The Kola Superdeep Borehole project (in the USSR) attempted to drill as deep as possible into the Earth's crust. Drilling began on 24 May 1970 and the deepest hole, SG-3, reached 12,261 metres (40,230 ft) in 1989. Earlier, in 1961, an attempt was made to reach the Mohorovicic Discontinuity, the boundary between the earth's crust and mantle, by drilling through the oceanic crust. The US, through the National Science Foundation, sponsored Project Moho, which drilled 601 feet into the crust, beginning 11,700 feet below the ocean surface.
The deepest scientist have been able to study earths interior depth is 12,262 meters
The coolest layer of the Earth is the lithosphere, which is the rigid outermost layer consisting of the crust and upper mantle. This layer's temperature decreases with depth, making it the coolest part of the Earth's structure.
1. we would never be able to get down to the bottom to the core because we dont have the machineary and if we got past the earths crust hot molten lava would pour out and destroy the country. 2. if we mined the earths core it would be so hot no thing could survive it and we couldn't mine it because it is extremely hard
Metal is more dense than rock. Early in the history of the Earth, the whole planet was very hot and everything was liquid, and the heavier liquid components of the planet were able to sink through the lighter liquids which floated to the top. We think of rock such as granite as being very dense, but everything is relative. Granite is less dense than iron, and it floats on top.
The crust. We have not been able to access the other layers.
miners have been able to dig into the earths crust by big machines and other huge tools and they have only dig ed 2 miles into the earths crust
equillibrium in earths crust such that the force tending to elevate land masses balance the forces tending to depress land masses equillibrium in earths crust such that the force tending to elevate land masses balance the forces tending to depress land masses
You are already closer to the earths core than you will ever be able to get to the sun
The deepest scientist have been able to study earths interior depth is 12,262 meters
If the court requires they sell certain things at auction, you are as able to bid on them as anyone. And anyone can out bid you.
Oxygen, though usually a gas, is still in a molecule form and can be bonded to with any other molecule that is able to do so. Oxygen is a very common element in the crust because many rocks and more importantly minerals that make up those rocks use it in there atomic bonds. A simple example is Quartz, SiO2 So each single structure has one silicon atom and two oxygen atoms.
it is floating on it
Microwave rays can pass through the Earth's atmosphere, as they are a form of electromagnetic radiation that is not absorbed or blocked by gases in the atmosphere. This is why microwave communication systems like satellites are able to transmit signals through the atmosphere.
Anyone is able to advertise on Google. Users can set up their advertisement themselves through the Google Ads website, or by calling Google for assistance.
when the moon passes through the earths shadowAt a full moon... the Earth casts a shadow on the moon causing it to appear reddish brown.
The coolest layer of the Earth is the lithosphere, which is the rigid outermost layer consisting of the crust and upper mantle. This layer's temperature decreases with depth, making it the coolest part of the Earth's structure.
The mantle is under high pressure and high temperature, which helps maintain its volume even as the crust thickens or thins. The mantle is a semi-fluid layer that can flow and adjust to changes in the crust without significant changes in its overall volume. As the crust thickens, the mantle can undergo convection to redistribute its mass and maintain equilibrium.