compression
When a shift occurs in the Earth's crust, the energy can radiate as seismic waves. These waves travel through the Earth's interior and can be detected and measured by seismographs. Depending on the type of fault movement, the seismic waves produced can be either compressional (P-waves) or shear (S-waves).
The Earth's crust is mainly composed of oxygen, silicon, aluminum, and iron, along with smaller amounts of other elements like calcium, sodium, and potassium. It is divided into oceanic crust, which is thinner and denser, and continental crust, which is thicker and less dense.
equillibrium in earths crust such that the force tending to elevate land masses balance the forces tending to depress land masses equillibrium in earths crust such that the force tending to elevate land masses balance the forces tending to depress land masses
crust
Earth's crust is mostly made up of Silicon and Oxygen
compression
compression
compression
When Earth's crust is squeezed into a smaller space, it can lead to the creation of mountains through a process called crustal folding. This compression forces the rock layers to fold and uplift, resulting in the formation of mountain ranges. Over time, erosion can further shape these mountains.
The Earth's crust is destroyed when subduction occurs.
earthquakes
Aftershocks.
Most Faults Occur Where The Earths Crust Is Extended
Wrinkling of the Earth's crust, also known as tectonic folding, occurs when tectonic forces compress the Earth's surface, causing layers of rock to bend and deform. This process can lead to the formation of mountains, hills, and valleys as the crust is pushed together or squeezed. Wrinkling typically occurs at convergent plate boundaries, where tectonic plates collide, and is a key aspect of the geological processes that shape the Earth's landscape over time.
I found that folding happens
When a shift occurs in the Earth's crust, the energy can radiate as seismic waves. These waves travel through the Earth's interior and can be detected and measured by seismographs. Depending on the type of fault movement, the seismic waves produced can be either compressional (P-waves) or shear (S-waves).
volcanic mountain