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24th Meridian West
The meridian 24° west of Greenwich is a line of longitude that extends from the North Pole across the Arctic Ocean, Greenland, Iceland, the Atlantic Ocean, the Southern Ocean, and Antarctica to the South Pole. The 24th meridian west forms a great circle with the 156th meridian east. From Pole to Pole Starting at the North Pole and heading south to the South Pole, the 24th meridian west passes through: : See also *23rd meridian west *25th meridian west The meridian 25° west of Greenwich is a line of longitude that extends from the North Pole across the Arctic Ocean, Greenland, the Atlantic Ocean, Cape Verde Islands, the Southern Ocean, and Antarctica to the South Pole. The 25th meridian wes ... {{geographical coordinates, state=collapsed w024 meridian west ...
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Prime Meridian
A prime meridian is an arbitrary meridian (a line of longitude) in a geographic coordinate system at which longitude is defined to be 0°. Together, a prime meridian and its anti-meridian (the 180th meridian in a 360°-system) form a great circle. This great circle divides a spheroid, like the Earth, into two hemispheres: the Eastern Hemisphere and the Western Hemisphere (for an east-west notational system). For Earth's prime meridian, various conventions have been used or advocated in different regions throughout history. The Earth's current international standard prime meridian is the IERS Reference Meridian. It is derived, but differs slightly, from the Greenwich Meridian, the previous standard. A prime meridian for a planetary body not tidally locked (or at least not in synchronous rotation) is entirely arbitrary, unlike an equator, which is determined by the axis of rotation. However, for celestial objects that are tidally locked (more specifically, synchronous ...
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Kejser Franz Joseph Fjord
Kaiser Franz Joseph Fjord ( da, Kejser Franz Josef Fjord; kl, Kangerluk Kejser Franz Joseph) is a major fjord system in the NE Greenland National Park area, East Greenland. Geography The Kaiser Franz Joseph Fjord has its mouth in the Foster Bay of the Greenland Sea, between Cape Mackenzie at the eastern end of Geographical Society Island and Cape Franklin, the southern end of the mainland's Gauss Peninsula; Bontekoe Island lies in the bay off its mouth. It extends westwards for about 100 km, then at Eleonore Bay in an NNE/SSW direction for about 32 km, bending again westwards at Cape Mohn, the western end of Ymer Island, branching again with the Isfjord extending northwestwards for over 60 km. Two tributary fjords, the wide Nordfjord —with the large Waltershausen Glacier at its head and the Muskox Fjord ''(Moskusokse Fjord)'' branching eastwards— and the narrower Geologfjord —with the Nunatak Glacier, branch from the northern side of the fjord, abou ...
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Fogo, Cape Verde
Fogo (Portuguese language, Portuguese for "fire") is an island in the Sotavento Islands, Sotavento group of Cape Verde. Its population is 35,837 (2015),Cabo Verde, Statistical Yearbook 2015
Instituto Nacional de Estatística (Cape Verde), Instituto Nacional de Estatística
with an area of 476 km2. It reaches the highest altitude of all the islands in Cape Verde, rising to above sea level at the summit of its active volcano, Pico do Fogo.


History

The eastern side of Fogo collapsed into the ocean 73,000 years ago, creating a tsunami 170 meters high which struck the nearby island of Santiago, Cape Verde, Santiago. Fogo was discovered in 1460 by Genoa, Genovese captain António de Noli on behalf of Henry the ...
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Santiago, Cape Verde
Santiago ( Portuguese for “Saint James”) is the largest island of Cape Verde, its most important agricultural centre and home to half the nation's population. Part of the Sotavento Islands, it lies between the islands of Maio ( to the east) and Fogo ( to the west). It was the first of the islands to be settled: the town of Ribeira Grande (now Cidade Velha and a UNESCO World Heritage Site) was founded in 1462. Santiago is home to the nation's capital city of Praia. History The eastern side of the nearby island of Fogo collapsed into the ocean 73,000 years ago, creating a tsunami 170 meters high which struck Santiago. In 1460, António de Noli became the first to visit the island. Da Noli settled at ''Ribeira Grande'' (now Cidade Velha) with his family members and Portuguese from Algarve and Alentejo in 1462.Valor simb ...
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São Nicolau, Cape Verde
São Nicolau ( Portuguese for ''Saint Nicholas'') is one of the Barlavento (Windward) islands of Cape Verde. It is located between the islands of Santa Luzia and Sal. Its population is 12,424 (2015),Cabo Verde, Statistical Yearbook 2015
with an area of . The main towns are Ribeira Brava and Tarrafal de São Nic ...
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Snæfellsnes
The Snæfellsnes () is a peninsula situated to the west of Borgarfjörður, in western Iceland. The Snæfellsjökull volcano, regarded as one of the symbols of Iceland, can be found in the area. With its height of 1446 m, it is the highest mountain on the peninsula and has a glacier at its peak (''jökull'' means "glacier" in Icelandic). The volcano can be seen on clear days from Reykjavík, a distance of about 120 km. The mountain is also known as the setting of the novel '' Journey to the Center of the Earth'' by the French author Jules Verne. The area surrounding Snæfellsjökull has been designated one of the four National Parks by the government of Iceland. It is also the home of the Ingjaldsholl church, a Protestant church. The peninsula is one of the main settings in the '' Laxdœla saga'' and it was, according to this saga, the birthplace of the first West Norse member of the Varangian Guard, Bolli Bollasson. Other historical people who lived in the area accor ...
