878 resultados para Abrasive Wear and Tear


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This layer is a georeferenced raster image of the historic paper map entitled: A new chart of Massachusetts Bay, and part of the coast of Maine, by Samuel Lambert, hydrographer, Salem, 1822 ; New edition published by Henry Whipple, 1853. Scale [ca. 1:200,000]. Covers the coast of New England from Buzzards Bay, Massachusetts to Monhegan Island, Maine. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Massachusetts State Plane Coordinate System, Mainland Zone (in Feet) (Fipszone 2001). 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, or other information associated with the principal map. This nautical chart shows coastal features such as rocks, channels, points, coves, harbors, islands, lighthouses, and more. Depths are shown by soundings and shading. It also shows land features such as settlements and more. This layer is part of a selection of digitally scanned and georeferenced historic maps of Massachusetts from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of regions, originators, ground condition dates (1755-1922), scales, and purposes. The digitized selection includes maps of: the state, Massachusetts counties, town surveys, coastal features, real property, parks, cemeteries, railroads, roads, public works projects, etc.

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The shapes and surface textures of sand-sized quartz grains from the sediments cored at Site 645 in southern Baffin Bay during ODP Leg 105 were studied to characterize the terrigenous materials and the settling processes involved in the deposition of these sediments. Here, we show a homogeneous sand fraction that results from mixing grains from various provenances. The characteristics inherited from terrestrial processes (varying degrees of wear; fluviatile, aeolian, and diagenetic features) dominate the characteristics that result from evolution in a high-energy marine environment. Thus, the influence of the last stage of sedimentation in a deep-marine environment was difficult to distinguish. However, fluctuations in the relative proportions of particular features reveal that the terrigenous material derived from sedimentary formations of Baffin Island and East Greenland or from direct abrasion of the crystalline shield, which changed through time as the dominant settling processes evolved. In particular, this study confirms the onset of major ice rafting as old as late Miocene.

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Federal Highway Administration, Office of Research, Development and Technology, Washington, D.C.

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National Highway Traffic Safety Administration, Washington, D.C.

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Transportation Department, Research and Special Programs Administration, Washington, D.C.

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National Bureau of Standards, Tire Systems Section, Washington, D.C.

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Texas State Department of Highways and Public Transportation, Transportation Planning Division, Austin

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Federal Highway Administration, Office of Research, Washington, D.C.

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Mode of access: Internet.

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Imprint varies: 19__-1910, New york, The Daily trade record co.; 1914- New York, Fairchild Publishing Co.