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	Till - Wikipedia, the free encyclopedia
		Glacial drift is a general term for the coarsely graded and extremely heterogeneous sediments of glacial origin.
		Till is deposited at the terminal moraine, along the lateral and medial moraines and in the ground moraine of a glacier.
		As a glacier melts, especially a continental glacier, large amounts of till are washed away and deposited as outwash in sandurs by the rivers flowing from the glacier and as varves in any proglacial lakes which may form.
	en.wikipedia.org /wiki/Glacial_till_plains (534 words)

	Glacial till plains (Ohio) - Wikipedia, the free encyclopedia
		The Glacial till plains are in the Northwest of Ohio.
		This region is fertile and has gently rolling moraine hills created by the movement of glaciers.
		Glacial till plains - Lake Erie - Lake Erie Islands - Black Swamp - Miami Valley - Western Reserve - Northwest Ohio
	en.wikipedia.org /wiki/Glacial_till_plains_(Ohio) (132 words)

	HA 730-K Central Lowland aquifers text
		The Paleozoic rocks that underlie the glacial deposits dip gently away from the axes of the Cincinnati, the Kan-kakee, and the Findlay Arches and the southern extension of the Wisconsin Arch (fig.
		On the arches and domes, the older Paleozoic rocks directly underlie the glacial deposits near the axes of the folds; in the structural basins, the younger Paleozoic rocks are directly beneath the glacial materials near the centers of the folds.
		Under natural conditions, water in the upper part of the glacial deposits discharges to local streams, lakes, or wetlands; however, water in the deeper parts of the sand and gravel deposits flows beneath local streams and lakes and discharges to larger streams that are regional drains.
	capp.water.usgs.gov /gwa/ch_k/K-text1.html (8031 words)

	Watershed, Crooked River, Geology Chapter (Site not responding. Last check: 2007-10-23)
		The entire basin is in the Dissected Till Plains and is near the southern edge of the area covered by glaciers (Detroy and Skelton 1983).
		The Missouri River flood plain near the mouth of the Crooked River is extremely flat and poorly drained.
		Most basin soils are formed from glacial till (a mixture of clay, rock, gravel and sand), alluvium (water deposited soil) and a windblown silt called loess.
	www.mdc.mo.gov /fish/watershed/crooked/geology/23agetxt.htm (594 words)

	Glacial till - Hutchinson encyclopedia article about Glacial till (Site not responding. Last check: 2007-10-23)
		Deposit of clay, mud, gravel, and boulders left by a glacier.
		It is unsorted, with all sizes of fragments mixed up together, and shows no stratification; that is, it does not form clear layers or beds.
		This information should not be considered complete, up to date, and is not intended to be used in place of a visit, consultation, or advice of a legal, medical, or any other professional.
	encyclopedia.farlex.com /Glacial+till (97 words)

	WDNR - Southeast Glacial Plains (Site not responding. Last check: 2007-10-23)
		Most of this Ecological Landscape is composed of glacial materials deposited during the Wisconsin Ice Age, but the southwest portion consists of older, pre-Wisconsin till with a more dissected topography.
		Historically, vegetation in the Southeast Glacial Plains consisted of a mix of prairie, oak forests and savanna, and maple-basswood forests.
		The Southeast Glacial Plains Region is economically prosperous with a well-educated and racially diverse population.
	www.dnr.state.wi.us /landscapes/se_glacial.htm (1029 words)

	Newport Soils \| Rhode Island NRCS
		This nearly level, well drained soil is on the crests of drumlins and glacial till plains in the southeastern part of the State.
		This gently sloping and sloping, well drained soil is on drumlins and glacial till plains in south eastern Rhode Island.
		The complex is on drumlins and glacial till plains of densely populated areas mainly in southeastern Rhode Island.
	www.ri.nrcs.usda.gov /technical/newport.htm (2004 words)

