Mata O Le Afi
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Mata O Le Afi
Mata o le Afi ("Eye of the Fire" or "Source of the Fire") is an active volcano on the island of Savai'i in Samoa. It last erupted in 1902. 1902 eruption An eruption began on 30 October 1902. It was preceded by a series of thirteen earthquakes, which damaged stone churches at Safune Safune is a traditional village district on the central north coast of Savai'i island in Samoa. It lies within the electoral constituency of Gaga'ifomauga. Safune is the birthplace of Mau leader Olaf Frederick Nelson and the filming location o ... and Sasina and destroyed the church at Paia. The inhabitants of these villages and of Aopo fled. On 8 November Dr Otto Tetens examined the volcano, finding a crater a hundred yards across emitting smoke and rocks, with a second crater two miles to the north where the eruption had finished. The eruption had already begun to die down, and ceased around 17 November. References Mountains of Samoa Volcanoes of Samoa Savai'i {{Samoa-geo-stub ...
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Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ...
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Samoa
Samoa, officially the Independent State of Samoa; sm, Sāmoa, and until 1997 known as Western Samoa, is a Polynesian island country consisting of two main islands (Savai'i and Upolu); two smaller, inhabited islands (Manono Island, Manono and Apolima); and several smaller, uninhabited islands, including the Aleipata Islands (Nu'utele, Nu'ulua, Fanuatapu and Namua). Samoa is located west of American Samoa, northeast of Tonga (closest foreign country), northeast of Fiji, east of Wallis and Futuna, southeast of Tuvalu, south of Tokelau, southwest of Hawaii, and northwest of Niue. The capital city is Apia. The Lapita culture, Lapita people discovered and settled the Samoan Islands around 3,500 years ago. They developed a Samoan language and Samoan culture, Samoan cultural identity. Samoa is a Unitary state, unitary Parliamentary system, parliamentary democracy with 11 Administrative divisions of Samoa, administrative divisions. It is a sovereign state and a member of the ...
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Safune
Safune is a traditional village district on the central north coast of Savai'i island in Samoa. It lies within the electoral constituency of Gaga'ifomauga. Safune is the birthplace of Mau leader Olaf Frederick Nelson and the filming location of Moana (1926 film), one of the first documentaries made in the world. The Mata o le Alelo pool associated with the Sina and the Eel Polynesian legend is also in Safune. The villages within Safune are Matavai, Faletagaloa and Fatuvalu as well as smaller traditional land boundaries, Faleolo and Lalomati. Olaf Frederick Nelson Olaf Frederick Nelson, a leader of the Mau, Samoa's independence movement during the colonial era in the early 1900s, was born in Safune on 24 February 1883. Nelson's father was a Swedish immigrant trader. His mother Sina Masoe was from Safune. In 1900, at the age of 17, Nelson worked for his father's store in Safune. When his father retired in 1903, Nelson expanded the family business. In 1904, he purchased a boa ...
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Sasina, Samoa
Sasina is a village on the north coast of Savai'i island in Samoa. It is situated on the central north coast of the island in the district of Gagaʻifomauga and the electoral district of Gagaʻifomauga 3. The population is 568. The village is part of a conservation area which includes the village of Aopo.
Strategies for sustainable development: experiences from the Pacific by John Overton and Regina Scheyvens, p.195
There is a primary school with a new assembly hall renovated by engineers from the United States, Australia and New Zealand under the US Navy's



Aopo
Aopo is a village in the Gaga'ifomauga district on the island of Savai'i in Samoa Samoa, officially the Independent State of Samoa; sm, Sāmoa, and until 1997 known as Western Samoa, is a Polynesian island country consisting of two main islands (Savai'i and Upolu); two smaller, inhabited islands (Manono Island, Manono an .... It is situated inland in the central north of the island in the district of Gagaʻifomauga and the electoral district of Gagaʻifomauga 3. The population is 383. The name of the village is derived from two words, ''ao'' (day) and ''po'' (night) and may be derived from a volcanic eruption. The village is located inland from the north coast of Savai'i, close to the main lava field from the island's volcanic cones. There is an Aopo Conservation Area open to visitors and the trail starts at the east end of the village. Hikers can ascend Mt Silisili, Samoa's highest peak, from Aopo. In 2007, Aopo village sold its teak plantation to Blue Bird Lumber. ...
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Otto Tetens
450px , Otto Tetens (right) with Mataafa in Mulinuu, Samoa 1904 Otto Tetens (26 September 1865, Rendsburg, Kingdom of Prussia – 15 February 1945, Teplitz-Schönau) was a German natural scientist with an astronomy background. Life Tetens was the son of a high ranked police officer in Schleswig, Northern Germany. He went to several universities for different natural science topics in Tübingen, Munich, Berlin and Kiel. After this period, he worked at the private astronomy observatory of Miklos Konkly-Thege in Ogyalla in Hungary. In 1891 he got his Doctor degree of Natural Science. He then worked at different institutes in astronomy such as the Deutsche Seewarte, Hamburg, and the Observatory of Strasbourg. From 1902 to 1905 Otto Tetens worked for the Royal Society of Science of Göttingen on a climate project in Samoa, then a German colony. He founded the Apia Observatory in June 1902 at Mulinuu near the main town of Apia. After his time in Samoa, he went back to Germany and Gö ...
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Mountains Of Samoa
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Volcanoes Of Samoa
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ...
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