have a lower average density
Geologists use seismic waves to map the Earth's interior. By studying how these waves travel through the Earth, geologists can infer information about the composition and structure of different layers beneath the surface. This helps them understand the different layers of the Earth, such as the crust, mantle, and core.
earthquakes happen when sections of the earths crust shift.These shifting parts called plates,are actually pieces of the crust floating on the hot molten interior of the earth. The majority of earthquakes happen along the edges of those plates,and along weak areas of the crust called fault zones
they are crust and the mantle and also the core
the mantle, which contains the lithosphere, asthenosphere and the mesosphere
The Earth's crust is the thinnest part of Earth's interior, ranging from about 5-70 kilometers (3-44 miles) in thickness. It is divided into two types: continental crust, thicker and less dense, and oceanic crust, thinner and more dense.
it depends on the deepth
Water
when the crust breacks apart it reveles objects beneth earths iner crust.
earthquakes happen when these sections of earths crust move
it depends on the deepth
it depends on the deepth
Geologists use seismic waves to map the Earth's interior. By studying how these waves travel through the Earth, geologists can infer information about the composition and structure of different layers beneath the surface. This helps them understand the different layers of the Earth, such as the crust, mantle, and core.
it means earthquakes will happen more often
earthquakes happen when sections of the earths crust shift.These shifting parts called plates,are actually pieces of the crust floating on the hot molten interior of the earth. The majority of earthquakes happen along the edges of those plates,and along weak areas of the crust called fault zones
Rock samples
oceanic crust is made of basalt while continental crust is made of silica rich rocks like granite.
The mantle