	Ecological Development in the Black River Watershed
		As a result of glaciation, the watershed consists of lake plains to the north (from Erie’s ancestral lakes) and till plains in the central part of the watershed (where glacial till comprises the soils).
		When the glaciers retreated, they left behind altered stream valleys and coated the landscape with a layer of glacial till.
		The biotic community that colonized the landscape as it was released from the grip of the ice consisted of a mixture of southern (“Carolinian”) species and northern (“boreal”) organisms whose propagules (seeds, spores, and eggs) survived physical transportation by the ice.
	www.noaca.org /ECO.HTML (2433 words)

	Info: IA Wetlands & Riparian Areas - Bear Creek Article
		They were beautiful little brooks, so clear, so overarched with tall grasses and willows, so plaided with the colors of the pebbles in the sun, so dark and mysterious in the shade; with secret pockets under the soddy banks for the shiners, pumpkinseeds, dace, chubs, and other small fish which populated the pure waters.
		The Western Corn Belt Plains ecoregion, which covers most of Iowa and parts of surrounding states, can be characterized as extensive cropland on level to gently rolling, dissected glacial till plains, hilly loess plains, and morainal hills with broad smooth ridgetops (Griffith et al.
		Soils of the region were primarily developed from glacial till and alluvial, lacustrine, and -wind-blown deposits.
	www.ag.iastate.edu /centers/iawetlands/Bearcrk.html (5521 words)

	Geohazards Mapping (Site not responding. Last check: 2007-10-23)
		To avoid or mitigate geologic hazards, a fundamental understanding of the geology of the affected area is required.
		Many geologic maps that depict glacial or bedrock deposits tell the reader a great deal more than the name and distribution of units or material.
		Maps that show depression contours on glacial-till-covered plains that indicate areas may contain thick deposits of unstable, coprogenous earth that is likely to shrink and swell.
	www.dnr.state.oh.us /htdocs/geosurvey/staff/mapgrp/hazards.htm (197 words)

	Establishment of Seeded Grasslands for Wildlife Habitat in the Prairie Pothole Region
		They occur on subirrigated lowlands, on nearly level to gently undulating glacial till plains, overflow sites, level swales and depressions, residual and glacial uplands, and bottomlands along rivers and streams.
		These tall native grasses also occur on nearly level to rolling glacial till plains, lake plains, and on high stream terraces in the southeastern portions of the prairie pothole region.
		Seed harvested from natural grassland in the central and northern plains should be used.
	www.npwrc.usgs.gov /resource/habitat/grasland/types.htm (2619 words)

	WMNH - Glaciers and Glacial Landforms(45 slides) $90 (Site not responding. Last check: 2007-10-23)
		WMNH - Glaciers and Glacial Landforms(45 slides) $90
		Sattelite, aerial and ground slides of glaciers in the Swiss Alps, Alaska's Brooks Range, the Canadian Rockies, the Sierra Nevada, the Southern Alps of New Zealand and the southern Andes near Tierra del Fuego.
		Landforms and structures include alpine and valley glaciers, continental glaciers, median/lateral/terminal moraines, cirques, aretes, horns, cols, crevices, ice falls, paternoster lakes, kettles, eskers, drumlins, outwash plains, glacial till, kame terraces.
	www.wmnh.com /wmsgg012.htm (86 words)

	[No title]
		Short-grass prairie occurs on the high plains east of the Rocky Mountains, and mid-grass prairie occurs in between.
		The glaciated northeastern sector is generally more level than the unglaciated western part.
		Extensive glacial till plains and glacial lake beds are almost dead flat.
	www.museum.state.il.us /exhibits/midewin/nagrasslands.html (533 words)

	Ecoregions of North Dakota and South Dakota
		This ecoregion has a relatively homogeneous topography of level to gently rolling glacial till plains with areas of morainal hills and loess deposits.
		Contouring and terracing are common practices in the loess-covered areas of the Western Corn Belt Plains.
		Of the two areas in South Dakota, the northern one is distinguished from neighboring regions by its rock-free soil and a paucity of wetlands.
	www.npwrc.usgs.gov /resource/habitat/ndsdeco/47a.htm (220 words)

