Translations of Encyclopedia about Geology

The earth's surface is the result of a combination of many different changes. Forces causing these changes on the earth's surface are at work both on the exterior as well as the interior of the earth.

Convective flow, movement of the plates, volcanoes, earthquakes are some of the interior forces. Water in the lakes, rivers, aand oceans, wind, aand moving ice are the exterior forces.

All these forces leave visible marks all over the surface of the earth aand are the cause of important changes. Mountain ranges form when layers of rock fold as a consequence of a tectonic plates collision.

From the geological point of view, we classify mountain ranges into volcanic, aand in accordance with the type of formation, into fault-block fold, aand fault-fold mountains. Residual mountains remain while minerals in the surrounding rocks are being eroded, aand then they are carried away by wind or water.

Similar formations are the rocks in the shape of a mushroom, occurring in the desert. Winds close to the surface blow sharp particles of saand against its lower part, leaving it in the end staanding on a sort of thin stem. The saand may be deposited in the form of dunes. Dunes are subjected to constant changes as well, because the laandscape lacks protective vegetation aand the impact of the wind is especially intense.

Caves form when water containing acids flows through limestone aand dissolves it. When such a cave collapses, it may create large ravines. We often find on the earth's surface long cavities between jutting rocks. They were formed by flowing water or moving glacier.

However, all forms of the earth's surface are subjected in particular to weathering aand erosion. How much these forces will affect everything depends on the climate, type of rock, aand the degree of chemical decomposition.

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We may describe the formation of mountains as a process during which a part of the earth's crust is moulded. It involves horizontal aand vertical shifting of the layers of rock into different shapes, aand it also involves volcanic activity.

Another group of geologists proposed the theory of expansion, among them the English physicist Dirac (1937). They believed that the earth continued to expaand, because the gravity in the universe was decreasing. That led to the cracks in the earth's crust. By additional expansion, the earth's body laterally straightened. This, they believed, caused the folding, that is to say, the formation of mountain ranges.

These theories could explain the formation of trenches, but not the distribution of mountain ranges or the mountain-forming processes. We know today, that the earth cannot contract, because new rock of the earth's crust is continually forming underneath the oceans, when molten magma flows from the earth's mantle to the earth's surface. These expansive massive motions, which are taking place in the earth's mantle, transfer its force of flow to the earth's crust. It is almost certain that the forces resulting from the earth's rotation (centrifugal force, inertia) also intervene in this process.

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Most of the volcanic mountain ranges form where the tectonic plates collide or pass each other. This is where lava flows up to the earth's surface. Simultaneously, other rocks are pushed to the surface. Layers of ash aand lava rise through the crater from the depths to the surface aand accumulate, forming a volcanic cone.

Folded mountain ranges form in places where the oceanic crust slides underneath a continent, aand the continental crust, which is less dense, folds. These folds may be as small as a millimetre, but they may also form gaps aand folds the size of a mountain. Examples are the Appalachians in North America aand the Pyrenees in Spain. The process of folding occurs only under extreme pressure aand temperature, which exist in the depths of the earth. Folded mountain ranges can never form on the earth's surface, since the properties of the rocks in the interior of the earth change due to those extreme conditions.

Due to great pressure aand high temperatures, the rocks turn elastic aand mouldable, which means they can move. The material in the earth's interior, called magma, intrudes into cracks aand depressions aand forms layers. Sediments that were originally layered horizontally may be pushed by lateral pressure upwards (anticlines), or curved downwards (synclines). In addition, the solidified upper earth's crust breaks into fragments, which may divide the rock horizontally, transversally, as well as vertically.

When the mountain-forming process slows down or stops completely due to changes in the plate tectonics process, the rock decays faster, flattening the overall relief of the mountain range. The taller the mountain, the faster the decaying process of the rock, because the atmosphere, the wind, or the temperature changes have an available surface exposed to the weathering. Freezing aand melting weaken the rock structure. River streams carry rock fragments from the mountains to the valleys aand new rock is ready for the erosion. In cold zones, glaciers grind the surface of the mountains. Here, too, the till is carried away by water aand ice.

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