Jūsu grozs ir tukšs

Pirkt

Skaits: 0

Kopā: 0,00

Faulting (intermediate)

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

Ģeogrāfija

Atslēgvārdi

vaina, plāksnes tektonika, kalnu veidošana, vainas bloks kalni, bloķēt, upthrust, grāvis, vainas terases, baseins, tektoniskā plāksne, vainas līnija, Šūpoles, pieaug, dilstošā secībā, 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.

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.

Terms of physical geography

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

The development of lakes

Standing bodies of water can form in depressions on the surface by both endogenic and exogenic forces, as well as by human activity.

Topography of the Earth

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

Waterfalls

Waterfalls form where a river flows over a steep precipice in its course.

Added to your cart.