|
Laussedat Heights
The Arctowski Peninsula () is a peninsula, long in a north-south direction, lying between Andvord Bay and Wilhelmina Bay on the west coast of Graham Land, Antarctica. Location The Arctowski Peninsula is on the Danco Coast on the west of the Antarctic Peninsula. It extends in a north-northwest direction from the Forbidden Plateau to the south into the Gerlache Strait to the north. Wilhelmina Bay is to the east. Across the Gerlache Strait the end of the peninsula faces the Solvay Mountains on Brabant Island to the north, and the Osterrieth Range on Anvers Island to the northwest. Rongé Island is west of the northwest side of the peninsula. The Laussedat Heights on the southwest side of the peninsula look over Andvord Bay to the west. The peninsula extends southeast to a line defined by Arago Glacier, which flows south into Henryk Cove, and Woodbury Glacier, which flows north into Piccard Cove. Northern features include Cape Anna, Mount Fourcade, Orne Harbour, Spigot Peak, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cuverville Island
Cuverville Island or Île de Cavelier de Cuverville is a dark, Rock (geology), rocky island lying in Errera Channel between Arctowski Peninsula and the northern part of Rongé Island, off the west coast of Graham Land in Antarctica. Cuverville Island was discovered by the Belgian Antarctic Expedition (1897–1899) under Adrien de Gerlache, who named it for Jules de Cuverville (1834–1912), a vice admiral of the French Navy. Important Bird Area The island has been identified as an Important Bird Area (IBA) by BirdLife International because it supports a bird colony, breeding colony of about 6500 pairs of gentoo penguins, the largest for this species on the Antarctic Peninsula. Other birds nesting at the site include southern giant petrels and Antarctic shags. File:Gentoo_Penguin_Colony_(16048405889).jpg File:Pingüinos,_Cuverville_1.jpg File:Top_of_Paradise_Harbor_(24412357410).jpg File:00_2118_Antarctica_-_Cuverville_Island.jpg See also * List of Antarctic and sub-Antarct ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Anna
Wilhelmina Bay () is a bay wide between the Reclus Peninsula and Cape Anna along the west coast of Graham Land on the Antarctic Peninsula. Location Wilhelmina Bay is on the Danco Coast on the west side of the Antarctic Peninsula. It indents the southeast side of Gerlache Strait opposite the Solvay Mountains of Brabant Island. The Arctowski Peninsula defines its southwest side, Forbidden Plateau its southeast side and Nansen Island is in the northeast of the bay. Wilhelmina Bay is between Charlotte Bay to the northeast and Andvord Bay to the southwest. Coastal features include, clockwise from the eastern entrance, *The Reclus Peninsula, including Jacques Peaks, Bancroft Bay, Cañón Point, Zapato Point, and Café Point. *Leonardo Glacier, Sadler Point, Blanchard Glacier, Garnerin Point, Pishtachev Peak and Rozier Glacier. * Piccard Cove, including Sophie Cliff, Balis Ridge, Montgolfier Glacier, Bacho Kiro Peak, Mechit Buttress, Woodbury Glacier and O'Neal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Advisory Committee On Antarctic Names
The Advisory Committee on Antarctic Names (ACAN or US-ACAN) is an advisory committee of the United States Board on Geographic Names responsible for recommending commemorative names for features in Antarctica. History The committee was established in 1943 as the Special Committee on Antarctic Names (SCAN). It became the Advisory Committee on Antarctic Names in 1947. Fred G. Alberts was Secretary of the Committee from 1949 to 1980. By 1959, a structured nomenclature was reached, allowing for further exploration, structured mapping of the region and a unique naming system. A 1990 ACAN gazeeter of Antarctica listed 16,000 names. Description The United States does not recognise territorial boundaries within Antarctica, so ACAN assigns names to features anywhere within the continent, in consultation with other national nomenclature bodies where appropriate, as defined by the Antarctic Treaty System. The research and staff support for the ACAN is provided by the United States Geologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Henryk Arctowski
