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Norton Bay
Norton Bay (''Kaŋiiqusuk'' in Inupiaq) is a waterway classified bay located on the northeastern part of the Norton Sound, on the Seward Peninsula in the Nome Census Area of the Bering Sea of the U.S. state of Alaska. The mouths of several rivers debouch at Norton Bay, including the Kwik, Kwiniuk, and Tubutulik rivers. The name Norton was assigned in 1859 by the Coast Survey. Norton Bay and Norton Sound were discovered as one entity by Captain James Cook in 1778, and named after Sir Fletcher Norton (who later became Lord Grantley), who was the speaker of the House of Commons of Great Britain. Geography The north shore of the bay is in front of the Kwiktalik Mountain () in Seaward Peninsula. The Reindeer Hills lie on the Southhead of the Bay. Cape Nome is at the entrance to the bay. Circa 1902, there were several Alaska Native villages on the northern shore of the Norton Bay: Kviguk and Kwik villages. The streams joining the north shore of the bay are Kvingak, Kwik, Kwiniuk, ...
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Norton Sound
Norton Sound (russian: Нортон-Саунд) is an inlet of the Bering Sea on the western coast of the U.S. state of Alaska, south of the Seward Peninsula. It is about 240 km (150 mi) long and 200 km (125 mi) wide. The Yukon River delta forms a portion of the south shore and water from the Yukon influences this body of water. It is ice-free from June to October. Norton Sound was explored by Captain James Cook in September 1778. He named the body of water after Sir Fletcher Norton, then Speaker of the British House of Commons. The Norton Sound area has been home to Yup'ik and Inupiat for many centuries. It is the boundary between the two peoples; the Inupiat live to the north and the Yup'ik to the south. The town of Nome is along the northern edge of Norton Sound. The villages of Elim, Golovin, Stebbins, White Mountain, Koyuk, Shaktoolik, St. Michael, and Unalakleet are on the shores or waterways flowing into Norton Sound. The Iditarod Trail Sled ...
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Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', " chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Ear ...
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Cape Denbigh
Cape Denbigh is located on the Seward Peninsula in Eastern Norton Sound in the U.S. state of Alaska. It is notable for the Iyatayet site, an Archaic stage hunter-gatherer archaeological site. The headland is a moderately high, rounded hill, joined to the mainland by a low, narrow neck. The head of the bight, eastward of the cape, is shoal, but in approaching the water shoals gradually. A good anchorage in northeasterly winds can be had eastward of the cape. The water shoals rapidly inside a depth of 4 fathoms when approaching the shore.01727672461 References External links * Landforms of the Bering Sea Denbigh Denbigh (; cy, Dinbych; ) is a market town and a community in Denbighshire, Wales. Formerly, the county town, the Welsh name translates to "Little Fortress"; a reference to its historic castle. Denbigh lies near the Clwydian Hills. History ... Landforms of Nome Census Area, Alaska Landforms of the Seward Peninsula {{NomeAK-geo-stub ...
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Iyatayet Site
The Iyatayet site is an archaeological site and National Historic Landmark located on the northwest shore of Cape Denbigh on Norton Bay in Nome Census Area, Alaska. It shows evidence of several separate cultures, dating back as far as 6000 B.C. It was excavated starting in 1948 by J. Louis Giddings, the pioneering archaeologist of the area. It is significant as the type site of the Norton culture, representative of human occupation c. 500BCE-500CE, first described by Giddings in 1964. It is also significant for the Denbigh Flint complex, which lay underneath the Norton materials, and provides evidence of some of the earliest human activity in the region. The site was declared a National Historic Landmark in 1961. Description The Iyatayet site is located on both sides of Iyatayet Creek, near its mouth on the northwest side of Cape Denbigh, a peninsular projection into Norton Bay, on the central-west coast of Alaska. The site has a complex series of depositions, which begi ...
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Walrus
The walrus (''Odobenus rosmarus'') is a large flippered marine mammal with a discontinuous distribution about the North Pole in the Arctic Ocean and subarctic seas of the Northern Hemisphere. The walrus is the only living species in the family Odobenidae and genus ''Odobenus''. This species is subdivided into two subspecies: the Atlantic walrus (''O. r. rosmarus''), which lives in the Atlantic Ocean, and the Pacific walrus (''O. r. divergens''), which lives in the Pacific Ocean. Adult walrus are characterised by prominent tusks and whiskers, and their considerable bulk: adult males in the Pacific can weigh more than and, among pinnipeds, are exceeded in size only by the two species of elephant seals. Walruses live mostly in shallow waters above the continental shelves, spending significant amounts of their lives on the sea ice looking for benthic bivalve mollusks to eat. Walruses are relatively long-lived, social animals, and they are considered to be a " keyston ...
