what sediments fall out of a glacier, they create a deposit called?
968234
D:till \n\nTill is an unsorted glacial sediment. Glacial drift is a general term for the coarsely graded and extremely heterogeneous sediments of glacial origin. Glacial till is that part of glacial drift which was deposited directly by the glacier. It may vary from clays to mixtures of clay, sand, gravel and boulders. A particularly sticky form of clay till is called gumbo. Clay in till may form balls called till balls. If a till ball rolls around in a stream and picks up rocks from the bed of the stream and becomes covered with them it may become an armored till ball.
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I think that hard frost is known as hoarfrost. Hoar frost is formed when the dew point is warmer than surface but colder than the air temperature, and colder than freezing point.
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Holocene Soil Development on Till and Outwash Inferred from Lake-Sediment Geochemistry in Michigan and Wisconsin \nAuthors: Ewing H.A.1; Nater E.A.2\nSource: Quaternary Research, Volume 57, Number 2, March 2002, pp. 234-243(10)\n\nParent material. Few soils weather directly from the underlying rocks. These "residual" soils have the same general chemistry as the original rocks. More commonly, soils form in materials that have moved in from elsewhere. Materials may have moved many miles or only a few feet. Windblown "loess" is common in the Midwest. It buries "glacial till" in many areas. Glacial till is material ground up and moved by a glacier. The material in which soils form is called "parent material." In the lower part of the soils, these materials may be relatively unchanged from when they were deposited by moving water, ice, or wind.\n\nSediments along rivers have different textures, depending on whether the stream moves quickly or slowly. Fast-moving water leaves gravel, rocks, and sand. Slow-moving water and lakes leave fine textured material (clay and silt) when sediments in the water settle out.\n\nClimate. Soils vary, depending on the climate. Temperature and moisture amounts cause different patterns of weathering and leaching. Wind redistributes sand and other particles especially in arid regions. The amount, intensity, timing, and kind of precipitation influence soil formation. Seasonal and daily changes in temperature affect moisture effectiveness, biological activity, rates of chemical reactions, and kinds of vegetation.\n\nTopography. Slope and aspect affect the moisture and temperature of soil. Steep slopes facing the sun are warmer, just like the south-facing side of a house. Steep soils may be eroded and lose their topsoil as they form. Thus, they may be thinner than the more nearly level soils that receive deposits from areas upslope. Deeper, darker colored soils may be expected on the bottom land.\n\nBiological factors. Plants, animals, micro-organisms, and humans affect soil formation. Animals and micro-organisms mix soils and form burrows and pores. Plant roots open channels in the soils. Different types of roots have different effects on soils. Grass roots are "fibrous" near the soil surface and easily decompose, adding organic matter. Taproots open pathways through dense layers. Micro-organisms affect chemical exchanges between roots and soil. Humans can mix the soil so extensively that the soil material is again considered parent material.\n\nThe native vegetation depends on climate, topography, and biological factors plus many soil factors such as soil density, depth, chemistry, temperature, and moisture. Leaves from plants fall to the surface and decompose on the soil. Organisms decompose these leaves and mix them with the upper part of the soil. Trees and shrubs have large roots that may grow to considerable depths.\n\nTime. Time for all these factors to interact with the soil is also a factor. Over time, soils exhibit features that reflect the other forming factors. Soil formation processes are continuous. Recently deposited material, such as the deposition from a flood, exhibits no features from soil development activities. The previous soil surface and underlying horizons become buried. The time clock resets for these soils. Terraces above the active floodplain, while genetically similar to the floodplain, are older land surfaces and exhibit more development features.\n\nThese soil forming factors continue to affect soils even on "stable" landscapes. Materials are deposited on their surface, and materials are blown or washed away from the surface. Additions, removals, and alterations are slow or rapid, depending on climate, landscape position, and biological activity.\n\nWhen mapping soils, a soil scientist looks for areas with similar soil-forming factors to find similar soils. The colors, texture, structure, and other properties are d
165493
Turbidite geological formations have their origins in turbidity current deposits, deposits from a form of underwater avalanche that are responsible for distributing vast amounts of clastic sediment into the deep ocean.
235598
sand stone, is a type of sediment rock,quartz conglomerate,shelly limestone,oil shale,coal,rock fragments that result from weathering may be transported by glacilar movements wind waves or current,this debris,is deposited at a new location,as a sediment.
405125
Often they form over centuries or millenia.  They are formed by snowfall that does not melt during the warmer months.  As each year's snowfall adds to the layers, it begins to move downhill.  Factors involved in the speed of glacier formation are the amount of snowfall, the amount of evaporation durning the dry season, and the amount of meltoff each year.  Some glaciers in Alaska and Siberia and Scadanavia are literally thousands of years old.  In Antarctica, they are millions of years old.  The glacier in the Mt. Saint Helens volcano crater (Washington State, USA), has formed in just 25 years!
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Two ideas: 1. Eroded (continental glaciers form deep valleys)\n                 2. Depressed (see link on isostacy)\n\nMaybe look in your text book.
