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Alofaaga Blowholes
The Alofaaga Blowholes, also known as the Taga Blowholes, are a natural feature located in the district of Palauli, south west of Salelologa wharf on the island of Savai'i in Samoa. The entrance to the blowholes is in the village of Taga. In this area, lava flows have created a series of tubes connecting a flat clifftop of lava rock with the ocean below. Waves breaking against the lower end of the lava tubes send water at high pressure up through the tubes, creating fountains that spray every few seconds. As most of the land in Samoa is under customary ownership, the village charges a small admission for entry to view the blowholes. The area is unfenced and surrounded by wet, slippery rocks which can be dangerous. Falling into one of the blowholes would be almost certainly fatal. A track along the coast can be followed west to the ancient village of Fagaloa. Gallery File:Blowholes Savai'i 2009.jpg File:Samoa Blowholes.JPG See also * Piula Cave Pool * Mata o le Alelo Pool ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palauli
Palauli is a district and village of Samoa, with a population (2016 Census) of 9,300. It consists of two sections on the southern side of Savai'i. The capital is Vailoa which is also referred to as Vailoa i Palauli (Vailoa in Palauli district). Geological formations of lava tubes have created the Taga Blowholes on the coast of Taga village and attracts visitors and tourists. In recent years, the inland village of Sili has refused to let the government of Samoa build a hydroelectric power plant on traditional land due to conservation and cultural concerns. The paramount title of this district is Lilomaiava, which is conferred in Vailoa. As part of the selection process for the title-holder, Vailoa must consult Safotu village in the Gagaifomauga political district. Safotu is the northern base of the Lilomaiava title in Savai'i. Archaeology Extensive pre-historic settlements have been surveyed and studied in the Palauli district where the Pulemelei Mound is situated. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salelologa
Salelologa is a village district at the east end of Savai'i island in Samoa. It is the main entry point into the island with the only ferry terminal on Savai'i. It also serves as the main township for shopping and public amenities with a market selling fresh produce and arts and crafts. Salelologa is made up of smaller sub-villages ''pito nu'u'' and falls within the electoral district of Fa'asaleleaga. Township The township consists of one main shopping street. Fresh fish, locally grown produce and arts and crafts are sold at the Salelologa Market (''makeki'') which was recently moved to a new site by the wharf in 2009. The market is open six days a week, Monday to Saturday. Most shops and markets in Samoa close on Sundays with a few small outlets opening in the late afternoon. There are also several small supermarkets, a wholesaler, petrol stations, bakeries such as Retzlaff's bakery, budget hotels and accommodation, as well as public amenities such as internet access, banks an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wharf
A wharf, quay (, also ), staith, or staithe is a structure on the shore of a harbour or on the bank of a river or canal where ships may dock to load and unload cargo or passengers. Such a structure includes one or more berths (mooring locations), and may also include piers, warehouses, or other facilities necessary for handling the ships. Wharves are often considered to be a series of docks at which boats are stationed. Overview A wharf commonly comprises a fixed platform, often on pilings. Commercial ports may have warehouses that serve as interim storage: where it is sufficient a single wharf with a single berth constructed along the land adjacent to the water is normally used; where there is a need for more capacity multiple wharves, or perhaps a single large wharf with multiple berths, will instead be constructed, sometimes projecting over the water. A pier, raised over the water rather than within it, is commonly used for cases where the weight or volume of cargos will b ... [...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] |
Taga, Samoa
Taga is a village on the island of Savai'i in Samoa. It is situated on the south coast of the island in the district of Palauli Palauli is a districts of Samoa, district and village of Samoa, with a population (2016 Census) of 9,300. It consists of two sections on the southern side of Savai'i. The capital is Vailoa which is also referred to as Vailoa i Palauli (Vailoa in P ... and the electoral district of Palauli 1. The population is 785. Geological formations have created the Taga blowholes on the coast. References Populated places in Palauli {{Samoa-geo-stub ... [...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] |
Lava Tube
A lava tube, or pyroduct, is a natural conduit formed by flowing lava from a volcanic vent that moves beneath the hardened surface of a lava flow. If lava in the tube empties, it will leave a cave. Formation A lava tube is a type of lava cave formed when a low-viscosity lava flow develops a continuous and hard crust, which thickens and forms a roof above the still-flowing lava stream. Tubes form in one of two ways: either by the crusting over of lava channels, or from pāhoehoe flows where the lava is moving under the surface. Lava usually leaves the point of eruption in channels. These channels tend to stay very hot as their surroundings cool. This means they slowly develop walls around them as the surrounding lava cools and/or as the channel melts its way deeper. These channels can get deep enough to crust over, forming an insulating tube that keeps the lava molten and serves as a conduit for the flowing lava. These types of lava tubes tend to be closer to the lava erupt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fagaloa
Afagaloa is a village on the island of Savai'i in Samoa. It is situated on the south coast of the island in the electoral constituency (''faipule district'') of Palauli West which is part of the larger political district of Palauli Palauli is a district and village of Samoa, with a population (2016 Census) of 9,300. It consists of two sections on the southern side of Savai'i. The capital is Vailoa which is also referred to as Vailoa i Palauli (Vailoa in Palauli district). .... References Populated places in Palauli {{Samoa-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Piula Cave Pool
Piula Cave Pool (also known as Fatumea Pool) is a natural freshwater pool by the sea beneath the historic Methodist Chapel at Piula on the north coast of Upolu island in Samoa. It is situated at Lufilufi in the political district of Atua, 26 km east from the capital Apia, along the scenic coastal road. Entry is by the main road through the painted stone wall of Piula Theological College with steps leading down to the pool. A popular swimming hole for locals and visitors, the pool is formed by a natural spring flowing out of a cave and out to sea. Inside the main cave opening on the north side is a short submerged tunnel leading to a smaller cave opening on the east side of the pool. It is open Mondays to Saturdays and there are small ''fale'' and changing rooms for visitors. The monastery charges a small visitor's fee. Freshwater pools are fairly common around the coastlines of Savai'i and Upolu islands which were formed from volcanic activity. Cooling lava flows from volca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mata O Le Alelo
Mata o le Alelo is a village pool in Samoa associated with the Polynesian legend Sina and the Eel. Mata o le Alelo is in the small village of Matavai, in the village district Safune on the central north coast of Savai'i island in Samoa. The pool is fed by a freshwater spring which flows out towards the sea. The underground spring discharges into a pool that is about 500mm above sea level. Water can be seen boiling up to the surface at one end of the pool. Preliminary Water Resource Investigations, Savai'i, Samoa by Ed Burke and David Scott, 1998, funded by SOPAC & CFTC. Retrieved 31 October 2009 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Falemauga Caves
The Falemauga Caves are large natural caverns in a series of lava-tunnels situated in the Tuamasaga district along the central ridge of Upolu island in Samoa. The caves have been studied by archaeologists in Samoa with evidence of human occupation in pre-history. They were also used as a place of refuge by the people of Tuamasaga. The caves were explored and excavated in the early 1940s by New Zealand anthropologist Derek Freeman who published his report in the Journal of the Polynesian Society in 1944. Platforms constructed of stacked rocks, charcoal, stone adzes and marine shells were found in the caves. In the Samoan language, the name ''Falemauga'' can be broken down into two words, ''fale'' which means 'house' and ''mauga'' which means 'mountain.' Location The Falemauga Caves are located in an inland area called Falemauga, about 6 miles south west from Apia, Samoa's capital. Entrance to the main system of tunnels is about five and a half miles south (inland) of the coas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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