545 resultados para brocket deer
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Chronic wasting disease is a fatal neurological disease found in deer and elk in 14 western and mid-western states and two Canadian provinces. It is believed to have been first observed in Colorado and Wyoming in 1967. It is a disease caused by prions by an unknown transmission vector and impossible to cure at this time. Most of the management options currently available are labor-intensive and costly. The potential use of controlled burns to reduce or eliminate the prions that cause the disease was shown to have no effect on the prevalence of the disease in either study area. The temperatures needed to destroy prions were not reached by either surface or crown fires.
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This layer is a georeferenced raster image of the untitled, historic nautical chart: [A chart of Great Bluehill Bay, Penobscot River &c.] (sheet originally published in 1776). The map is [sheet 41] from the Atlantic Neptune atlas Vol. 3 : Charts of the coast and harbors of New England, from surveys taken by Samuel Holland and published by J.F.W. Des Barres, 1781. Scale [ca. 1:50,000]. This layer is image 2 of 2 total images of the two sheet source map, representing the eastern portion of the map. Covers a portion of Penobscot Bay, including Blue Hill Bay, Deer Island, and Eggemoggin Reach, Maine. The image is georeferenced to the surface of the earth and fit to the 'World Mercator' (WGS 84) projected coordinate system. All map collar information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, or other information associated with the principal map. This map shows coastal features such as harbors, inlets, rocks, channels, points, coves, shoals, islands, and more. Includes also selected land features such as cities and towns, and buildings. Relief is shown by hachures; depths by soundings. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection. The entire Atlantic Neptune atlas Vol. 3 : Charts of the coast and harbors of New England has been scanned and georeferenced as part of this selection.
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This layer is a georeferenced raster image of the historic paper map entitled: Map of the county of Milwaukee, Wisconsin, from surveys under the direction of H.F. Walling ; engraved, printed, colored & mounted at H.F. Wallings Map Establishment. It was published by M.H. Tyler in 1858. Scale [1:31,680]. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Wisconsin South State Plane NAD 1983 coordinate system (in Feet) (Fipszone 4803). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This cadastral map shows features such as roads, railroads and stations, drainage, city wards, selected buildings, property lots, and names of landowners, and more. Includes insets: City of Milwaukee -- Humboldt (Milwaukee) -- Franklin -- Oak Creek -- Wauwatosa. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.
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This layer is a georeferenced raster image of the historic, topographic paper map entitled: Milwaukee and vicinity, Wisconsin, 1959, mapped, edited and published by the Geological Survey. It was published by U.S. Dept. of the Interior, Geological Survey in 1962. Scale 1:24,000. Compiled from 1:24,000-scale maps of Thiensville, Menomonee Falls, Wauwatosa, Milwaukee, South Milwaukee, Greendale 1958, and Hales Corners 1959 7.5 minute quadrangles. Selected hydrographic data compiled from U.S. Lake Survey Charts 74 and 743 (1957). This layer is image 1 of 4 total images of the four sheet source map representing the northwest portion of the map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Wisconsin South State Plane NAD 1927 coordinate system (Fipszone 4803). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This is a typical topographic map portraying both natural and manmade features. It shows and names works of nature, such as mountains, valleys, lakes, rivers, vegetation, etc. It also identify the principal works of humans, such as roads, railroads, boundaries, transmission lines, major buildings, etc. Relief shown by contours (interval 10 feet) and spot heights. Depths shown by contours and soundings. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.
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This layer is a georeferenced raster image of the historic, topographic paper map entitled: Milwaukee and vicinity, Wisconsin, 1959, mapped, edited and published by the Geological Survey. It was published by U.S. Dept. of the Interior, Geological Survey in 1962. Scale 1:24,000. Compiled from 1:24,000-scale maps of Thiensville, Menomonee Falls, Wauwatosa, Milwaukee, South Milwaukee, Greendale 1958, and Hales Corners 1959 7.5 minute quadrangles. Selected hydrographic data compiled from U.S. Lake Survey Charts 74 and 743 (1957). This layer is image 2 of 4 total images of the four sheet source map representing the northeast portion of the map. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Wisconsin South State Plane NAD 1927 coordinate system (Fipszone 4803). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This is a typical topographic map portraying both natural and manmade features. It shows and names works of nature, such as mountains, valleys, lakes, rivers, vegetation, etc. It also identify the principal works of humans, such as roads, railroads, boundaries, transmission lines, major buildings, etc. Relief shown by contours (interval 10 feet) and spot heights. Depths shown by contours and soundings. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.
