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East Falkland
East Falkland () is the largest island of the Falkland Islands, Falklands in the South Atlantic, having an area of or 54% of the total area of the Falklands. The island consists of two main land masses, of which the more southerly is known as Lafonia; it is joined by a narrow isthmus where the settlement of Goose Green is located, and it was the scene of the Battle of Goose Green during the Falklands War. The two main centres of population in the Falklands, Stanley, Falkland Islands, Stanley and Mount Pleasant, Falkland Islands, Mount Pleasant, which are both in the northern half of East Falkland, are home to three-quarters of the island's population. Geography East Falkland, which has an area of , a little over half the total area of the islands consists of two land masses of approximately equal size. The island is almost bisected by two deep fjords, Choiseul Sound and Brenton Loch-Grantham Sound, which are separated by the wide isthmus that connects Lafonia in the south to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Islands Of The Falkland Islands
The following list contains larger islands and other notable islands in the Falkland Islands, Falklands. Area data are from the USGS unless otherwise specified. Islands larger than 1 Other notable islands List of Falkland Islands named after people This is a short list of islands, which are known to be named after someone. Until at least 1781, the Falklands as a whole were known as the Sebald or Sebaldine Island after Sebald de Weert, who sighted them and tried to make landfall on the Jason Islands in January 1600. * Beauchene Island - Jacques Gouin de Beauchêne * Keppel Island - Augustus Keppel, 1st Viscount Keppel, Augustus Keppel * Lafonia (peninsula) - Samuel Fisher Lafone * Saunders Island, Falkland Islands, Saunders Island - Charles Saunders (Royal Navy officer), Charles Saunders * Tyssen Islands - John Tyssen (1811–1893), British naval officer * Weddell Island - James Weddell Spanish names derived from people A list of the derivations of Span ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeozoic
The Paleozoic ( , , ; or Palaeozoic) Era is the first of three geological eras of the Phanerozoic Eon. Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma at the start of the Mesozoic Era. The Paleozoic is subdivided into six geologic periods (from oldest to youngest), Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. Some geological timescales divide the Paleozoic informally into early and late sub-eras: the Early Paleozoic consisting of the Cambrian, Ordovician and Silurian; the Late Paleozoic consisting of the Devonian, Carboniferous and Permian. The name ''Paleozoic'' was first used by Adam Sedgwick (1785–1873) in 1838 to describe the Cambrian and Ordovician periods. It was redefined by John Phillips (1800–1874) in 1840 to cover the Cambrian to Permian periods. It is derived from the Greek ''palaiós'' (παλαιός, "old") and ''zōḗ'' (ζωή, "life") meaning "ancient l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesozoic
The Mesozoic Era is the Era (geology), era of Earth's Geologic time scale, geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Period (geology), Periods. It is characterized by the dominance of archosaurian reptiles such as the dinosaurs, and of Gymnosperm, gymnosperms such as cycads, ginkgoaceae and Araucariaceae, araucarian conifers; a hot Greenhouse and icehouse earth, greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since Cambrian explosion, complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic. The era began in the wake of the Permian–Triassic extinction event, the largest mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction whose victims included the non-avian dinosaurs, Pterosaur, pterosaurs, Mosasaur, mosasaurs, and Plesiosaur, plesiosaurs. The Mesozoic was a time of significant tectonic, climatic, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anchorage (maritime)
An anchorage is a location at sea where ships can lower anchors. Anchorages are where anchors are lowered and utilised, whereas moorings usually are tethering to buoys or something similar. The locations usually have conditions for safe anchorage in protection from weather conditions, and other hazards. The purpose of resting a ship at sea securely can be for waiting to enter ports, as well as taking on cargo or passengers where insufficient port facilities exist. Some coastlines without port facilities have extensive anchorage locations. In the days of large-scale sailing ship operations, a ship could wait at an anchorage for the wind to change, allowing it to continue its journey. The mooring of large ships in locations with adequate conditions for secure berthing is an engineering task requiring considerable technical skill. See also * Roadstead * Sea anchor A sea anchor (also known as a parachute anchor, drift anchor, drift sock, para-anchor or boat brake) is a devi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Port William, Falkland Islands
Port William (French: ''Baye Choiseul'',Dom Pernety, Antoine-Joseph. ''Journal historique d'un voyage fait aux Iles Malouïnes en 1763 et 1764 pour les reconnoître et y former un établissement; et de deux Voyages au Détroit de Magellan, avec une Rélation sur les Patagons.'' Berlin: Etienne de Bourdeaux, 1769. 2 volumes, 704 pp.Online vol. 1vol. 2Abridged English version Spanish: ''Puerto Groussac'') is a large inlet on the east coast of East Falkland island. A strait called "the Narrows" leads into Stanley Harbour. Port William has several other bays on it, namely Gypsy Cove and Yorke Bay, which is a noted beauty spot, Hearnden Water, which is effectively the estuary of the Murrell River and Weir Creek, Blanco Bay and Sparrow Cove. Kidney Island is just north of Port William. The peninsula on which Canopus Hill, Stanley Airport and Gypsy Cove lie, together with a narrow spit of land known as Navy Point, effectively divides Port William from Stanley Harbour. As such ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Berkeley Sound
