The presence of marine fossils found high above sea level is a key indicator of crustal uplift. Additionally, the presence of erosional features such as river valleys in mountainous regions suggests uplift has occurred. Geological structures like fault blocks and folds also provide evidence of crustal uplift.
Fold moutains are actually formed by crust which have been uplifted and folded by compressional forces. This occurs along convergent plate boundaries where 2 plates move towards each other, between continental plates or between an oceanic and a continental plate. The crust and the rocks get bent and crumpled, and massive layers of Earth's crust gets uplifted as a result, forming spectacular fold mountains. More well-know examples of fold mountains are the Himalayas in Asia and the Andes in South America.
A crack in the Earth's crust is a fracture where rocks have pulled apart, whereas a fault is a fracture where there has been movement along the fracture plane. In other words, a fault is a type of crack in the Earth's crust that has undergone displacement.
Fossils are the remains of living things that have been preserved in the Earth's crust. These can include bones, shells, plants, and traces of organisms such as footprints or burrows. Fossils provide valuable information about ancient life forms and environments.
Earth's earliest crust, which formed over 4 billion years ago, has been recycled through processes like subduction, where it is pulled back into the mantle. This constant recycling of Earth's crust, along with the effects of erosion and weathering, means that no original pieces of the earliest crust remain intact today.
Peridotite is typically found in the upper mantle of the Earth. It can also be found in ophiolite complexes, which are sections of oceanic crust that have been uplifted and exposed on land through tectonic processes. Additionally, peridotite can sometimes be found in areas of ancient continental crust that have been deeply eroded.
miners have been able to dig into the earths crust by big machines and other huge tools and they have only dig ed 2 miles into the earths crust
it has been washed into the oceans as the continental crust has eroded.
Fossils
Fossils
rejuvenated
Yes, Fold mountains are actually formed by crust which have been uplifted and folded by compressional forces. This occurs along convergent plate boundaries where 2 plates move towards each other, between continental plates or between an oceanic and a continental plate. The crust and the rocks get bent and crumpled, and massive layers of Earth's crust gets uplifted as a result, forming spectacular fold mountains this is how the Andes are formed.
Fossils, although technically they are not preserved in the earths crust; the minerals in the bones and pore spaces have been replaced by other harder minerals which take much longer to weather.There are a number of different fossilization processes. See this link :How are Fossils Formed?
A plateau.
Uplifted mountains are formed through the collision of tectonic plates, which creates immense pressure and forces the landmass to rise. This process can take millions of years as the Earth's crust is pushed upwards, resulting in the formation of mountains. Erosion and weathering can further shape and expose these uplifted mountains over time.
a mountain
Many elements and materials which could not have been produced any other way (like diamonds).
No, Earth's crust movement has been occurring for billions of years as part of the process of plate tectonics. The movement of the Earth's crust has shaped the planet's surface and continues to do so over long geological timescales.