What is a discontinuity in geology?
Answers
Answered by
1
A discontinuity in geotechnical engineering (in geotechnical literature often denoted by joint) is a plane or surface that marks a change in physical or chemical characteristics in a soil or rock mass. ... A discontinuity makes a soil or rock mass anisotropic.
Answered by
1
Discontinuities are the boundaries in the earth which indicate difference in velocity in seismic wave.
Explanation:
- Discontinuity is a geological term.
- Discontinuities can be defined as the boundaries inside the earth.
- These boundaries are marked by the abrupt changes in the seismic waves.
- There are basically five types of discontinuities.They are:-
- Conrad Dicontinuity
- Mohorovicic Discontinuity
- Repetti Discontinuity
- Gutenberg Discontinuity
- Lehmann Discontinuity
- Conrad Discontinuity: It lies between that lies between transition zone between the SIAL and SIMA.
- Mohorovicic Discontinuity: It lies between transition zone between the crust and Mantle.
- Repetti Discontinuity: It is the transition zone that lies between outer mantle and inner mantle.
- Gutenberg Discontinuity: It is the transition zone between the mantle and core.
- Lehman Discontinuity: It is the transition zone between the outer core and inner core.
Similar questions