Henryk Arctowski (15 July 1871 – 21 February 1958; ), born Henryk Artzt, was a Polish scientist and explorer. Living in exile for a large part of his life, Arctowski was educated in Belgium and France. He was one of the first humans to winter in Antarctica, as part of the Belgian Antarctic Expedition, and became an internationally renowned meteorologist, also working for over 10 years in the United States. Arctowski was instrumental in restoring Polish independence after the First World War, after which he returned to Poland, where he continued a prolific academic career, having even declined an offer to become Minister of Education. At the time World War II broke out, Arctowski and his wife were in America, and they were unable to return; he spent the final part of his career working as a researcher at the Smithsonian until his retirement, and died in 1958 in Bethesda, Maryland. Several geographical features, the Henryk Arctowski Polish Antarctic Station and a medal of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adrien De Gerlache
Baron Adrien Victor Joseph de Gerlache de Gomery (; 2 August 1866 – 4 December 1934) was a Belgian officer in the Belgian Royal Navy who led the Belgian Antarctic Expedition of 1897–99. Early years Born in Hasselt in eastern Belgium as the son of an army officer, de Gerlache was educated in Brussels. From a young age, he was deeply attracted by the sea, and made three voyages in 1883 and 1884 to the United States as a cabin boy on an ocean liner. He studied engineering at the Free University of Brussels. After finishing his third year in 1885, he quit the university and joined the Belgian Navy on 19 January 1886. After graduating from the nautical college of Ostend he worked on fishery protection vessels as second and third lieutenant. In October 1887 he signed on as a seaman on the ''Craigie Burn'', an English ship, for a voyage to San Francisco, but the ship failed to round Cape Horn and was sold for scrap in Montevideo. He returned to Europe after spending time in Ur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Belgian Antarctic Expedition
The Belgian Antarctic Expedition of 1897–1899 was the first expedition to winter in the Antarctic region. Led by Adrien de Gerlache de Gomery aboard the RV ''Belgica'', it was the first Belgian Antarctic expedition and is considered the first expedition of the Heroic Age of Antarctic Exploration. Among its members were Frederick Cook and Roald Amundsen, explorers who would later attempt the respective conquests of the North Pole. Preparation and surveying In 1896, after a period of intensive lobbying, Adrien Victor Joseph de Gerlache de Gomery purchased the Norwegian-built whaling ship ''Patria'', which, following an extensive refit, he renamed . Gerlache had worked together with the Geographical Society of Brussels to organize a national subscription, but was able to outfit his expedition only after the Belgian government voted in favor of two large subsidies, making it a state-supported undertaking. With a multinational crew that included Roald Amundsen from Norway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Late Cretaceous
The Late Cretaceous (100.5–66 Ma) is the more recent of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', the Latin word for the white limestone known as chalk. The chalk of northern France and the white cliffs of south-eastern England date from the Cretaceous Period. Climate During the Late Cretaceous, the climate was warmer than present, although throughout the period a cooling trend is evident. The tropics became restricted to equatorial regions and northern latitudes experienced markedly more seasonal climatic conditions. Geography Due to plate tectonics, the Americas were gradually moving westward, causing the Atlantic Ocean to expand. The Western Interior Seaway divided North America into eastern and western halves; Appalachia and Laramidia. India maintained a northward course towards Asia. In the Southern Hemisphere, Aus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andean Intrusive Suite
The Andes ( ), Andes Mountains or Andean Mountain Range (; ) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is long and wide (widest between 18°S and 20°S latitude) and has an average height of about . The Andes extend from south to north through seven South American countries: Argentina, Chile, Bolivia, Peru, Ecuador, Colombia, and Venezuela. Along their length, the Andes are split into several ranges, separated by intermediate depressions. The Andes are the location of several high plateaus—some of which host major cities such as Quito, Bogotá, Cali, Arequipa, Medellín, Bucaramanga, Sucre, Mérida, El Alto, and La Paz. The Altiplano Plateau is the world's second highest after the Tibetan Plateau. These ranges are in turn grouped into three major divisions based on climate: the Tropical Andes, the Dry Andes, and the Wet Andes. The Andes are the highest mountain range ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mid-Cretaceous
