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Faulting (basic)

Faulting (basic)

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

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Atslēgvārdi

vaina, vainas bloks kalni, kalnu veidošana, bloķēt, upthrust, grāvis, vainas terases, vainas līnija, Šūpoles, pieaug, dilstošā secībā, kalns, Dabaszinības, Ģeogrāfija

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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.

Folding (intermediate)

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

Continental drift on a geological timescale

The Earth's continents have been in constant motion during the history of the planet.

Topographic map of Hungary

This animation demonstrates the geographical regions of Hungary.

Vulkānisms

Šajā animācijā iepazīsiet dažādus vulkānu izvirdumu veidus.

Seafloor map

The boundaries of tectonic plates can be seen on the seafloor.

Terms of physical geography

This animation demonstrates the most important relief features, surface waters and their relevant symbols.

Tectonic plates

Tectonic plates can move in relation to each other.

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