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Sandefjord Cove
Sandefjord Cove (sometimes called Sandefjord Bay) is a cove between Cape Ingrid and the terminus of Tofte Glacier on the west side of Peter I Island. A Norwegian expedition under Eyvind Tofte circumnavigated Peter I Island in the '' Odd I'' in 1927. In February 1929, the Norvegia under Nils Larsen carried out a series of investigations all around the island, landing on February 2 to hoist the Norwegian flag. The cove was named for Sandefjord, Norway, center of the Norwegian whaling industry. Framnes Head is a small rock point forming one of the headlands of the cove. dIt was charted and named by Larsen's expedition. It is steep and rugged, composed of lava and basaltic tuff. When members of the US Navy Second Antarctic Development Project landed there in 1948, they discovered a small colony of Adelie penguins Adelie or Adélie may refer to: * Adélie Land, a claimed territory on the continent of Antarctica * Adelie Land meteorite Adelie Land is a meteorite discovered on ...
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Cove
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, 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 Weathering is the deterioration of rocks, soils and minerals as well as wood and artificial materials through contact with water, atmospheric gase ...
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Cape Ingrid
Cape Ingrid () is a dark rock promontory separating Norvegia Bay and Sandefjord Cove on the west side of Peter I Island, Antarctica. It was discovered in 1927 by a Norwegian expedition under Eyvind Tofte in the '' Odd I'', a vessel of Lars Christensen's whaling fleet, and named for Ingrid Christensen Ingrid Christensen (10 October 1891 – 18 June 1976) was an early polar explorer. She was known as the first woman to view Antarctica and land on the Antarctic mainland. Early life Christensen (née Dahl) was the daughter of Alfhild Freng Dahl ..., the wife of Lars. References Headlands of Antarctica Peter I Island {{Subantarctic-geo-stub ...
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Tofte Glacier
Tofte Glacier is a glacier immediately south of Sandefjord Cove on the west side of Peter I Island Peter I Island ( no, Peter I Øy) is an uninhabited volcanic island in the Bellingshausen Sea, from continental Antarctica. It is claimed as a dependency of Norway and, along with Bouvet Island and Queen Maud Land, composes one of the three No .... Discovered in 1927 by a Norwegian expedition in the and named for Eyvind Tofte, leader of the expedition. References Glaciers of Antarctica Peter I Island Subantarctic glaciers {{subantarctic-glacier-stub ...
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Peter I Island
Peter I Island ( no, Peter I Øy) is an uninhabited volcanic island in the Bellingshausen Sea, from continental Antarctica. It is claimed as a dependency of Norway and, along with Bouvet Island and Queen Maud Land, composes one of the three Norwegian dependent territories in the Antarctic and Subantarctic. The island measures approximately , with an area of ; its highest point is the ultra-prominent, Lars Christensen Peak. Nearly all the island is covered by a glacier, and it is surrounded most of the year by pack ice, making it inaccessible during these times. There is little vertebrate animal life on the island, apart from some seabirds and seals. The island was first sighted by Fabian Gottlieb von Bellingshausen on 21 January 1821 and was named for Peter I of Russia. Not until 2 February 1929 did anyone set foot on the island, when Nils Larsen and Ola Olstad's Second ''Norvegia'' Expedition, financed by Lars Christensen, was successful. They claimed it for Norway, which an ...
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Odd I
''Odd I'' was a Norwegian whaler, launched in 1912 as ''Dominion II''. She was renamed ''Odd I'' in 1921 and retained that name until 1963 when she became ''Annstein'', except for a period during World War II when she served as a ''Vorpostenboot'' for the German Kriegsmarine under the name ''Orkan''. She was condemned in 1971 and was deleted from the Norwegian Ship Register on 15 March 1971. Description The ship was long, with a beam of and a depth of . She was assessed at , . She was powered by a triple expansion steam engine which drive a single screw propeller. It had cylinders of , and diameter by stroke. The engine was rated at 58 nhp. History ''Dominion II'' was built in 1912 as yard number 68 by Porsgrund Mekaniske Værksted, Porsgrund for A/S Dominion Whaling Ltd, Sandefjord. She was launched in July. The Code Letters MHSQ were allocated and her port of registry was Sandefjord. She was operated under the management of T. Dannevig & Co. Sandefjord. In December 1918, ...
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Norvegia (ship)
Norvegia (; Latin for "Norway") is a Norwegian cow's milk cheese produced by Tine. It has a market share of about 60% of white cheeses in Norway.norvegia
Store norske leksikon, retrieved 3 Mar, 2019
It is similar to , has a mild taste and melts easily. There are different types of it. It has been produced since the 1890s. Its recipe details remain a of Tine.


