Complete answer:Rock cycle is a group of changes that enable sedimentary, igneous and metamorphic rocks to transform from kind to another through processes like melting, cooling, eroding, compacting and deforming. Igneous rock is the primary rock which is formed by cooling of magma.

Sedimentary rocks are the product of 1) weathering of preexisting rocks, 2) transport of the weathering products, 3) deposition of the material, followed by 4) compaction, and 5) cementation of the sediment to form a rock. The latter two steps are called lithification.

Rocks on the Earth’s surface are gradually broken down into smaller pieces by water, ice, wind, plants and animals (known as weathering). These broken up pieces are called sediment and are transported away, or eroded, by rivers, glaciers and wind.

There are three main types of rocks: sedimentary, igneous, and metamorphic. Each of these rocks are formed by physical changes—such as melting, cooling, eroding, compacting, or deforming—that are part of the rock cycle. Sedimentary rocks are formed from pieces of other existing rock or organic material.

Answer: Any natural mass of mineral matter that makes up the earth’s crust is called a rock. The earth’s crust is made up of various types of rocks of different texture, size and colour.

Three main layers are classified into the Earth-Crust (outermost), mantle and core (innermost).

If we subdivide the Earth based on rheology, we see the lithosphere, asthenosphere, mesosphere, outer core, and inner core. However, if we differentiate the layers based on chemical variations, we lump the layers into crust, mantle, outer core, and inner core.

The mantle

There are three main sources of heat in the deep earth: (1) heat from when the planet formed and accreted, which has not yet been lost; (2) frictional heating, caused by denser core material sinking to the center of the planet; and (3) heat from the decay of radioactive elements.

crust

Mesosphere

thermosphere

Earth’s interior is made of several layers. The surface of the planet, where we live, is called the crust—it’s actually a very thin layer, just 70 kilometres deep at its thickest point. Deep in the centre of the planet is the ‘inner core’, which we think is made of solid iron and nickel.

40,230ft

Earth’s crust is divided into two types: oceanic crust and continental crust. The transition zone between these two types of crust is sometimes called the Conrad discontinuity. Silicates (mostly compounds made of silicon and oxygen) are the most abundant rocks and minerals in both oceanic and continental crust.

Earth Crust: Oceanic Crust vs Continental Crust. Earth’s crust is all around us. Actually, it’s the layer we live on.

Continental crust

Seven years of satellite temperature data show that the Lut Desert in Iran is the hottest spot on Earth. The Lut Desert was hottest during 5 of the 7 years, and had the highest temperature overall: 70.7°C (159.3°F) in 2005.

Crust, mantle, core, lithosphere, asthenosphere, mesosphere, outer core, inner core.