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Folding (advanced)

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

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Atslēgvārdi

locīšana, reizes, sinclines, anticline, sincline, reizes kalns, kalnu veidošana, plāksnes tektonika, sedimentu baseins, nogulsnes, tektoniskā plāksne, spiedes spēks, Šūpoles, kalns, rock slānis, 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 (basic)

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

Folding (intermediate)

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

Torsion balances

A force can be measured by measuring the twisting of the torsion wire in a torsion balance.

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