Know one really knows who discovered the Earth's crust.
The earliest geologists were Islamic scholars in western Asia (circa 1000 AD), who studied how seas may have later become mountaintops. The idea of a separate "crust" atop an elastic mantle developed through the late 19th century, from observations of upthrust mountains, spreading seafloor and subduction along the edges of continents. German geologist Alfred Wegener first proposed the theory of continental drift in 1912.
The boundary between the crust and the mantle was discovered by Croatian seismologist Andrija Mohorovičić in 1909. This boundary is known as the Mohorovičić discontinuity or "Moho" and marks the change in seismic wave velocities between the Earth's crust and mantle.
The crust-mantle seismic discontinuity was discovered by Yugoslav seismologist, Andrija Mohorovičić, in 1909 through his observation of seismic waves. This discontinuity marks the boundary between Earth's crust and mantle, characterized by a sudden increase in seismic wave velocity.
The force of changing earth's crust is...... that the earth's crust is a lot thinner
The outermost layer, called the crust, is the thinnest layer of the earth.
The 2nd most abundant in the earth's crust and has 14 neutrons is silicon In 1824 Silicon was discovered by a Swedish chemist.
when the first man tripped and fell on it.
The earth's crust is called the crust because it the outer surface of the earth like the crust of pizza.
The boundary between the crust and the mantle was discovered by Croatian seismologist Andrija Mohorovičić in 1909. This boundary is known as the Mohorovičić discontinuity or "Moho" and marks the change in seismic wave velocities between the Earth's crust and mantle.
The crust is the top part of the Earth. It is where we live. The Earth's crust is 6 miles deep. That is the Earth's crust.
The crust is the top part of the Earth. It is where we live. The Earth's crust is 6 miles deep. That is the Earth's crust.
in the mantel
The crust-mantle seismic discontinuity was discovered by Yugoslav seismologist, Andrija Mohorovičić, in 1909 through his observation of seismic waves. This discontinuity marks the boundary between Earth's crust and mantle, characterized by a sudden increase in seismic wave velocity.
Crust and the upper mantle
In general the Earth's oceanic crust is thinner then the continental crust
the earth has a crust but the sun appears to not have a crust
The force of changing earth's crust is...... that the earth's crust is a lot thinner
The outermost layer, called the crust, is the thinnest layer of the earth.