The amount of gravity the moon has.
The earth's mass is increasing slightly. Not much gets out of the gravity well except what we launch, and we are the subject of falling rocks on a 24/7/365 basis.
Moon rocks resemble rocks from the Earth's crust layer. They are predominantly composed of igneous rocks like basalt and anorthosite, similar to those found on Earth's crust.
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Moon rocks are very similar to earth rocks an they are not intrinsically magnetic.
The mean density of the Moon is around 3.34 g/cm³, which is similar to the densities of mantle rocks found on Earth. The Moon's composition is primarily made up of silicate rocks similar to those found in the Earth's mantle, which contributes to its comparable density.
thickness 1/8( a mixture of lighter and heavier rocks which were forced out from the mantle by volcanic activity)
As the earth formed, the heavier, more dense elements sunk toward the center, while the lighter, less dense ones stayed near the surface. The result was layers of rocks of similar density.
As the earth formed, the heavier, more dense elements sunk toward the center, while the lighter, less dense ones stayed near the surface. The result was layers of rocks of similar density.
The main theory on the continental divide is that they relate to the plate techonics theory of the Earth's crust. The other theory is the continental drift theory where lighter rocks float on heavier crustal material.
Dark igneous rocks usually have higher amounts of heavier elements such as iron. Light-colored igneous rocks tend to be richer in lighter elements like sodium and aluminum.
As the earth formed, the heavier, more dense elements sunk toward the center, while the lighter, less dense ones stayed near the surface. The result was layers of rocks of similar density.
The earth's mass is increasing slightly. Not much gets out of the gravity well except what we launch, and we are the subject of falling rocks on a 24/7/365 basis.
Earth's layers were formed through a process called differentiation, which occurred during the early stages of the planet's formation. As rocks melted due to intense heat from radioactive decay and impacts, denser materials sank towards the center to form the core, while lighter materials rose to the surface to form the crust and mantle. This process created distinct layers based on the density of the materials.
To begin with the Earth was like a ball of hot bubbling liquid of rocks made from different elements and compounds. Some rocks were heavier than others. The heavy rocks started to sink and moved towards the center of the earth. Lighter rocks moved towards its surface. This separation of layers took millions of years. The present day Earth comprises the crust, the mantle and the core.
Continental crust is generally lighter in color than oceanic crust. This is because continental crust is composed of lighter-colored rocks such as granite, which contain lighter minerals like quartz and feldspar. In contrast, oceanic crust is made up of darker-colored rocks like basalt, which contain heavier minerals like pyroxene and olivine.
A composite or stratovolcano typically has light and heavy rocks. These types of volcanoes are characterized by alternating layers of lava flows and volcanic ash, which can contain both lighter materials like pumice and heavier rocks like basalt.
The Earth's surface is covered by two types of crust: continental crust and oceanic crust. Continental crust is thicker and less dense, primarily composed of lighter rocks like granite, while oceanic crust is thinner and more dense, mainly composed of heavier basaltic rocks. As a result, oceanic crust is denser than continental crust.