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Excavations were carried out in a Late Palaeolithic site in the community of Bad Buchau-Kappel between 2003 and 2007. Archaeological investigations covered a total of more than 200 m**2. This site is the product of what likely were multiple occupations that occurred during the Late Glacial on the Federsee shore in this location. The site is situated on a mineral ridge that projected into the former Late Glacial lake Federsee. This beach ridge consists of deposits of fine to coarse gravel and sand and was surrounded by open water, except for a connection to the solid shore on the south. A lagoon lay between the hook-shaped ridge and the shore of the Federsee. This exposed location provided optimal access to the water of the lake. In addition, the small lagoon may have served as a natural harbor for landing boats or canoes. Sedimentological and palynological investigations document the dynamic history of the location between 14,500 and 11,600 years before present (cal BP). Evidence of the deposition of sands, gravels and muds since the Bølling Interstadial is provided by stratigraphic and palynological analyses. The major occupation occurred in the second half of the Younger Dryas period. Most of the finds were located on or in the sediments of the ridge; fewer finds occurred in the surrounding mud, which was also deposited during the Younger Dryas. Direct dates on some bone fragments, however, demonstrate that intermittent sporadic occupations also took place during the two millennia of the Meiendorf, Bølling, and Allerød Interstadials. These bones were reworked during the Younger Dryas and redeposited in the mud. A 14C date from one bone of 11,600 years ago (cal BP) places the Late Palaeolithic occupation of the ridge at the very end of the Younger Dryas, which is in agreement with stratigraphic observations. Stone artifacts, numbering 3,281, comprise the majority of finds from the site. These include typical artifacts of the Late Palaeolithic, such as backed points, short scrapers, and small burins. There are no bipointes or Malaurie-Points, which is in accord with the absolute date of the occupation. A majority of the artifacts are made from a brown chert that is obtainable a few kilometers north of the site in sediments of the Graupensandrinne. Other raw materials include red and green radiolarite that occur in the fluvioglacial gravels of Oberschwaben, as well as quartzite and lydite. The only non-local material present is a few artifacts of tabular chert from the region near Kelheim in Bavaria. A unique find consists of two fragments of a double-barbed harpoon made of red deer antler, which was found in the Younger Dryas mud. It is likely, but not certain, that this find belongs to the same assemblage as the numerous stone artifacts. Although not numerous, animal bones were also found in the excavations. Most of them lay in sediments of the Younger Dryas, but several 14C dates place some of these bones in earlier periods, including the Meiendorf, Bølling, and Allerød Interstadials. These bones were reworked by water and redeposited in mud sediments during the Younger Dryas. As a result, it is difficult to attribute individual bones to particular chronological positions without exact dates. Species that could be identified include wild horse (Equus spec.), moose or elk (Alces alces), red deer (Cervus elaphus), roe deer (Capreolus capreolus), aurochs or bison (Bos spec.), wild boar (Sus scrofa), as well as birds and fish, including pike (Esox Lucius).
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Cf. Sabin 40807.
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Includes appendixes.
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"The native melodies used in these dances were supplied by Mr. R.R. De Poe, chief of the Rogue River tribe in Oregon." - Cover verso.
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National Highway Traffic Safety Administration, Washington, D.C.
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Mode of access: Internet.
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Ascobolus castaneus Teng, determined by S.C. Teng
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Metalwork, Iran, Seljuk; 8 3/16 in.x 6 39/64 in.; stonepaste; openwork, underglaze-painted, glazed in transparent turquoise
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Vol. [1]-[5] as Fur and feather series.
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Mode of access: Internet.