The Cenomanian is, in the International Commission on Stratigraphy's (ICS) geological timescale, the oldest or earliest age of the Late Cretaceous Epoch or the lowest stage of the Upper Cretaceous Series. An age is a unit of geochronology; it is a unit of time; the stage is a unit in the stratigraphic column deposited during the corresponding age. Both age and stage bear the same name. As a unit of geologic time measure, the Cenomanian Age spans the time between 100.5 and 93.9 million years ago (Mya). In the geologic timescale, it is preceded by the Albian and is followed by the Turonian. The Upper Cenomanian starts around at 95 Mya. The Cenomanian is coeval with the Woodbinian of the regional timescale of the Gulf of Mexico and the early part of the Eaglefordian of the regional timescale of the East Coast of the United States. At the end of the Cenomanian, an anoxic event took place, called the Cenomanian-Turonian boundary event or the "Bonarelli event", that is associated with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctic Peninsula Volcanic Group
The Antarctic (, ; commonly ) is the polar region of Earth that surrounds the South Pole, lying within the Antarctic Circle. It is diametrically opposite of the Arctic region around the North Pole. The Antarctic comprises the continent of Antarctica, the Kerguelen Plateau, and other island territories located on the Antarctic Plate or south of the Antarctic Convergence. The Antarctic region includes the ice shelves, waters, and all the island territories in the Southern Ocean situated south of the Antarctic Convergence, a zone approximately wide and varying in latitude seasonally. The region covers some 20 percent of the Southern Hemisphere, of which 5.5 percent (14 million km2) is the surface area of the Antarctica continent itself. All of the land and ice shelves south of 60°S latitude are administered under the Antarctic Treaty System. Biogeographically, the Antarctic realm is one of eight biogeographic realms on Earth's land surface. Climate change in Antarctic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Early Cretaceous
The Early Cretaceous (geochronology, geochronological name) or the Lower Cretaceous (chronostratigraphy, chronostratigraphic name) is the earlier or lower of the two major divisions of the Cretaceous. It is usually considered to stretch from 143.1 Megaannum#SI prefix multipliers, Ma to 100.5 Ma. Geology Proposals for the exact age of the Barremian–Aptian boundary ranged from 126 to 117 Ma until recently (as of 2019), but based on drillholes in Svalbard the defining Anoxic event#Cretaceous, early Aptian Oceanic Anoxic Event 1a (OAE1a) was dated to 123.1±0.3 Ma, limiting the possible range for the boundary to c. 122–121 Ma. There is a possible link between this anoxic event and a series of Early Cretaceous large igneous provinces (LIP). The Ontong Java Plateau, Ontong Java-Manihiki Plateau, Manihiki-Hikurangi Plateau, Hikurangi large igneous province, emplaced in the South Pacific at c. 120 Ma, is by far the largest LIP in Earth's history. The Onto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trinity Peninsula Group
The Trinity (, from 'threefold') is the Christian doctrine concerning the nature of God, which defines one God existing in three, , consubstantial divine persons: God the Father, God the Son (Jesus Christ) and God the Holy Spirit, three distinct persons ('' hypostases'') sharing one essence/substance/nature (''homoousion''). As the Fourth Lateran Council declared, it is the Father who s, the Son who is , and the Holy Spirit who proceeds. In this context, one essence/nature defines God is, while the three persons define God is. This expresses at once their distinction and their indissoluble unity. Thus, the entire process of creation and grace is viewed as a single shared action of the three divine persons, in which each person manifests the attributes unique to them in the Trinity, thereby proving that everything comes "from the Father", "through the Son", and "in the Holy Spirit". This doctrine is called Trinitarianism, and its adherents are called Trinitarians, while i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
