Ajedrez de entrenamiento by Alexander Koblenz PDF

By Alexander Koblenz

ISBN-10: 8427000472

ISBN-13: 9788427000476

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1. LANDSCAPE ELEMENTS AND PROPERTIES Views which suggest that humid tropical landforms differ little from their temperate counterparts emphasise that both are fluvially carved landscapes subject to chemical weathering and the laws of water flow. This is correct but unhelpful; in the same way that it would be specious to argue that all vegetation responds to the DNA code and grows by a common process involving photosynthesis. This is, firstly, because the weathered mantle is thicker, more pervasive and has distinctive properties in hurnid tropical areas (Deere and Patton 1971; Geological Society 1990; Thomas 1994), and, secondly, because the pathways of water flow and their effects on the erosional system are strongly influenced by the weathered layer and also by distinctive soil structures.

Significant change in volume Completely weathered All rock material decomposed andlor disintegrated to soil. Original mass structure still largely intact IV Highly weathered More than 50% of rock material decomposed and/or disintegrated to soil. Fresh/discoloured rock present as discontinuous framework or corestones 111 Moderately weathered 11 Slightly weathered Less than 50% of rock material decomposed and/or disintegrated to soil. Fresh/discoloured rock present as continuous framework or corestones Discolouration indicates weathering of rock material and discontinuity surfaces.

Thus, the widespread deep chemical alteration of rocks outside of mountainous regions reduces the availability of coarse bedload and increases tbe proportion of sand reaching the river. Bank erosion and landslides reaching the channel can also inject quantities of fine suspended sediment, much of it clay, into the stream. Tropical floodplains are, therefore, frequently dominated by fine grained sediments: mainly sandy, channel sediments and thick, c1ayrich overbank deposits. Exceptions, however, are common, because coarse cobbles and even boulders can form the stream bed in steep and rocky terrain, as in other parts of the world.

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Ajedrez de entrenamiento by Alexander Koblenz

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