crust
No, because to reach the center of the Earth, they need to pass through the outer core. Secondary waves, or S-waves, can't pass through liquids, such as the liquid outer core, so they can't thus even reach the center of the Earth.
The principal divisions of the solid Earth based on compositional differences are the crust, mantle, and core. The crust is the outermost layer and is composed mainly of lighter elements like silicon and oxygen. The mantle lies beneath the crust and consists of denser silicate minerals. The Earth's core is located at the center and is primarily made up of iron and nickel.
The density of the Earth can be estimated by observing the time that seismic waves take to travel through it. Waves travel faster through denser objects leading to the conclusions that the Earth is density stratified with the most dense material at the center. The change in velocity of the seismic waves gives an estimate of the density of the material that it is traveling through. Knowing the depth of these composition changes allows us to calculate the volume of each particular compositional "shell" and a weighted average of these will give an estimate of the Earth's density.
Seismic waves are produced by earthquakes and travel through the Earth. These waves can be divided into two main types: body waves (P-waves and S-waves) that travel through the interior of the Earth, and surface waves that travel along the Earth's surface.
Earth's compositional layers refer to the different materials that make up the planet (crust, mantle, core), while its structural layers refer to the physical attributes and properties of these layers (lithosphere, asthenosphere, mesosphere, outer core, inner core). The compositional layers focus on the elements and compounds present, while the structural layers focus on how these layers behave and interact.
No, because to reach the center of the Earth, they need to pass through the outer core. Secondary waves, or S-waves, can't pass through liquids, such as the liquid outer core, so they can't thus even reach the center of the Earth.
the difference is that the earth's theory is similar to that of a hypotheses , structure and compositional layer of the earth.
Core Crust and Mantle
The principal divisions of the solid Earth based on compositional differences are the crust, mantle, and core. The crust is the outermost layer and is composed mainly of lighter elements like silicon and oxygen. The mantle lies beneath the crust and consists of denser silicate minerals. The Earth's core is located at the center and is primarily made up of iron and nickel.
The density of the Earth can be estimated by observing the time that seismic waves take to travel through it. Waves travel faster through denser objects leading to the conclusions that the Earth is density stratified with the most dense material at the center. The change in velocity of the seismic waves gives an estimate of the density of the material that it is traveling through. Knowing the depth of these composition changes allows us to calculate the volume of each particular compositional "shell" and a weighted average of these will give an estimate of the Earth's density.
mantle,crust,core
The crust, mantle, and core. :)
Light is a wave that travels through space across matter. The same way that waves travel from the center of a pond to the edges when you toss a stone in it.
No, because it's to hot for a human being or anything else to go to the center of the earth. I think
The densest layer of Earth's compositional layers is the inner core. Composed primarily of iron and nickel, it has a solid state due to the immense pressure at Earth's center, despite the high temperatures. The inner core is surrounded by the outer core, which is liquid and also primarily made of iron and nickel, but the solid inner core is denser than the surrounding layers.
Due to the huge amount of pressure and the lack of a purpose to travel to the center of the Earth, probably not.
S waves cannot travel through liquid. The Earth's core is liquid.