Berkeley Sound is an inlet, or fjord in the north east of East Falkland in the Falkland Islands. The inlet was the site of the first attempts at colonisation of the islands, at Port Louis, by the French. Berkeley Sound has several smaller bays within it – Uranie Bay, Port Louis harbour and Johnson's Harbour bay, separated by Grave Point, and includes islands such as Hog Island, Kidney Island (a nature reserve) and Long Island. It was enlarged as the result of glacial action. Berkeley Sound was visited by Charles Darwin during his round-the-world voyage on HMS ''Beagle'' in 1834. He found it an "undulating land, with a desolate and wretched aspect". Berkeley Sound is used by the fishing industry as a designated locality for the transshipment of fish, with accidental oil spills having occurred in the process. Settlements * Green Patch * Johnson's Harbour * Port Louis Port Louis (, ; or , ) is the capital and most populous city of Mauritius, mainly located in the Por ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tarns
A tarn (or corrie loch) is a mountain lake, pond or pool, formed in a cirque (or "corrie") excavated by a glacier. A moraine may form a natural dam below a tarn. Etymology The word is derived from the Old Norse word ''tjörn'' ("a small mountain lake without tributaries") meaning pond. In parts of Northern England – predominantly Cumberland and Westmorland (where there are 197), but also areas of North Lancashire and North Yorkshire – 'tarn' is widely used as the name for small lakes or ponds, regardless of their location and origin (e.g. Talkin Tarn, Urswick Tarn, Malham Tarn). Similarly, in Scandinavian languages, a ''tjern'' or ''tjørn'' (both Norwegian) or ''tjärn'' or ''tärn'' (both Swedish) is a small natural lake, often in a forest or with vegetation closely surrounding it or growing into the tarn. The name of the Tjörnin in Reykjavik, Iceland is also from a related word. The specific technical use for a body of water in a glacial corrie comes from the hig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsh
In ecology, a marsh is a wetland that is dominated by herbaceous plants rather than by woody plants.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p More in general, the word can be used for any low-lying and seasonally waterlogged terrain. In Europe and in agricultural literature low-lying meadows that require draining and embanked polderlands are also referred to as marshes or marshland. Marshes can often be found at the edges of lakes and streams, where they form a transition between the aquatic and terrestrial ecosystems. They are often dominated by grasses, rushes or reeds. If woody plants are present they tend to be low-growing shrubs, and the marsh is sometimes called a carr. This form of vegetation is what differentiates marshes from other types of wetland such as swamps, which are dominated by trees, and mires, which are wetlands that have accumulated deposits of acidic peat. Marshes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pasture
Pasture (from the Latin ''pastus'', past participle of ''pascere'', "to feed") is land used for grazing. Types of pasture Pasture lands in the narrow sense are enclosed tracts of farmland, grazed by domesticated livestock, such as horses, cattle, sheep, or swine. The vegetation of tended pasture, forage, consists mainly of grasses, with an interspersion of legumes and other forbs (non-grass herbaceous plants). Pasture is typically grazed throughout the summer, in contrast to meadow which is ungrazed or used for grazing only after being mown to make hay for animal fodder. Pasture in a wider sense additionally includes rangelands, other unenclosed pastoral systems, and land types used by wild animals for grazing or browsing. Pasture lands in the narrow sense are distinguished from rangelands by being managed through more intensive agricultural practices of seeding, irrigation, and the use of fertilizers, while rangelands grow primarily native vegetation, managed with e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Usborne
Mount Usborne () is a mountain on East Falkland. At above sea level, it is the highest point in the Falkland Islands. It is only taller than Mount Adam, the highest peak on West Falkland. The mountain is referenced by Charles Darwin in Chapter 9 of ''Zoology of the Voyage of H.M.S. Beagle''. It is named after Alexander Burns Usborne, master's assistant on , the ship that took Darwin on his famous voyage. As one of the highest mountains of the Falklands, it experienced some glaciation. The remains of glacial cirque A (; from the Latin word ) is an amphitheatre-like valley formed by Glacier#Erosion, glacial erosion. Alternative names for this landform are corrie (from , meaning a pot or cauldron) and ; ). A cirque may also be a similarly shaped landform a ...s can be seen on the mountain. The handful of Falklands mountains over have References Sources * Stonehouse, B (ed.) ''Encyclopedia of Antarctica and the Southern Oceans'' (2002, ) External links A Stroll up ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wickham Heights
The Wickham Heights () are a rugged chain of mountains on East Falkland in the Falkland Islands. They include the island group's highest peak, Mount Usborne, Mount Wickham and are partly contiguous with No Man's Land. The slopes of Wickham Heights feature numerous stone run A stone run (called also ''stone river'', ''stone stream'' or ''stone sea''Lafonia. Rivers and streams such as the [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
