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Saleaula
Sale'aula is a village on the central north coast of Savai'i island in Samoa and is the traditional center of the Gaga'emauga political district. Chief council meetings are held at Vaitu’utu’u malae in the village. The village has a population of 600. Volcanic eruptions Volcanic eruptions of Mt Matavanu (1905 - 1911) in central Savai'i swept northwards towards the coast and destroyed villages in its path. The lava flowed over of countryside to the sea and also destroyed another village Salago. The depth of the lava flow in some parts was 400 feet. A Catholic church and a meetinghouse of the LDS Church were also buried. Sale'aula land was covered by lava that reached other villages to the east including Mauga and Samalae'ulu. The colonial German administration acquired land on the main island Upolu and resettled villagers at Salamumu and Leauva'a. Today, those villagers are still part of the Gaga'emauga electoral district on Savai'i. Today, a few families have r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salamumu
Salamumu is a village on the south west coast of Upolu island in Samoa. The village has two settlements, Salamumu Uta (population 338) and Salamumu Tai (population 33). The village's name is derived from the words ''sala'' (fire) and ''mumu'' (punishment), and refers to its origin when people from Sale'aula were relocated to Upolu during the 1905—1911 eruption of Mt Matavanu. Although the village, area 13.11 km2, is geographically located on Upolu, the village is politically (and historically) part of the Gaga'emauga electoral district on the island of Savai'i. The people of Salamumu still have strong kinship cultural ties to their land on Savai'i. Le'auva'a is another settlement on Upolu island which was also relocated from Savai'i following the volcanic eruptions. Climate Salamumu has a tropical rainforest climate A tropical rainforest climate, humid tropical climate or equatorial climate is a tropical climate sub-type usually found within 10 to 15 degrees latitud ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mauga
Mauga is a village in Savai'i island in Samoa. The village is in the Gaga'emauga 1 constituency, a sub-division of the larger Gaga'emauga district. The population is 162. The word ''mauga'' means ''mountain'' in the Samoan language. The settlement is built around the crater of a small volcano. Mauga is in the Gaga'emauga political district near the central north coast of the island. The large meeting houses of the village are situated in a circle facing each other around the rim of the crater which can be seen in high altitude photography. The main island road passes by the village which is situated about a 40-minute drive north west from Salelologa township and ferry terminal. To the southeast is Samalae'ulu village and to the west Saleaula where the main road cuts through large areas of black lava fields. The physical setting of Gaga'emauga I district contains no development along its 10 km coastline, unlike the rest of the island, due to the barren lava cliffs by the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava Fields - Savai'i Island - Samoa
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes'', w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mt Matavanu
Mt Matavanu is an active volcano on the island of Savai'i in Samoa. The volcano was formed during an eruption in 1905. Lava flows from the eruption covered a large area of land in the Gaga'emauga district, leading to the relocation of several villages. The name of the mountain refers to a valley (''vanu'') with an eye-shaped feature (''mata''). In November 2022 Matavanu was recognised by the International Union of Geological Sciences as an international Geological Heritage Site. 1905 - 1911 eruption The eruption began on 4 August 1905, with a new crater being formed nine miles to the east of Mata o le Afi, which had erupted in 1902. An expedition led by governor Wilhelm Solf observed flames shooting 400 feet into the sky at intervals of ten seconds along with lava flowing through the bush. An expedition to examine the crater found "a larger heap of stones about 300ft high, from the top of which, at intervals of about 10 seconds, masses of stone were being thrown up into the air ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Safotulafai
Safotulafai is a traditional village at the east end of Savai'i island with historical and political significance in Samoa's history. It is the traditional center of the island of Savaii, now became the center of Fa'asaleleaga political district. Safotulafai is the original 'Pule', which is why Savaii is called 'Pule' of Samoa. Years later, Safotulafai chose to divide the 'Pule' into six while reserving the right to be the 'Matua' of 'Pule'. Today, Safotulafai remains to be one of the traditional 'Pule' (customary authority) ruling districts of Savai'i. Chief ( ''matai'') council meetings are held at Fuifatu malae. Safotulafai is the village name with its sub-villages: Tuasivi, Fogapoa, Fatausi, Fuifatu, Fusi, and Eveeve. History In the early 1900s, during the time when the country was called German Samoa (1900 - 1914), this is also the place which saw the beginnings of the Mau, Samoa's independence movement. This initial resistance movement against German colonial ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Samoa Time Zone
250px, SST is UTC-11:00 The Samoa Time Zone or Samoa Standard Time (SST) observes standard time by subtracting eleven hours from Coordinated Universal Time ( UTC-11:00). The clock time in this zone is based on the mean solar time of the 165th meridian west of the Greenwich Observatory. The zone includes the U.S. territory of American Samoa, as well as the Midway Islands and the uninhabited islands of Jarvis, Palmyra, and Kingman Reef. It also includes the country of Niue. The zone is one hour behind Hawaii-Aleutian Time Zone and one hour ahead of the Howland and Baker islands, and 23 hours behind Wake Island Time Zone. The nation of Samoa also observed the same time as the Samoa Time Zone until it moved across the International Date Line at the end of 29 December 2011; it is now 24 hours (25 hours in southern hemisphere summer) ahead of American Samoa.{{cite web, url=http://www.heraldsun.com.au/news/breaking-news/samoa-to-move-the-international-dateline/story-e6frf7jx-12260 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcano Eruption Mt Matavanu - Savai'i - 1905 - Photo By Thomas Andrew
A volcano is a rupture in the Crust (geology), crust of a Planet#Planetary-mass objects, planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and volcanic gas, gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where list of tectonic plates, tectonic plates are divergent boundary, diverging or convergent boundary, 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Countries Of The World
The following is a list providing an overview of sovereign states around the world with information on their status and recognition of their sovereignty. The 206 listed states can be divided into three categories based on membership within the United Nations System: 193 member states of the United Nations, UN member states, 2 United Nations General Assembly observers#Present non-member observers, UN General Assembly non-member observer states, and 11 other states. The ''sovereignty dispute'' column indicates states having undisputed sovereignty (188 states, of which there are 187 UN member states and 1 UN General Assembly non-member observer state), states having disputed sovereignty (16 states, of which there are 6 UN member states, 1 UN General Assembly non-member observer state, and 9 de facto states), and states having a political status of the Cook Islands and Niue, special political status (2 states, both in associated state, free association with New Zealand). Compi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