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Mukluk
Mukluks or kamik ( iu, ᑲᒥᒃ ) (singular: , plural: ) are a soft boot, traditionally made of reindeer ( caribou) skin or sealskin, and worn by Arctic aboriginal people, including the Inuit, Iñupiat, and Yup'ik. Mukluks may be worn over an inner boot liner and under a protective overshoe. The term ''mukluk'' is often used for any soft boot designed for cold weather, and modern designs may use both traditional and modern materials. The word ''mukluk'' is of Yup'ik origin, from , the bearded seal, while ''kamik'' is an Inuit word. Related boots Soft-soled boots, of similar materials (mostly sealskin and caribou-skin) and designs, but with local variations, are traditionally worn in circumpolar areas. These include the North American Arctic, including Greenland, the European Arctic, including Fennoscandia, and Siberia. Another type of boot, sometimes called an Inuit boot, originating in Greenland and the eastern part of Alaska, is made by binding it with animal cartilage ...
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Herring
Herring are forage fish, mostly belonging to the family of Clupeidae. Herring often move in large schools around fishing banks and near the coast, found particularly in shallow, temperate waters of the North Pacific and North Atlantic Oceans, including the Baltic Sea, as well as off the west coast of South America. Three species of ''Clupea'' (the type genus of the herring family Clupeidae) are recognised, and comprise about 90% of all herrings captured in fisheries. The most abundant of these species is the Atlantic herring, which comprises over half of all herring capture. Fish called herring are also found in the Arabian Sea, Indian Ocean, and Bay of Bengal. Herring played an important role in the history of marine fisheries in Europe, and early in the 20th century, their study was fundamental to the development of fisheries science. These oily fish also have a long history as an important food fish, and are often salted, smoked, or pickled. Herring are also kno ...
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Tomcod
''Microgadus tomcod'', also commonly known as frostfish, Atlantic tomcod or winter cod, is a type of cod found in North American coastal waters from the Gulf of St. Lawrence, St. Lawrence River and northern Newfoundland, south to Virginia. The fishing season of the tomcod varies by location—one known example is the Sainte-Anne River in Quebec, where its season is from late-December to mid-February. A bimonitoring program tracked hormone levels of Atlantic tomcod caught near Miramichi and Kouchibouguac in 1993 and 1994, demonstrating that the preparatory period for spawning began in September with maximal steroid levels in November, and spawning took place from late December to January. The town of Sainte-Anne-de-la-Pérade is notable for its fishing village built on the frozen waters of the Ste-Anne, playing host to the scores of fishermen visiting the town to fish for the species. After General Electric dumped polychlorinated biphenyls (PCBs) in the Hudson River from 1947 ...
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Tertiary
Tertiary ( ) is a widely used but obsolete term for the geologic period from 66 million to 2.6 million years ago. The period began with the demise of the non- avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start of the Cenozoic Era, and extended to the beginning of the Quaternary glaciation at the end of the Pliocene Epoch. The time span covered by the Tertiary has no exact equivalent in the current geologic time system, but it is essentially the merged Paleogene and Neogene periods, which are informally called the Early Tertiary and the Late Tertiary, respectively. The Tertiary established the Antarctic as an icy island continent. Historical use of the term The term Tertiary was first used by Giovanni Arduino during the mid-18th century. He classified geologic time into primitive (or primary), secondary, and tertiary periods based on observations of geology in Northern Italy. Later a fourth period, the Quaternary, was applied. In the early ...
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Placer Gold
Placer mining () is the mining of stream bed (alluvial) deposits for minerals. This may be done by open-pit (also called open-cast mining) or by various surface excavating equipment or tunneling equipment. Placer mining is frequently used for precious metal deposits (particularly gold) and gemstones, both of which are often found in alluvial deposits—deposits of sand and gravel in modern or ancient stream beds, or occasionally glacial deposits. The metal or gemstones, having been moved by stream flow from an original source such as a vein, are typically only a minuscule portion of the total deposit. Since gems and heavy metals like gold are considerably denser than sand, they tend to accumulate at the base of placer deposits. Placer deposits can be as young as a few years old, such as the Canadian Queen Charlotte beach gold placer deposits, or billions of years old like the Elliot Lake uranium paleoplacer within the Huronian Supergroup in Canada. The containing materia ...
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