the crust then comes the mantel the inner layer then core
Rock is the most abundant material in the crust.
There are two types of crust's. I dont know which one you are talking about, but it is probably the continental crust. The other type of crust is the Oceanic crust. The first continental crust is about 4-7 miles (6-11 km) thick and mainly consists of heavy rocks, like basalt. The Continental crust is thicker than the Oceanic crust, about 19 miles(30 km) thick. It is mainly made up of light material like granite.
First Nations theory often views the Earth as a living entity, with the crust being a key element in this interconnected ecosystem. The theory emphasizes the importance of honoring and preserving the Earth's crust as sacred and essential for the well-being of all living beings. It highlights the need for sustainable practices that respect the Earth's crust and its vital role in supporting life.
The density and thickness of the earth crust varies depending on if you are looking at oceanic or continental crust. The oceanic crust's density averages to around 2900 kg/m3 and ranges from 7 to 10 kilometers thick. The continental crust's density averages to around 2700 kg/m3 and ranges 25 to 70 kilometers thick.
The first layer beneath the Earth's crust is called the mantle. The mantle extends to a depth of about 2,900 kilometers (1,800 miles) and is composed of semi-solid rock that can flow slowly over geological time. It is divided into the upper mantle and the lower mantle, with the upper mantle being more rigid and the lower mantle exhibiting more fluid-like behavior.
Rock is the most abundant material in the crust.
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Edwin L. drake
No one invented metal. Metals are naturally occurring elements in the earths crust (and core)
The Earths three layers are : Crust - the first layer of the earth Mantle - the second layer of the earth which is closest to the core. Core - the hottest and inner most layer of the earth.
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.
There are two types of crust's. I dont know which one you are talking about, but it is probably the continental crust. The other type of crust is the Oceanic crust. The first continental crust is about 4-7 miles (6-11 km) thick and mainly consists of heavy rocks, like basalt. The Continental crust is thicker than the Oceanic crust, about 19 miles(30 km) thick. It is mainly made up of light material like granite.
Continental crust is the thicker, less dense, and older type of crust found beneath continents, primarily composed of granite and sedimentary rock. Oceanic crust is the thinner, more dense, and younger type of crust located beneath oceans, primarily composed of basalt. The boundary between continental and oceanic crust is known as the continental-oceanic crust boundary.
The two outer layers of the Earth are called the crust and the mantle. The crust is the outermost layer, while the mantle lies beneath the crust and makes up the largest portion of the Earth's interior.
The Earth's crust is the outermost solid layer of the Earth, forming the Earth's surface. It is found beneath the oceans and continents and varies in thickness, with the oceanic crust being thinner than the continental crust.
First Nations theory often views the Earth as a living entity, with the crust being a key element in this interconnected ecosystem. The theory emphasizes the importance of honoring and preserving the Earth's crust as sacred and essential for the well-being of all living beings. It highlights the need for sustainable practices that respect the Earth's crust and its vital role in supporting life.
The density and thickness of the earth crust varies depending on if you are looking at oceanic or continental crust. The oceanic crust's density averages to around 2900 kg/m3 and ranges from 7 to 10 kilometers thick. The continental crust's density averages to around 2700 kg/m3 and ranges 25 to 70 kilometers thick.