-06.
- Dr Temakei Tebano & others (September 2008). "Island/atoll climate change profiles - Butaritari Atoll". Office of Te Beretitent - Republic of Kiribati Island Report Series (for KAP II (Phase 2). Archived from the original on November 6, 2011. Retrieved 28 April 2015.
- Grimble, Arthur (1981). A Pattern of Islands. Penguin Travel Library. Penguin Books. ISBN 0-14-009517-9.
- Grimble, Arthur (1989). Tungaru traditions: writings on the atoll culture of the Gilbert Islands. Penguin Travel Library. University of Hawaii Press. ISBN 978-0-8248-1217-1.
- "Kiribati Census Report 2010 Volume 1" (PDF). National Statistics Office, Ministry of Finance and Economic Development, Government of Kiribati. Archived from the original (PDF) on 10 August 2014. Retrieved 17 March 2013.
- "1. Makin" (PDF). Office of Te Beretitent - Republic of Kiribati Island Report Series. 2012. Retrieved 28 April 2015.
- Dr Temakei Tebano & others (August 2008). "Island/atoll climate change profiles - Makin Atoll". Office of Te Beretitent - Republic of Kiribati Island Report Series (for KAP II (Phase 2). Archived from the original on November 6, 2011. Retrieved 28 April 2015.
- Grimble, Arthur (1981). A Pattern of Islands. Penguin Travel Library. Penguin Books. ISBN 0-14-009517-9.
- Grimble, Arthur (1989). Tungaru traditions: writings on the atoll culture of the Gilbert Islands. Penguin Travel Library. University of Hawaii Press. ISBN 978-0-8248-1217-1.
- Canby 1984, p. 1
- Hoiberg 1998, p. 7
- "4. Abaiang" (PDF). Office of Te Beretitent - Republic of Kiribati Island Report Series. 2012. Retrieved 2 May 2015.
- Kiribati National Statistics Office 2012, pp. 36–37
- Kiribati National Statistics Office 2012, p. 223
- Islas de Abaiang |url=https://web.archive.org/web/20151117022742/http://ki.tepuy.org/Islas/Abaiang |date=November 17, 2015 : Eke, Iaia, Iku, Manra, Nanikirata, Ouba, Taete, Teirio
- "Kiribati Census Report 2010 Volume 1" (PDF). National Statistics Office, Ministry of Finance and Economic Development, Government of Kiribati. Archived from the original (PDF) on 2014-08-10.
- Grimble, Arthur (1981). A Pattern of Islands. Penguin Travel Library. Penguin Books. ISBN 0-14-009517-9.
- Return to the Islands (1957), which was republished by Eland, London in 2011, ISBN 978-1-906011-45-1
- Grimble, Arthur (1989). Tungaru traditions: writings on the atoll culture of the Gilbert Islands. Penguin Travel Library. University of Hawaii Press. ISBN 978-0-8248-1217-1.
- "Kiribati government website". Government of Kiribati. Archived from the original on 26 June 2010. Retrieved 29 May 2014.
- "European Union – list of countries in the world".
- "North Tarawa Island Report 2012". Government of Kiribati.
- "South Tarawa Island Report 2012". Government of Kiribati.
- North Tarawa Socioeconomic Report 2008. Secretariat of the Pacific Community and Government of Kiribati
- Howe, K. R. (2006). Vaka Moana – voyages of the ancestors. David Bateman. ISBN 1869536258.
- Dr Temakei Tebano & others (October 2008). "Island/atoll climate change profiles - Marakei Atoll". Office of Te Beretitent - Republic of Kiribati Island Report Series (for KAP II (Phase 2). Archived from the original on November 6, 2011. Retrieved 28 April 2015.
- "Aranuka factsheet". Kiribati Tourism, Government of Kiribati. Archived from the original on 2013-06-21. Retrieved 2013-04-27.
- "Abemama Atoll". Encyclopædia Britannica (15th) I: A-ak Bayes: 27. (2010). Chicago, IL: Encyclopædia Britannica Inc..
- "8. Abemama" (PDF). Office of Te Beretitent - Republic of Kiribati Island Report Series. 2012. Retrieved 28 April 2015.
- Canby. Historic Places. p. 2
- "Geody.com, Abemama". Retrieved 25 April 2013.
- "11. Nonouti" (PDF). Office of Te Beretitent - Republic of Kiribati Island Report Series. 2012. Retrieved 28 April 2015.
- Luomala, Katharine (1980). "Some fishing customs and beliefs in Tabiteuea (Gilbert Islands, Micronesia)". Anthropos 75 (3/4): 523-558.
- "12. Tabiteuea North" (PDF). Office of Te Beretitent - Republic of Kiribati Island Report Series. 2012. Retrieved 28 April 2015.
- "13. Tabiteuea South" (PDF). Office of Te Beretitent - Republic of Kiribati Island Report Series. 2012. Retrieved 28 April 2015.