	Scio Soils \| Rhode Island NRCS
		This nearly level, moderately well drained soil is in depressions of glacial till plains.
		Areas are long and narrow and range mostly from 5 to 20 acres.
		This nearly level to gently sloping, moderately well drained soil is on glacial till plains.
	www.ri.nrcs.usda.gov /technical/scio.htm (813 words)

	UW CFR Pack Forest - Kapowsin
		The Kapowsin series consists of moderately deep, moderately well drained soils formed in glacial till.
		GEOGRAPHIC SETTING: Kapowsin soils are on convex or undulating glacial till plains and moraines at elevations from 50 to 900 feet.
		This pedon has andic intergrade soil properties from 0 to 16 inches with estimated properties of >5 percent volcanic glass, 1.0 to 2.0 percent Al + 1/2 Fe by acid-oxalate, and bulk density of 0.85 to 1.0 g/cc.
	soilslab.cfr.washington.edu /esc410/1997/Justin/kapowsin.htm (932 words)

	Expedition enters Dissected Till Plains - greatfallstribune.com (Site not responding. Last check: 2007-10-23)
		The "Bald pated hills" Whitehouse mentions are the Dissected Till Plains which stretch across the southern part of Iowa and extend north, along the Missouri and Big Sioux rivers into northwestern Iowa.
		Ice-age glaciers left glacial "drift" consisting of clay, sand, gravel, and boulders.
		This deposit is called till, a coarser form of loess.
	www.greatfallstribune.com /news/stories/20040717/localnews/864607.html (229 words)

	Important Natural Features
		Much of the land in Ada Township is rolling to steep terrain, in areas bordering the Grand River and its major tributaries.
		These areas, formed as glacial moraines, are often covered in second growth oak forest, with occasional areas of more mature maple-beech forest.
		Nearly level terrain is found in two major areas of the Township - in the valley of the Grand River along its entire length through the Township, and in the northeast part of the Township, in upland glacial till plains.
	www.ada.mi.us /adatwp/INF.htm (1852 words)

	Ft. Belknap
		To facilitate hunting, the tribe broke into two bands, one group remaining in the northern plains to hunt bison.
		By the late 1700s the Gros Ventre had moved from the northern prairies to the northern plains and became allies with the Blackfeet.
		Their relationship with the Blackfeet remained solid until the mid-1800s, when a number of cultural and social factors caused the Blackfeet and the Gros Ventre people to wage war against each other.
	www.bigskytribes.com /ft__belknap.htm (644 words)

	Intensive Grazing/Seasonal Dairying: Chapter 8 Agronomic Summary
		The soils of the fields used in the study were Canfield and Ravenna silt loams, typical soils of northeast Ohio.
		Both soils are moderately well drained and occur on nearly level to gently sloping areas in glacial till plains.
		In 1987, potash was applied to all fields at 300 lb per acre; lime was applied in the fall of 1989 at two tons per acre.
	ohioline.osu.edu /rb1190/b1190_10.html (748 words)

	Virtual Saskatchewan - Mid-Boreal Upland Ecoregion
		Landscape: Area immediately south of the Shield features a varied landscape that includes steeply sloping and eroded escarpments, hilly glacial till plains and level plateaus.
		Loamy, gray soils produce taller trees than in the Shield - aspen, white spruce, jack pine, fl spruce and tamarack are common.
		Duck Mountain Provincial Park, home to picturesque Madge Lake, offers a full range of summer recreational activities (including wheelchair accessible camping), as well as downhill and cross-country skiing, and snowmobiling in the winter.
	www.virtualsk.com /maps/ecoregions_5.html (337 words)

