orogeny and epeirogeny
The two types of Earth's crust are continental crust and oceanic crust. Continental crust is thicker, less dense, and composed mainly of granite, while oceanic crust is thinner, denser, and made up mostly of basalt.
The two types of Crust is the Continental Crust and the Oceanic Crust.
The lithosphere can have two main types of crust: continental crust and oceanic crust. Continental crust is thicker, older, and less dense than oceanic crust. Oceanic crust is thinner, younger, and denser, primarily composed of basaltic rocks.
Oxygen and silicon are the two most abundant elements in the Earth's crust. They make up about 75% of the Earth's crust by weight.
The two main types of crust are oceanic crust, which is denser and thinner, primarily composed of basaltic rock, and continental crust, which is less dense and thicker, mainly made up of granitic rock.
orogeny and epeirogeny
The two types of Earth's crust are continental crust and oceanic crust. Continental crust is thicker, less dense, and composed mainly of granite, while oceanic crust is thinner, denser, and made up mostly of basalt.
The two types of Crust is the Continental Crust and the Oceanic Crust.
Basalt and limestone.
The two types of deformation are elastic deformation and plastic deformation. Elastic deformation occurs when a material changes shape under stress but returns to its original form once the stress is removed. In contrast, plastic deformation occurs when a material undergoes permanent change in shape due to exceeding its yield strength, resulting in a new shape that does not revert when the stress is removed.
The two types of lithospheric crust are continental crust, which is thicker and less dense than oceanic crust, and oceanic crust, which is thinner and more dense than continental crust.
The lithosphere can have two main types of crust: continental crust and oceanic crust. Continental crust is thicker, older, and less dense than oceanic crust. Oceanic crust is thinner, younger, and denser, primarily composed of basaltic rocks.
Oxygen and silicon are the two most abundant elements in the Earth's crust. They make up about 75% of the Earth's crust by weight.
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.
Clay and Quartz!
Oceanic Crust & Continental Crust
The two main types of crust are oceanic crust, which is denser and thinner, primarily composed of basaltic rock, and continental crust, which is less dense and thicker, mainly made up of granitic rock.