answersLogoWhite

0


Best Answer

mantle and crust

User Avatar

Wiki User

βˆ™ 12y ago
This answer is:
User Avatar
More answers
User Avatar

AnswerBot

βˆ™ 1mo ago

crust and mantle, known as the MohorovičiΔ‡ discontinuity or Moho. This boundary is where seismic waves change speed, indicating a transition between the Earth's outermost solid layer (crust) and the underlying denser layer (mantle).

This answer is:
User Avatar

Add your answer:

Earn +20 pts
Q: The propagation of seismic waves through the Earth's interior provides evidence of internal layering the first boundary discovered was the boundary between the?
Write your answer...
Submit
Still have questions?
magnify glass
imp
Related questions

Boundary between earth's crust and mantle?

It is called the Mohorovičić discontinuity or the Moho for short.It was one of the fist features of the Earth's interior that was discovered using seismic waves. In 1909, Andrija Mohorovicic discovered this boundary and it was named in his honor.


What is the synonym and antonym of plate boundary?

Synonym: Tectonic boundary Antonym: Interior boundary


What is the boundary between the interior and the exterior of the cell?

Plasma membrane


What is the boundary between the interior and exterior of the cell?

Plasma membrane


Who discovered Gutenberg Discontinuity?

The Gutenberg Discontinuity was discovered by Beno Gutenberg and Charles Francis Richter in the early 20th century. It is a boundary within the Earth's interior where seismic waves change velocity, indicating a change in composition between the outer core and the lower mantle.


Who discovered the interior of Africa?

The British


What are interior points in geometry?

For a closed shape, they are point inside its boundary or perimeter.


What is the difference between interior optimum and boundary optimum?

The interior optimum method uses an a choice that is determined by the position of an agent at a tangency that rests between the curves of two points on a graph. The boundary optimum method analyzes the position of waves.


Geologists learn about Earths interior using indirect evidence from?

Geologists learn about Earth's interior using indirect evidence from seismic waves, magnetic field data, and rock samples from volcanoes and deep drilling. These methods help provide insights into the composition, structure, and properties of Earth's interior layers.


How to describe one way in which geologists have gained indirect evidence about earths interior?

Studying how seismic waves refract inside the earth and if they "cast shadows" indicating that some layers inside earth are opaque to some types of seismic waves. Seismic waves "illuminate" the interior of the earth like light waves illuminate a room, permitting what is there to be seen if you have the correct tools to observe them.


Difference between boundary fill and flood fill?

boundaryfill fills area till the single boundary color is reached whereas floodfill fills area not defined by single boundary colourfloodfill replaces interior colour instead of searching for boundary colour


How do you obtain indirect evidence about earths interior?

Seismic waves