8-65km
A fault is a break in the Earth's crust where pieces of the crust move relative to each other. This movement can cause earthquakes as stress builds up along the fault line and is released suddenly. Faults are common in regions where tectonic plates interact and are essential for understanding earthquake hazards.
Crust
Block mountains are formed when geological faults cause blocks of the Earth's crust to move vertically, leading to the formation of tall mountain ranges. An example of a block mountain is the Sierra Nevada in California, USA. Rift valleys, on the other hand, are formed by the stretching and thinning of the Earth's crust, leading to the development of deep valleys. The East African Rift Valley is a well-known example of a rift valley.
The crust is typically thicker beneath continents compared to oceans. Continental crust can be up to 40 km thick, while oceanic crust is generally around 5-10 km thick.
OxygenOxygen is about 46% of Earth's crust.
The Earth's crust can vary in thickness, but on average it is about 5-70 kilometers (3-44 miles) thick. However, it can be much thicker under mountain ranges and thinner under the ocean floor.
The Earths crust is approximately 650 km deep.
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
mantle
The earth's crust is not stress
No, not all metals are found in the Earth's crust. While the Earth's crust contains a wide variety of metals, some metals are very rare and are not commonly found in geological formations. Additionally, some metals are found in concentrations that are too low to be economically viable for extraction.
half of earths layer
continental crust
The earth's crust is generally solid.
crust
The crust is the thinnest part on the Earth.
the crust and the core