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Erosion forms sand\nSand settles as sediment\nSediment hardens over time\nVoila, Sandstone
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I think that what you are asking about might be better called coastal deposition.\n\nOver the span of geologic time the sea level has changed dramatically. As the sea level has moved up and down over time the coastal erosion process has created continental shelves that are covered in deposits eroded from dry land around some continents. This process has also helped shape the coastlines of the continents. \n\nOne of the more spectacular examples of coastal deposition are river deltas. The sediment carried by the river is deposited as the flow of river water slows. This tends to sort the sediments according to the energy level of the water that is flowing into the open ocean. First larger grains like gravel and pebbles settle down, and as the river slows, sand, and finally clay size particles settle out of the water. Many river deltas have built up sediment deposits that are several miles thick and cover areas as large as some states. Most of southern Louisiana is a river delta deposit. \n\nAlong many coasts there is a predominant wind direction that helps to build coast long-shore currents. These currents move parallel to the coastline and will cause sediment accumulations (from rivers) such as sand bars and islands to slowly migrate in one direction. Much of the sand on beaches is actually slowly migrating along the shore. As heavier winter waves move the sand offshore, the sand also tends to move along the shore and sometimes temporarily moves back up onto the beach at a new location. \n\nAnother geologic process that is involved in coastal change is both uplift and subsidence. Uplift is taking place on some coasts due to tectonic plate motion. Other coasts are subsiding, or sinking, due to both faulting and slow compaction of underlying sediments. This sort of subsidence is taking place along the Gulf Coast of the US where there are large growth faults that parallel the coast that are sinking towards the Gulf. Sediment deposited thousands and millions of years ago is still settling in some areas and this leads to loss of coastal wetlands and rising local sea level. \n\nIn other areas coastlines are being changed by local erosion of uplifted sediments (e.g. California). Landslides carry hillsides down to the coastline. Another change in many coastlines is being caused by a geologic process called isostacy. As glaciers accumulated across North America during the last ice age, they weighed down that part of the earth's crust and caused it to sink into the asthenosphere. The glaciers melted long ago, but the areas that were covered by glaciers are still rising. This creates a sort of teeter-totter effect, where some coastlines like parts of the East Coast of the US and the Louisiana coast are sinking. \n\nInformation on isostatic rebound:\nhttp://www.homepage.montana.edu/~geol445/hyperglac/isostasy1/\n\nMississippi River Delta:\nhttp://www.lacoast.gov/geography/basins/mr/\n\nExplanation of long shore drift:\nhttp://www.cofc.edu/CGOInquiry/longshoredrift.htm\n\nGood explanation of barrier islands:\nhttp://www3.csc.noaa.gov/beachnourishment/html/geo/barrier.htm\n\nA very good illustration of differential erosion in a coastal setting:\nhttp://www.rgs.edu.sg/events/geotrip/stack.html\n\nUN Coastal Types:\nhttp://www.oceansatlas.com/servlet/CDSServlet?status=ND0yNzYwJmN0bl9pbmZvX3ZpZXdfc2l6ZT1jdG5faW5mb192aWV3X2Z1bGwmNj1lbiYzMz0qJjM3PWtvcw~~
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Ice crystals that form in the cells and destroy them
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Glaciers flow because of gravity.\n\nView this page:\nhttp://www.answers.com/topic/last-glacial-maximum\nFor info and a pic of what the world probably looked like during the last ice age. The grey denotes glaciers. The land (brown) has been adjusted for the drop in sea level and the ocean temperature difference is shown.\n\nThe ocean levels dropped. Much of the continental shelf which is now under water was exposed, dry land. The water that now covers them was locked up in the the glaciers.\n\nAlso look:\nhttp://uk.encarta.msn.com/encnet/RefPages/RefMedia.aspx?refid=461527006&artrefid=761570002&pn=3&sec=-1
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Igneous rock becomes sedimentary rock by weathering and erosion which makes sediments. The sediments then is deposited and is cemented together to cause sedimentary rock.
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Erratics are boulders transported and deposited by a glacier. Their composition (lithology) is different than the bedrock upon which they are sitting.\nThe Great Lakes region was once covered by glaciers. Photos of glacial erratics in Wisconsin at second url.\nPhoto and location of erratic in New York, third url.\nPhoto and discussion of erratics in Minnesota, fourth url.
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The mouth.\nLakes,streams from mountains.The ice from mountains melt,causing tiny streams of water running down the mountain.As it goes along,more water is collected(rain etc.),and it becomes a small river.There are three stages of a river.First,the valley is narrow,second,it gets wider,and third, it is almost flat and very wide.it ends at the sea. \nHope this helps :)
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A clastic rock is a sedimentary rock formed of particles deposited by water, wind, ice, gravity.  The particles themselves would give the rock texture--think of the gritty surface of a sandtone. Detrital texture is described by size, shape, and composition or the sorting of the redeposited particles. \n\nA chemical sedimentary rock is formed by precipitating from water solution. They precipate "in place", and are not formed by redeposited particles like clastic rocks. These include evaporites, opal, some carbonates, iron oxides, etc. Stalactites are examples. Dried up lake beds form flat layers of evaporites, another example. Chemical textures are usually crystalline with some special descriptions like pisolitic or  oolitic.\n\nThe category not mentioned is that of biological sedimentary rocks--composed largely of plant or animal material.
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Wind: Creates dunes and erodes rock\nRain: Erode the land and forms the river and lakes\nGlaciers: Formation of the glaciers is due to atmospheric effects, so is their melting, which as they slide down mountains craves things up.
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Generally, they're formed by freezing and erosion. Essentially what happens is that water gets into the cracks of larger rocks and then freezes and expands, causing pieces to fall off. Sometimes these smaller rocks end up in streams or rivers where they are carried by the current and rolled along the bottom, smoothing them out. over time, they get smaller and smoother becoming what we know as pebbles.