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Vatnahverfi (Norse Greenland)
Vatnahverfi was a district in the Norse Greenlanders’ Eastern Settlement (Eystribyggð) and is generally regarded by archaeologists and historians as having the best pastoral land in the colony. The Norse settled Vatnahverfi in the late 10th century and farmed there for nearly 500 years before mysteriously disappearing from the district and the entirety of Greenland, likely at some point in the latter 15th century. Its name is roughly translated as “Lake District." Placement Located on Greenland's southwest coast, Vatnahverfi can be broadly thought of as a peninsula stretching northeast from the Labrador Sea to the Jespersens Glacier some 60 km inland and covering approximately 500 km2. It lies between Einarsfjord (today the fjord and the settlement at the fjord's head are both called Igaliku) and Hrafnsfjord (today called Agdluitsoq). The heart of peninsula (60.732307, -45.458640) is approximately 140 km northwest of Greenland's southernmost tip at Cape Far ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norse Greenland
The Norse exploration of North America began in the late 10th century, when Norsemen explored areas of the North Atlantic colonizing Greenland and creating a short term settlement near the northern tip of Newfoundland. This is known now as L'Anse aux Meadows where the remains of buildings were found in 1960 dating to approximately 1,000 years ago. This discovery helped reignite archaeological exploration for the Norse in the North Atlantic. This single settlement, located on the island of Newfoundland and not on the North American mainland, was abruptly abandoned. The Norse settlements on Greenland lasted for almost 500 years. L'Anse aux Meadows, the only confirmed Norse site in present-day Canada, was small and did not last as long. Other such Norse voyages are likely to have occurred for some time, but there is no evidence of any Norse settlement on mainland North America lasting beyond the 11th century. The Norse exploration of North America has been subject to numerous con ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Herjolfsnes (Norse Greenland)
Herjolfsnes was a Norse settlement in Greenland, 50 km northwest of Cape Farewell. It was established by Herjolf Bardsson in the late 10th century and is believed to have lasted some 500 years. The fate of its inhabitants, along with all the other Norse Greenlanders, is unknown. The site is known today for having yielded remarkably well-preserved medieval garments, excavated by Danish archaeologist Poul Nörlund in 1921. Its name roughly translates as Herjolf's Point or Cape. Establishment As noted in the Landnámabók (Icelandic Book of Settlements), Herjolf Bardsson was one of the founding chieftains of the Norse colony in Greenland, and was said to be "a man of considerable stature." He was part of an exodus from Iceland accompanying Erik the Red, who led an expedition of colonists in 25 ships in AD 985. Landing on Greenland's southwest coast, Erik and his other kinsmen almost invariably chose to settle further inland away from the open Labrador Sea, at the heads of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ammassalik
Ammassalik Island ( da, Ammassalik Ø) is an island in the Sermersooq municipality in southeastern Greenland, with an area of .Norwegian University of Science and Technology Geography Ammassalik Island is located in the region. Separating Ammassalik Island from the mainland of Greenland are the wide in the west and the Ikaasartivaq Strait in the northeast. To th ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snæfellsnes
The Snæfellsnes () is a peninsula situated to the west of Borgarfjörður, in western Iceland. The Snæfellsjökull volcano, regarded as one of the symbols of Iceland, can be found in the area. With its height of 1446 m, it is the highest mountain on the peninsula and has a glacier at its peak (''jökull'' means "glacier" in Icelandic). The volcano can be seen on clear days from Reykjavík, a distance of about 120 km. The mountain is also known as the setting of the novel ''Journey to the Center of the Earth'' by the French author Jules Verne. The area surrounding Snæfellsjökull has been designated one of the four National Parks by the government of Iceland. It is also the home of the Ingjaldsholl church, a Protestant church. The peninsula is one of the main settings in the '' Laxdœla saga'' and it was, according to this saga, the birthplace of the first West Norse member of the Varangian Guard, Bolli Bollasson. Other historical people who lived in the area accor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jared Diamond
Jared Mason Diamond (born September 10, 1937) is an American geographer, historian, ornithologist, and author best known for his popular science books ''The Third Chimpanzee'' (1991); ''Guns, Germs, and Steel'' (1997, awarded a Pulitzer Prize); ''Collapse'' (2005), ''The World Until Yesterday'' (2012), and '' Upheaval'' (2019). Originally trained in biochemistry and physiology,Jared Diamond, ''Collapse: How Societies Choose to Fail or Survive'', Penguin Books, 2005 and 2011 () Diamond is known for drawing from a variety of fields, including anthropology, ecology, geography, and evolutionary biology. He is a professor of geography at UCLA. In 2005, Diamond was ranked ninth on a poll by '' Prospect'' and ''Foreign Policy'' of the world's top 100 public intellectuals. Early life and education Diamond was born on September 10, 1937, in Boston, Massachusetts, United States. Both of his parents were from Ashkenazi Jewish families who had emigrated to the United States. His father, L ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Midden
A midden (also kitchen midden or shell heap) is an old dump for domestic waste which may consist of animal bone, human excrement, botanical material, mollusc shells, potsherds, lithics (especially debitage), and other artifacts and ecofacts associated with past human occupation. These features provide a useful resource for archaeologists who wish to study the diets and habits of past societies. Middens with damp, anaerobic conditions can even preserve organic remains in deposits as the debris of daily life are tossed on the pile. Each individual toss will contribute a different mix of materials depending upon the activity associated with that particular toss. During the course of deposition sedimentary material is deposited as well. Different mechanisms, from wind and water to animal digs, create a matrix which can also be analysed to provide seasonal and climatic information. In some middens individual dumps of material can be discerned and analysed. Shells A shell mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Ice Age