	Hillslope Hydrology and Soil Morphology for a Wetland Basin in South-Central Minnesota -- Reuter and Bell 67 (1): 365 ...
		An extensive soil catena of the glacial till plains of Minnesota
		of ablation till overlying dense and compacted basal till (Bettis et al., 1996).
		Landscape evolution and shallow groundwater hydrology of a till landscape in central Iowa.
	soil.scijournals.org /cgi/content/full/67/1/365 (3537 words)

	birding facts Birding Resources by the Fat Birder
		The Boreal Plain boasts steep escarpments, glacial till plains and wetlands.
		Finally, the Prairie, which covers only 38% of the province, contains aspen groves, glacial till and glacial lake plains, sand hills, potholes and badlands.
		Even though more than half of the province has a sub-arctic climate, the rest being continental and steppe climates, with temperatures ranging from -40 degrees Celsius in the winter to +40 degrees in the summer, Saskatchewan is the home or resting place for large numbers of many bird species.
	www.fatbirder.com /links_geo/america_canada/saskatchewan.html (1880 words)

	Lester (Site not responding. Last check: 2007-10-23)
		These soils formed in friable loam glacial till.
		This undulating, well drained soil is on ridges, knolls, and convex side slopes on glacial till plains.
		Individual areas are irregular in shape and range from 3 to about 70 acres in size.
	www.soils.agri.umn.edu /academics/classes/soil2125/..../doc/lestrsw.htm (330 words)

	UW CFR Pack Forest - Norma
		The Norma series consists of deep, poorly drained soils formed in old alluvium in depressions on glacial till plains and drainageways.
		GEOGRAPHIC SETTING: Norma soils are in depressions on glacial till plains and drainageways at elevations from near sea level to about 1,000 feet.
		The base saturation (by NH4OAc) of these soils is assumed to increase to more than 50 percent within 60 inches.
	soilslab.cfr.washington.edu /ESC410/1997/Justin/norma.htm (688 words)

	Newport Soil Map Unit Description- RI
		NeA - Newport silt loam, 0 to 3 percent slopes.
		NeB - Newport silt loam, 3 to 8 percent slopes.
		NeC silt loam, 8 to 15 percent slopes.
	nesoil.com /ri/newport.htm (1997 words)

	Energy Citations Database (ECD) - Energy and Energy-Related Bibliographic Citations (Site not responding. Last check: 2007-10-23)
		Energy Citations Database (ECD) Document #5032352 - Ground water transport of nitrate in loess and glacial till
		Availability information may be found in the Availability, Publisher, Research Organization, Resource Relation and/or Author (affiliation information) fields and/or via the "Full-text Availability" link.
		Ground water transport of nitrate in loess and glacial till
	www.osti.gov /energycitations/product.biblio.jsp?osti_id=5032352 (150 words)

	[No title]
		This TIF image was derived from USGS Digital Elevation Model (DEM) data.
		Purpose: The map was created to illustrate the various landforms of Illinois, which include but are not limited to: glacial moraines, river valleys, glacial till plains, and bedrock structures.
		This map can to a limited extent serve as base map information.
	www.isgs.uiuc.edu /nsdihome/outmeta/shaderel.txt (884 words)

	Riparian Forest Effect on Lateral Stream Channel Migration in the Glacial Till Plains
		Volume 34, Number 1, February 1998, pages 179-184
		Dendrochronology analyses of point bar complexes were used to quantify the effects of riparian forests on local lateral migration of bends in seven streams in the glacial till plains of north central Missouri.
		Stream bends were paired with similar bank height, midchannel radius of curvature, soil composition, and watershed size.
	www.awra.org /jawra/papers/J97023.html (156 words)

	Glacial Till Farm - LocalHarvest
		We are located in east central South Dakota in the midst of the Glacial Lakes region.
		We currently garden for the Down Town Farmers' Market in Sioux Falls, SD, and we also sell to restaurants in Sioux Falls and Watertown.
		Your use of this site constitutes your acceptance of our
	www.localharvest.org /farms/M9278 (116 words)

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