See also

* Jarlsberg cheese *

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Island
An island (or isle) is an isolated piece of habitat that is surrounded by a dramatically different habitat, such as water. Very small islands such as emergent land features on atolls can be called islets, skerries, cays or keys. An island in a river or a lake island may be called an eyot or ait, and a small island off the coast may be called a holm. Sedimentary islands in the Ganges delta are called chars. A grouping of geographically or geologically related islands, such as the Philippines, is referred to as an archipelago. There are two main types of islands in the sea: continental and oceanic. There are also artificial islands, which are man-made. Etymology The word ''island'' derives from Middle English ''iland'', from Old English ''igland'' (from ''ig'' or ''ieg'', similarly meaning 'island' when used independently, and -land carrying its contemporary meaning; cf. Dutch ''eiland'' ("island"), German ''Eiland'' ("small island")). However, the spelling of the word ...
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Norwegian Flag
The national flag of Norway ( nb, Norges flagg; nn, Noregs flagg; ) is red with a navy blue Scandinavian cross fimbriated in white that extends to the edges of the flag; the vertical part of the cross is shifted to the hoist side in the style of the ''Dannebrog'', the flag of Denmark. History It is difficult to establish what the earliest flag of Norway looked like. During ancient times countries did not fly flags. Kings and other rulers flew flags, especially in battle. Saint Olav used a serpent within a white mark at the Battle of Nesjar. Prior to this the raven or dragon was used. Magnus the Good used the same mark as Saint Olav. Harald Hardrade used the raven banner. This flag was flown by various Viking chieftains and other Scandinavian rulers during the 9th, 10th, and 11th centuries AD. Inge used a red lion on gold. Sverre used an eagle in gold and red. The earliest known flag which could be described as a national flag of Norway is the one used today as the Roya ...
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Sandefjord
Sandefjord () is a city and the most populous municipality in Vestfold og Telemark county, Norway. The municipality of Sandefjord was established on 1 January 1838. The municipality of Sandar was merged into Sandefjord on 1 January 1969. On 1 January 2017, rural municipalities of Andebu and Stokke were merged into Sandefjord as part of a nationwide municipal reform. This merger was the first one to take place during the reform. The city is known for its rich Viking history and the prosperous whaling industry, which made Sandefjord the richest city in Norway.Porter, Darwin and Danforth Prince (2003). ''Frommer's Norway''. Wiley. p. 158. . Today, it has built up the third-largest merchant fleet in Norway. It is home to Europe's only museum dedicated to whaling, and is home to Gokstad Mound where the 9th century Gokstad Ship was discovered. Sandefjord has numerous nicknames, including the Viking, Whaling "capital" of Norway or as the undisputed summer city of Norway. The city i ...
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Whaling In Norway
Whaling in Norway involves hunting of minke whales for use as animal and human food in Norway and for export to Japan. Whale hunting has been a part of Norwegian coastal culture for centuries, and commercial operations targeting the minke whale have occurred since the early 20th century. Some still continue the practice in the modern day. History Norwegians caught whales off the coast of Tromsø as early as the 9th or 10th century. Vikings from Norway also introduced whaling methods for driving small cetaceans, like pilot whales, into fjords in Iceland. The Norse sagas, and other ancient documents, provide few details on Norwegian whaling. The sagas recount some disputes between families over dead whales but do not describe any organized whale fishery in Norway. Spear-drift whaling was practised in the North Atlantic as early as the 12th century. In open boats, hunters would strike a whale with a marked spear, with the intent of later locating the dead beached whale to claim a righ ...
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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 ...
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Basaltic Tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcani ...
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