mantle
Crust and Mantle.
Every discontinuity inside the earth can reflect seismic waves. These occur between major layers (crust, mantle, outer core, inner core) and are named after scientists (Mohorovicic and Gutenberg for example).
Seismic waves can dramatically change in velocity and direction when they encounter boundaries between different types of rock or geological formations. These changes, known as refraction and reflection, occur at interfaces with contrasting physical properties, leading to the bending or bouncing of seismic waves. The behavior of seismic waves at these boundaries provides valuable information about the Earth's interior structure.
tides will occur.
tides will occur.
at boundaries between moving parts of the crust
Volcanoes occur at divergent and convergent plate boundaries due to the fact that crust is either being destroyed or created. Volcanoes also occur at hotspots, for example in Hawaii. Hotspots occur where the crust is particularly thin or weak, and plumes of magma rising from the asthenosphere (between upper mantle and the crust) end up giving rise to volcanoes or volcanic islands.
Where crust is destroyed
The crust is the upper layer of the earth. It is where the movement of plates occur due to which earthquakes occur. The Earth's crust is a thin layer of rock, like skin on an apple.
The crust is compressed into mountains (if it is continental crust) or subducted back into the mantle if it is oceanic crust.
A continuous spectrum contains all the wavelengths. A discontinuous spectrum has stripes of specific colors and can be used to identify the elements making it
the crust