By Joseph Holden

ISBN-10: 0273740695

ISBN-13: 9780273740698

This hugely revered and best-selling textbook presents an attractive and complete advent to the foremost issues inside actual geography. It makes a speciality of realizing the inter-linkages among approaches, locations and environments and is totally illustrated to illustrate how the actual surroundings works. An advent to actual Geography and the surroundings is observed via a wealthy and wide variety of digital aid assets together with up-to-date weblinks correct for every bankruptcy, a number of selection questions, fieldwork routines, interactive versions and movies. The textual content is appropriate for either undergraduate and postgraduate learn within the box of actual geography.

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Extra resources for An Introduction to Physical Geography and the Environment

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Different combinations of mechanisms result in different events, some of which can then be observed or measured. not always produce an event. Events occur only when the mechanisms interact at the right place at the right time. 8 shows how events are associated with the coming together of mechanisms, which are themselves influenced by other events. An event may be the shattering of a piece of rock. The underlying mechanisms to produce that event will include fluctuating temperatures above and below freezing, the presence of water in rock, and expansion and contraction of water within the rock upon freezing and thawing.

The measurements that were being performed in the 1950s and 1960s often did not allow us to evaluate or understand physical processes properly. They tended to be quantitative descriptions rather than the measurement of processes. For example, in 1953 Leopold and Maddock, physical geographers who studied rivers, published results of a survey of streams and rivers in the central and southwest United States. g. 5; see Chapter 12). As the discharge increased downstream the equations suggested that channel width, mean depth and mean velocity should all increase.

12 Land ice extent predicted by Gildor and Tziperman’s (2001) model in the northern polar box as a proportion of total land area. 11(b). The two polar boxes of the ocean may be covered by sea ice to variable extent. Each of the four atmosphere (a) Atmosphere SP 45°S EQ 45°N NP boxes had land, ocean, land ice or sea ice at its base, each with a specified reflection of the Sun’s energy. The land part of the polar boxes may (b) Ocean be covered by glaciers that can be of variable extent. Each model then used simple energy and mass balance equations.

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An Introduction to Physical Geography and the Environment by Joseph Holden


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