- Geographic Names Information System. United States Geological Survey 1393033 Howland Island February 24, 2009
- "United States Pacific Island Wildlife Refuges". World Factbook. Central Intelligence Agency. Retrieved 25 June 2019.
- "Howland Island National Wildlife Refuge". Archived from the original on 2015-06-02. Retrieved 2019-03-11.
- Hague, James D. Web copy "Our Equatorial Islands with an Account of Some Personal Experiences."  August 6, 2007 Century Magazine, Vol. LXIV, No. 5, September 1902. Retrieved: January 3, 2008.
- Suárez 2004, p. 17.
- Bryan, E.H. "Sydney Island." janeresture.com. Retrieved: July 7, 2008.
- Irwin 1992, pp. 176–179.
- Stevenson, Robert Louis (August 1998) [letter: 2 December 1889]. "Chapter 13, Part V". Letters of Robert Louis Stevenson (e-book). 2. Seattle, Washington, USA.: The World Wide SchoolTM.
- Denger, Otto; Gillaspy, Edwin (August 15, 1955). Atoll Research Bulletin, Canton Island, South Pacific (PDF). 41. Washington DC: Pacific Science Board, National Academy of Sciences-National Research Council. p. 6. Retrieved 2008-12-17.
The whaler 'Phoenix' discovered Winslow Reef, northwest of Canton, in 1851, and the name of this vessel became attached to the entire group of islands.
- Ships' Log Collection, Phoenix, Nov. 7, 1848 – Feb. 5, 1853. In the Nantucket Historical Association, Resource Library and Archives. 
- "The Earhart Project". TIGHAR. Retrieved July 15, 2011.
- "The 70th Anniversary Expedition". TIGHAR. Retrieved July 15, 2011.
- "McKean Island, Phoenix Group". Jane's Oceania Home Page. Jane Resture. September 28, 2008. Retrieved July 15, 2011.
- Mike Pearson; Jonathan Willis-Richards. "Islands of Kiribati". Retrieved 2007-02-21.
- W. J. L. Wharton (May 26, 1903). "Notices to Mariners". London Gazette. London. Retrieved 2015-12-27.
- Kiribati. CIA World Factbook.
- Maslyn Williams & Barrie Macdonald (1985). The Phosphateers. Melbourne University Press. ISBN 0-522-84302-6.
- Albert Fuller Ellis (1935). Ocean Island and Nauru; Their Story. Sydney, Australia: Angus and Robertson, limited. OCLC 3444055.
- Thomas, Frank R. (2003). "Kiribati: 'Some aspects of human ecology,' forty years later". Atoll Research Bulletin (Natural Museum of Natural History Smithsonian Institution) 501: 1–40. doi:10.5479/si.00775630.501.1. http://www.sil.si.edu/DigitalCollections/AtollResearchBulletin/issues/00501.pdf.
- Harris, Aimee (April 1999). Millennium: Date Line Politics, In: Honolulu Magazine. Retrieved 14 June 2006.
- "Hull Island, Phoenix Group, Republic of Kiribati". Jane's Oceania Home Page. Jane Resture. Retrieved July 15, 2011.
- Resture, Jane. "Canton Island (Kanton - Abariringa) Phoenix Group, Kiribati". Retrieved 25 January 2015.
- "Archived copy" (PDF). Archived from the original (PDF) on 13 September 2006. Retrieved 13 September 2006.CS1 maint: Archived copy as title (link), p. 2.
- "World Port Index" (PDF).
- Resture, Jane. "Birnie Island, Phoenix Group". Jane Resture. Retrieved 25 January 2015.
- "Sydney Island, Phoenix Group, Republic of Kiribati". Jane's Oceania Home Page. Jane Resture. September 28, 2008. Retrieved July 15, 2011.
- "Rawaki Islands – Rawaki". Oceandots.com. July 24, 2001. Archived from the original on December 23, 2010. Retrieved July 15, 2011.
- "Phoenix Island, Phoenix Group, Republic of Kiribati". Jane's Oceania Home Page. Jane Resture. Retrieved July 15, 2011.
- Darwin, Charles; Bonney, Thomas George (1897). The structure and distribution of coral reefs. New York: D. Appleton and Company. p. 207. ISBN 978-0-520-03282-8.
- "Jarvis Island". DOI Office of Insular Affairs. Retrieved January 26, 2007.
- Hiroa, Te Rangi (Sir Peter Henry Buck) (1964). Vikings of the Sunrise. NZ Electronic Text Centre, Victoria University, NZ Licence CC-BY-SA 3.0 (reprint ed.). Whitcombe and Tombs Ltd. p. 67. Retrieved 2 March 2010.
- Crowe, Andrew (2018). Pathway of the Birds: The Voyaging Achievements of Māori and their Polynesian Ancestors. Auckland, New Zealand: Bateman. p. 62-64. ISBN 9781869539610.
