Pressure waves passing through the liquid outer core are?

are decelerated and deviated at the core limit

Explanation:

P-waves travel through the fluid layers of Earth's interior, and yet are slightly refracted as they pass through the transition between the semi-solid mantle and the outer core liquid. As a result, there is a P "shadow zone" wave between 103 ° and 142 ° from the focus of the earthquake, where the initial P waves are not recorded in the earthquake. In contrast, S-waves do not travel through liquids; instead, they are attenuated.

because the asteroid belt is between the mars and jupiter orbits, it is around 2.2 to 3.2 astronomical units (au) from the sun – which is approximately 329,115,316 to 478,713,186 km. the average distance between objects is a massive 600,000 miles.

explanation:

bc blah

explanation:

bc blah