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Background information - Science Web Australia
Background information - Science Web Australia

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... lakes are createdwhen creeksand rivers carry salts into a lake, and there is no outlet to carrv the salt awav.The Great Salt Lake in Utah is the remnant of a large freshwater lake-Lake Bonneville. Its water outflows were cut off, causing the remaining water to become more salty as the water evaporat ...
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Geology Walk - Edinburgh Geological Society

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Sample Unit of Study - New York Science Teacher
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Draft Museum Guide - Valley Geology

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Weathering, Mass Wasting and Karst
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Sharktooth Hill Geology Background
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LAKE COMO - CLIL EXCELLENCE
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measuring the earth - Mepham Earth Science
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Quiz 5 - Brooklyn College
Quiz 5 - Brooklyn College

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the effects of isostasy - Earth Science Activities
the effects of isostasy - Earth Science Activities

... 1. Place the white painted block which represents an ice sheet on the sponge. Note the troughs which form either side. The trough forms because the crust is depressed by the weight of the ice sheet but the crust is too rigid to be depressed only where the ice is resting. So the area of the crust tha ...
1 Introduction to Geomorphology I. INTRODUCTION A
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Click here for a full book sample
Click here for a full book sample

... earth is made up of big pieces. The pieces are called tectonic plates. These plates can move apart or crash into each other. One tectonic plate can slip over or under another one. When the plates move, the land shakes. The earth can crack or change shape. ...
Key Question
Key Question

... Water • Nearly three quarters of all the fresh water used annually is consumed in farming, not in cities • Industries use another 20 percent of the world’s water supply, contributing heavily to pollution when the used water is returned to streams, lakes, and aquifers • Hydrologic cycle: where water ...
Quiz 5 - Brooklyn College
Quiz 5 - Brooklyn College

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The Esk Valley - Edinburgh Geological Society
The Esk Valley - Edinburgh Geological Society

... angle. Often they are near vertical. Fault - A discontinuity surface across which the rock has been displaced. Glaciofluvial - Referring to glacial meltwater activity. Intrusive igneous body - An igneous body that is pushed into the surrounding rock at depth. Meltwater channel - A channel cut by gla ...
The Greenhouse Effect on Earth
The Greenhouse Effect on Earth

... • Flow: If water or air combines with the downward movement, the regolith can “flow” downhill • Creep – The imperceptibly slow downslope flow of regolith • Unstable slopes move very slowly over long periods of time ...
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Overdeepening



Overdeepening is a characteristic of basins and valleys eroded by glaciers. An overdeepened valley profile is often eroded to depths which are hundreds of metres below the deepest continuous line (the thalweg) along a valley or watercourse. This phenomenon is observed under modern day glaciers, in salt-water fjords and fresh-water lakes remaining after glaciers melt, as well as in tunnel valleys which are partially or totally filled with sediment. When the channel produced by a glacier is filled with debris, the subsurface geomorphic structure is found to be erosionally cut into bedrock and subsequently filled by sediments. These overdeepened cuts into bedrock structures can reach a depth of several hundred metres below the valley floor.Overdeepened fjords and lakes have significant economic value as harbours and fisheries. Overdeepened basins and valleys filled with sediment (termed tunnel valleys) are of particular interest to engineers, petroleum geologists, and hydrologists; engineers apply the information for developing foundations and tunnel construction, petroleum geologists use tunnel valley locations to identify potential oil fields, while hydrologists apply this knowledge for groundwater resource management.
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