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Breiðafjörður
Breiðafjörður (, ''wide fjord'') is a large shallow bay, about 50 km wide and 125 km long, in the west of Iceland. It separates the region of the Westfjords (Vestfirðir) from the Snæfellsnes peninsula to the south. Breiðafjörður is encircled by mountains, including Kirkjufell and the glacier Snæfellsjökull on the Snæfellsnes peninsula, and the Látrabjarg bird cliffs at the tip of the Westfjords. Numerous smaller fjords extend inland from Breiðafjörður, the largest being Hvammsfjörður at its southeastern corner. An interesting feature of the bay is that the land to the north was formed about 15 million years ago, whereas the land to the south was formed less than half that time ago. Nature Breiðafjörður has a spectacular land and seascape consisting of shallow seas, small fjords and bays, and intertidal areas, dotted with about 3,000 islands, islets and skerries. The area contains about half of Iceland's intertidal area and tides can be six met ...
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Westfjords
The Westfjords or West Fjords ( is, Vestfirðir , ISO 3166-2:IS: IS-4) is a large peninsula in northwestern Iceland and an administrative district, the least populous administrative district. It lies on the Denmark Strait, facing the east coast of Greenland. It is connected to the rest of Iceland by a seven-kilometre-wide isthmus between Gilsfjörður and Bitrufjörður . The Westfjords are very mountainous; the coastline is heavily indented by dozens of fjords surrounded by steep hills. These indentations make roads very circuitous and communications by land difficult. In addition many of the roads are closed by ice and snow for several months of the year. The Vestfjarðagöng road tunnel from 1996 has improved that situation. The cliffs at Látrabjarg comprise the longest bird cliff in the northern Atlantic Ocean and are at the westernmost point in Iceland. The Drangajökull glacier is located in the north of the peninsula and is the fifth-largest of the country, but the ...
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Greenland Sea
The Greenland Sea is a body of water that borders Greenland to the west, the Svalbard archipelago to the east, Fram Strait and the Arctic Ocean to the north, and the Norwegian Sea and Iceland to the south. The Greenland Sea is often defined as part of the Arctic Ocean, sometimes as part of the Atlantic Ocean. However, definitions of the Arctic Ocean and its seas tend to be imprecise or arbitrary. In general usage the term "Arctic Ocean" would exclude the Greenland Sea. In oceanographic studies the Greenland Sea is considered part of the Nordic Seas, along with the Norwegian Sea. The Nordic Seas are the main connection between the Arctic and Atlantic oceans and, as such, could be of great significance in a possible shutdown of thermohaline circulation. In oceanography the Arctic Ocean and Nordic Seas are often referred to collectively as the "Arctic Mediterranean Sea", a marginal sea of the Atlantic. The sea has Arctic climate with regular northern winds and temperatures rare ...
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Scoresby Sund
Scoresby Sound (Danish: ''Scoresby Sund'', Greenlandic: ''Kangertittivaq'') is a large fjord system of the Greenland Sea on the eastern coast of Greenland. It has a tree-like structure, with a main body approximately Scoresby Sund
Encyclopædia Britannica on-line
long that branches into a system of s covering an area of about . The longest of the fjords extends 340–350 km (210-216 mi) inland from the coastline. The depth is 400–600 m (1,310-1,970 ft) in the main basin, but depths increase to up to in some fjords. It is one of the largest and longest fjord systems in the world.Archaeology, p. 7 On the northern side of the mouth of the Scores ...
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Jameson Land
Jameson Land is a peninsula in eastern Greenland. Geography Jameson Land is bounded to the southwest by Scoresby Sound (the world's largest fjord), to the northwest by the Stauning Alps, to the north by Scoresby Land, to the northeast by the Fleming Fjord and the Nathorst Fjord of the Greenland Sea, and to the east by Carlsberg Fjord, the smaller Liverpool Land peninsula branching off, and Hurry Inlet. Its northeastern end is Cape Biot. The Mestersvig military base is located in the northern part of the peninsula. Geology Jameson Land mainly consists of a tilted peneplain of Jurassic sandstone, highest in the east. In the northern end there are also rocks of Triassic age. Two formations are predominant in Jameson Land: the Triassic Fleming Fjord Formation and the Jurassic Kap Stewart Formation. Triassic fossils of the Fleming Fjord Formation in Jameson Land include: the dipnoi Ceratodus, prosauropod and theropod dinosaurs bones and tracks, sauropod tracks, phytosaurs, temno ...
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King Oscar Fjord
King Oscar Fjord ( da, Kong Oscar Fjord) is a fjord in East Greenland, marking the northern border of the Scoresby Land Peninsula. It was named by A.G. Nathorst on his 1899 expedition as ''Konung Oscars Fjord'' for Oscar II, King of Sweden from 1872 to 1907 and of Norway from 1872 until 1905. Geography King Oscar Fjord is a major fjord system in NE Greenland. The main fjord is 10–25 km wide, bounded by Traill Island and Geographical Society Island in the east. In the inner and northern end of the fjord lies Ella Island. The Davy Sound at the southeastern end connects with the Greenland Sea after extending for about 20 km in a NW/SE direction.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute'', p. 118 Lyell Land forms the western boundary and Scoresby Land with the Stauning Alps lies to the southwest. The Antarctic Sound separates the Suess Land Peninsula and Ymer Island and connects with the Kaiser Franz Joseph Fjord system to the north. Other bran ...
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