600 degrees Celsius. Which would be 1,112 degrees Fahrenheit.
"moho" is the plate boundary between earth's crust and the mantle.
ummm hello! its just the moho layer! the moho layer is the boundary between the mantle and the crust!there is absolutely no boundary between the moho layer and the mantle! you think i am wrong? then drill to the moho layer and find out!
No, the Outer Core is not known as the Moho. The Moho, short for Mohorovicic Discontinuity, is the boundary between the Earth's crust and mantle, while the Outer Core is a layer of molten iron and nickel that surrounds the Earth's solid inner core.
The Moho separates the crust and the mantle.
The core is actually located beneath the Earth's mantle. The layer immediately beneath the Moho is the Earth's mantle, which is a region of hot, flowing rock that lies between the crust and the outer core.
The temperature of the Moho discontinuity is estimated to be around 500 to 900 degrees Celsius. This high temperature is due to the increased heat coming from the Earth's interior, causing the rocks to be partially melted along this boundary.
FeaR is MoHo
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.
The Moho, or Mohorovičić discontinuity, is approximately 600 to 800 degrees Celsius (about 1100 to 1500 degrees Fahrenheit) in temperature. This boundary between the Earth's crust and mantle is significant as it marks a change in composition and seismic properties.
"moho" is the plate boundary between earth's crust and the mantle.
No. The Moho is simply the boundary between the mantle and the crust.
ummm hello! its just the moho layer! the moho layer is the boundary between the mantle and the crust!there is absolutely no boundary between the moho layer and the mantle! you think i am wrong? then drill to the moho layer and find out!
The Moho is an abbreviation of the Mohorovicic Discontinuity, the boundary between the crust and the upper mantle.
Moho
Andriza Mohorivicic
Moho
No, the Outer Core is not known as the Moho. The Moho, short for Mohorovicic Discontinuity, is the boundary between the Earth's crust and mantle, while the Outer Core is a layer of molten iron and nickel that surrounds the Earth's solid inner core.