- Living Archipelagos: Malden Island. https://web.archive.org/web/20070105145111/http://www.livingarchipelagos.org/sitepage.asp?name=Malden 5 January 2007 Retrieved on 7 July 2008.
- Bryan, E.H. Malden Island. Retrieved on 7 July 2008.
- Heyerdahl, Thor; & Skjolsvold, Arne (1956). "Archaeological Evidence of Pre-Spanish Visits to the Galápagos Islands", Memoirs 12, Society for American Archaeology.
- Lundh, Jacob (1995). "A brief account of some early inhabitants of Santa Cruz Island." In Noticias de Galápagos No. 55. Charles Darwin Foundation for the Galápagos Islands.
- Cho, Lisa (2005) Moon Galápagos Islands. Avalon Travel Publishing. p. 200. ISBN 163121151X.
- Correal, Urrego G. (1993). "Nuevas evidencias culturales pleistocenicas y megafauna en Colombia". Boletin de Arqueologia (8): 3–13.
- Hoopes, John (1994). "Ford Revisited: A Critical Review of the Chronology and Relationships of the Earliest Ceramic Complexes in the New World, 6000-1500 B.C. (1994)". Journal of World Prehistory 8 (1): 1–50. doi:10.1007/bf02221836.
- Van der Hammen, T; Correal, G (1978). "Prehistoric man on the Sabana de Bogotá: data for an ecological prehistory". Palaeogeography, Palaeoclimatology, Palaeoecology 25 (1–2): 179–190. doi:10.1016/0031-0182(78)90077-9.
- Broadbent, Sylvia (1965). "Los Chibchas: organización socio-polític". Serie Latinoamericana 5.
- Álvaro Chaves Mendoza; Jorge Morales Gómez (1995). Los indios de Colombia (in Spanish). 7. Editorial Abya Yala. ISBN 978-9978-04-169-7.
- "Historia de Colombia: el establecimiento de la dominación española – Los Pueblos Indígenas del Territorio Colombiano" (in Spanish). banrepcultural.org.
- de Mahecha, Ana María Groot (1988). "Intento de delimitación del territorio de los grupos étnicos Pastos y Quillacingas en el altiplano nariñense." (in Spanish). Boletín de Arqueología de la Fian 3 (3): 3–31. http://publicaciones.banrepcultural.org/index.php/fian/article/view/5130/5381.
- Romero-Figueroa, Andrés. Basic Word Order and Sentence Types in Kari'ña. Meunchen: Lincom Europa 2000
- Carlin, Eithne and Boven, Karen (2002). The native population: Migrations and identities. In: Atlas of the languages of Suriname, Eithne Carlin and Jacques Arends (Eds.) Leiden: KITLV Press
- Romero, Simon (27 March 2014). "Discoveries Challenge Beliefs on Humans' Arrival in the Americas". New York Times. Retrieved 31 May 2014.
- Mann, Charles C. (2006) . 1491: New Revelations of the Americas Before Columbus. Vintage Books. pp. 326–33. ISBN 978-1-4000-3205-1.
- About.com, http://gobrazil.about.com/od/ecotourismadventure/ss/Peter-Lund-Museum.htm
- Robert M. Levine; John J. Crocitti (1999). The Brazil Reader: History, Culture, Politics. Duke University Press. pp. 11–. ISBN 978-0-8223-2290-0. Retrieved 12 December 2012.
- Science Magazine, 13 December 1991 http://www.sciencemag.org/content/254/5038/1621.abstract
- Levine, Robert M. (2003). The History of Brazil. Palgrave Macmillan. p. 32. ISBN 978-1-4039-6255-3.
- Levine (2003), p. 31.
- Fausto, Carlos (2000). Zahar, Jorge (ed.). Os Índios antes do Brasil [The Indians before Brazil] (in Portuguese). pp. 45–46, 55. ISBN 978-85-7110-543-0.
- Gomes, Mercio P. The Indians and Brazil University Press of Florida 2000 ISBN 0-8130-1720-3 pp. 28–29
- Fausto (2000), pp. 78–80.
- Fausto (2000), p. 50.
- Araujo Costa, Costa. (2014). "Marajó". Grove Art Online. Oxford, UK: Oxford University Press. Retrieved on 17 December 2014.
- Mann, Charles C. (2006-10-10). 1491 (Second Edition): New Revelations of the Americas Before Columbus. Knopf Doubleday Publishing Group. pp. 328–340. ISBN 9780307278180.
- Mann, Charles C. (2006-01-01). 1491: New Revelations of the Americas Before Columbus. Vintage Books. p. 335. ISBN 9781400032051.
- "The geology of Ascension Island". Ascension Island Volcanology. 25 October 2017. Archived from the original on 5 January 2018. Retrieved 5 January 2018.
- Detailed description of the BBC Atlantic Relay Station