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Lukovo Point
Mihaylovski Cove ( bg, Михайловски залив, Mihaylovski zaliv, ) is the 5 km wide cove indenting for 1.3 km the northwest coast of South Bay in Livingston Island, Antarctica that is entered west of Ereby Point and east of Lukovo Point, and has its head fed by Kamchiya Glacier. The area was known to early 19th century sealers who operated from nearby Johnsons Dock. The feature is named after the brothers Petar Mihaylovski, physician at St. Kliment Ohridski base during the 2007/08 and subsequent seasons, and Hristo Mihaylovski, engineer in the national Antarctic campaign during 2015/16 and subsequent seasons. Location Mihaylovski Cove is centred at . British mapping in 1968, Chilean in 1971, Argentine in 1980, and Bulgarian in 2005, 2009 and 2017. Related features Lukovo Point Lukovo Point is the mostly ice-free point on the northwest coast of South Bay in Livingston Island, Antarctica projecting 200 m southwards. It is surmounted by Krakra Bluff on the n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hannah Point
Hannah Point is a point on the south coast of Livingston Island in the South Shetland Islands, Antarctica. It forms the east side of the entrance to Walker Bay and the west side of the entrance to South Bay. Surmounted by Ustra Peak to the north, with Liverpool Beach extending between the peak and the tip of Hannah Point. Ice-free area ca. . The area was visited by early 19th century sealers frequenting nearby Johnsons Dock. The British base camp Station P on the east side of Hannah Point operated from 29 December 1957 until 15 March 1958. Among the birds that make their home here are the gentoo and macaroni penguins as well as kelp gulls. Southern giant petrels nest here as do blue-eyed shags, skuas, and snowy sheathbills. Southern elephant seals and Antarctic fur seals are among the larger life forms observed at the point. Hannah Point is one of the most popular Antarctic tourist sites frequented by cruise ships. The geographical feature is named after the British seal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beaches Of Livingston Island
A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from rock, such as sand, gravel, shingle, pebbles, etc., or biological sources, such as mollusc shells or coralline algae. Sediments settle in different densities and structures, depending on the local wave action and weather, creating different textures, colors and gradients or layers of material. Though some beaches form on inland freshwater locations such as lakes and rivers, most beaches are in coastal areas where wave or current action deposits and reworks sediments. Erosion and changing of beach geologies happens through natural processes, like wave action and extreme weather events. Where wind conditions are correct, beaches can be backed by coastal dunes which offer protection and regeneration for the beach. However, these natural forces have become more extreme due to climate change, permanently altering beaches at very rapid ra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands Of Livingston Island
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coves Of Livingston Island
A cove is a small type of bay or coastal inlet. Coves usually have narrow, restricted entrances, are often circular or oval, and are often situated within a larger bay. Small, narrow, sheltered bays, inlets, creek (tidal), creeks, or recesses in a coast are often considered coves. Colloquially, the term can be used to describe a sheltered bay. Geomorphology describes coves as precipitously-walled and rounded cirque-like openings as in a valley extending into or down a mountainside, or in a hollow or nook of a cliff or steep mountainside. A cove can also refer to a corner, nook, or cranny, either in a river, road, or wall, especially where the wall meets the floor. A notable example is Lulworth Cove on the Jurassic Coast in Dorset, England. To its west, a second cove, Stair Hole, is forming. Formation Coves are formed by differential erosion, which occurs when softer rocks are worn away faster than the harder rocks surrounding them. These rocks further erode to form a circular b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctic Place-names Commission
The Antarctic Place-names Commission was established by the Bulgarian Antarctic Institute in 1994, and since 2001 has been a body affiliated with the Ministry of Foreign Affairs of Bulgaria. The Commission approves Bulgarian place names in Antarctica, which are formally given by the President of the Republic according to the Bulgarian Constitution (Art. 98) and the established international practice. Bulgarian names in Antarctica Geographical names in Antarctica reflect the history and practice of Antarctic exploration. The nations involved in Antarctic research give new names to nameless geographical features for the purposes of orientation, logistics, and international scientific cooperation. As of 2021, there are some 20,091 named Antarctic geographical features, including 1,601 features with names given by Bulgaria.Bulgarian Antarctic Gazett ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch Ness Monster
The Loch Ness Monster ( gd, Uilebheist Loch Nis), affectionately known as Nessie, is a creature in Scottish folklore that is said to inhabit Loch Ness in the Scottish Highlands. It is often described as large, long-necked, and with one or more humps protruding from the water. Popular interest and belief in the creature has varied since it was brought to worldwide attention in 1933. Evidence of its existence is anecdotal, with a number of disputed photographs and sonar readings. The scientific community explains alleged sightings of the Loch Ness Monster as hoaxes, wishful thinking, and the misidentification of mundane objects. The pseudoscience and subculture of cryptozoology has placed particular emphasis on the creature. Origin of the name In August 1933, the ''Courier'' published the account of George Spicer's alleged sighting. Public interest skyrocketed, with countless letters being sent in detailing different sightingsR. Binns ''The Loch Ness Mystery Solved'' pp 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Bay (Livingston Island)
South Bay () is a wide bay indenting for the south coast of Livingston Island in the South Shetland Islands, Antarctica. The bay is lying northwest of False Bay, Livingston Island, False Bay and east of Walker Bay, and is entered between Hannah Point and Miers Bluff. The glaciers Kamchiya Glacier, Kamchiya, Pimpirev Glacier, Pimpirev, Perunika Glacier, Perunika, Contell Glacier, Contell, Johnsons Glacier, Johnsons and Hurd Ice Cap feed the bay. South Bay was known to both US, American and UK, British sealers as early as 1820, and the name has been well established in international usage for over 100 years. Maps Chart of South Shetland including Coronation Island, &c.from the exploration of the sloop Dove in the years 1821 and 1822 by George Powell Commander of the same. Scale ca. 1:200000. London: Laurie, 1822. South Shetland Islands.Scale 1:200000 topographic map No. 5657. DOS 610 – W 62 60. Tolworth, UK, 1968. * Islas Livingston y Decepción. Mapa topográfico a escala 1: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Composite Gazetteer Of Antarctica
The Composite Gazetteer of Antarctica (CGA) of the Scientific Committee on Antarctic Research (SCAR) is the authoritative international gazetteer containing all Antarctic toponyms published in national gazetteers, plus basic information about those names and the relevant geographical features. The Gazetteer includes also parts of the International Hydrographic Organization (IHO) General Bathymetric Chart of the Oceans (GEBCO) gazetteer for under-sea features situated south of 60° south latitude. , the overall content of the CGA amounts to 37,893 geographic names for 19,803 features including some 500 features with two or more entirely different names, contributed by the following sources: {, class="wikitable sortable" ! Country ! Names , - , United States , 13,192 , - , United Kingdom , 5,040 , - , Russia , 4,808 , - , New Zealand , 2,597 , - , Australia , 2,551 , - , Argentina , 2,545 , - , Chile , 1,866 , - , Norway , 1,706 , - , Bulgaria , 1,450 , - , Ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lukovo, Bulgaria
Lukovo is a village in Svoge Municipality, Sofia Province, in western Bulgaria. Accessed Nov 11, 2014 Lukovo Point in Antarctica
Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest contine ... is named after the village.
References Villages in Sofia Province {{Sof ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
