The discovery of the Mohorovičić discontinuity (Moho) was based on the analysis of seismic waves that travel through the Earth. Scientists observed a change in the velocity of seismic waves at a certain depth, indicating a boundary between the Earth's crust and mantle. This discovery provided valuable insights into the structure and composition of the Earth's interior.
The discovery of moho was through seismic waves...There are two 2 waves namely, Primary and Secondary waves...Secondary waves cannot pass through liquid and gasses. Thus, There is an abrupt increase in the velocity of earthquake waves (specifically P- waves) at this point.
The discovery of the Mohorovičić discontinuity, or Moho, was primarily based on the observation of seismic wave travel times. Scientists noted that seismic waves traveled at different speeds through the Earth's layers; specifically, they accelerated significantly when passing from the Earth's crust into the underlying mantle. This abrupt increase in wave velocity indicated a boundary between the less dense rocks of the crust and the denser rocks of the mantle, thus identifying the Moho.
Andrija Mohorovicic discovered the Moho boundary, or Mohorovicic discontinuity, in 1909 by observing the travel times of seismic waves. He noticed a sudden increase in seismic wave velocity at a certain depth in the Earth's interior, which indicated a change in composition and density between the Earth's crust and mantle. This boundary was later named after Mohorovicic in recognition of his discovery.
The Moho , short for Mohorovicic discontinuity , is about 7 kilometers below the floor of the ocean and the MANTLE is the layer immediately beneath the Moho !
The Moho discontinuity is 31 miles/50KM thick.
The discovery of moho was through seismic waves...There are two 2 waves namely, Primary and Secondary waves...Secondary waves cannot pass through liquid and gasses. Thus, There is an abrupt increase in the velocity of earthquake waves (specifically P- waves) at this point.
FeaR is MoHo
The boundary at the bottom of the Earth's crust is called the Mohorovičić discontinuity, or more commonly, the Moho. It separates the crust from the underlying mantle based on differences in seismic wave velocities.
The Moho, or Mohorovicic Discontinuity, is the boundary between the crust and the mantle.
Assignment Discovery - 1992 Statistics and Data Analysis in Sports was released on: USA: 2007
"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.
Risk Analysis is based on both assets and facilities.
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.
Assignment Discovery - 1992 Probability and Data Analysis 5-19 was released on: USA: 4 October 2007
Which of the following integrates quantitative analysis into qualitative analysis, based on the above record of passengers?