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Folding (intermediate)

Lateral compressive forces cause rocks to form folds. This is how fold mountains are formed.

Ģeogrāfija

Atslēgvārdi

locīšana, reizes, sincline, reizes kalns, kalnu veidošana, vertikālas reizes, apgāztas reizes, lejupslīde, tektoniskā plāksne, rock slānis, spiedes spēks, Šūpoles, kalns, Dabaszinības, Ģeogrāfija

Saistītie vienumi

Faulting (basic)

Vertical forces can break up layers of rock into fault blocks, which then move vertically along the fracture planes.

Faulting (intermediate)

Vertical forces can break up layers of rock into fault blocks, which then move vertically along the fracture planes.

Folding (advanced)

Lateral compressive forces cause rocks to form folds. This is how fold mountains are formed.

Folding (basic)

Lateral compressive forces cause rocks to form folds. This is how fold mountains are formed.

Geyser

A geyser is a spring characterised by intermittent discharge of water and steam.

Topography of the Earth

The animation presents the largest mountains, plains, rivers, lakes and deserts of the Earth.

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