The Little Ice Age (LIA) was a period of regional cooling, particularly pronounced in the North Atlantic region. It was not a true ice age of global extent. The term was introduced into scientific literature by François E. Matthes in 1939. Matthes described glaciers in the Sierra Nevada of California that he believed could not have survived the hypsithermal; his usage of "Little Ice Age" has been superseded by "Neoglaciation". The period has been conventionally defined as extending from the 16th to the 19th centuries, (noted in Grove 2004:4). but some experts prefer an alternative timespan from about 1300 to about 1850. The NASA Earth Observatory notes three particularly cold intervals. One began about 1650, another about 1770, and the last in 1850, all of which were separated by intervals of slight warming. The Intergovernmental Panel on Climate Change Third Assessment Report considered that the timing and the areas affected by the Little Ice Age suggested largely independent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thule People
The Thule (, , ) or proto-Inuit were the ancestors of all modern Inuit. They developed in coastal Alaska by the year 1000 and expanded eastward across northern Canada, reaching Greenland by the 13th century. In the process, they replaced people of the earlier Dorset culture that had previously inhabited the region. The appellation "Thule" originates from the location of Thule (relocated and renamed Qaanaaq in 1953) in northwest Greenland, facing Canada, where the archaeological remains of the people were first found at Comer's Midden. The links between the Thule and the Inuit are biological, cultural, and linguistic. Evidence supports the idea that the Thule (and also the Dorset, but to a lesser degree) were in contact with the Vikings, who had reached the shores of Canada in the 11th century as part of Norse colonization of North America. In Viking sources, these peoples are called the ''Skrælingjar''. Some Thule migrated southward, in the "Second Expansion" or "Second Phase". ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saga Of Erik The Red
The ''Saga of Erik the Red'', in non, Eiríks saga rauða (), is an Icelandic saga on the Norse exploration of North America. The original saga is thought to have been written in the 13th century. It is preserved in somewhat different versions in two manuscripts: ''Hauksbók'' (14th century) and ''Skálholtsbók'' (15th century). Despite its title, the saga mainly chronicles the life and expedition of Thorfinn Karlsefni and his wife Gudrid, also recounted in the ''Saga of the Greenlanders''. For this reason it was formerly also called ;Halldór Hermannsson"Eiríks saga rauða ''or'' Þorfinns saga karlsefnis ok Snorra Þorbrandssonar" ''Bibliography of the Icelandic Sagas and Minor Tales'', Islandica 1, Ithaca, New York: Cornell University Libraries, 1908, , p. 16. Árni Magnússon wrote that title in the blank space at the top of the saga in . It also details the events that led to the banishment of Erik the Red to Greenland and the preaching of Christianity by his son ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beothuk
The Beothuk ( or ; also spelled Beothuck) were a group of indigenous people who lived on the island of Newfoundland. Beginning around AD 1500, the Beothuk culture formed. This appeared to be the most recent cultural manifestation of peoples who first migrated from Labrador to present-day Newfoundland around AD 1. The ancestors of this group had three earlier cultural phases, each lasting approximately 500 years. Description The Beothuk lived throughout the island of Newfoundland, mostly in the Notre Dame and Bonavista Bay areas. Estimates vary as to the number of Beothuk at the time of contact with Europeans. Beothuk researcher Ingeborg Marshall has argued that a valid understanding of Beothuk history and culture is directly impacted by how and by whom historical records were created, pointing to the ethnocentric nature of European accounts as inherently unreliable. Scholars of the 19th and early 20th century estimated about 2,000 individuals at the time of European contact ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dorset Culture
The Dorset was a Paleo-Eskimo culture, lasting from to between and , that followed the Pre-Dorset and preceded the Thule people (proto-Inuit) in the North American Arctic. The culture and people are named after Cape Dorset (now Kinngait) in Nunavut, Canada, where the first evidence of its existence was found. The culture has been defined as having four phases due to the distinct differences in the technologies relating to hunting and tool making. Artifacts include distinctive triangular end-blades, oil lamps () made of soapstone, and burins. The Dorset were first identified as a separate culture in 1925. The Dorset appear to have been extinct by 1500 at the latest and perhaps as early as 1000. The Thule people, who began migrating east from Alaska in the 11th century, ended up spreading through the lands previously inhabited by the Dorset. There is no strong evidence that the Inuit and Dorset ever met. Modern genetic studies show the Dorset population were distinct from later ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Climatic Optimum
The Medieval Warm Period (MWP), also known as the Medieval Climate Optimum or the Medieval Climatic Anomaly, was a time of warm climate in the North Atlantic region that lasted from to . Climate proxy records show peak warmth occurred at different times for different regions, which indicate that the MWP was not a globally uniform event. Some refer to the MWP as the ''Medieval Climatic Anomaly'' to emphasize that climatic effects other than temperature were also important. The MWP was followed by a regionally cooler period in the North Atlantic and elsewhere, which is sometimes called the Little Ice Age (LIA). Possible causes of the MWP include increased solar activity, decreased volcanic activity, and changes in ocean circulation. Research The Medieval Warm Period (MWP) is generally thought to have occurred from –, during the European Middle Ages. In 1965, Hubert Lamb, one of the first paleoclimatologists, published research based on data from botany, historical document res ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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