Seismology - echo patterns of sound waves traveling through the earth.
Seismology - echo patterns of sound waves traveling through the earth.
Volcanoes allow the molten lava from the outer core to pass through weak spots in the mantle.
Because of the difference/wavering in the earths magnetic field due to thwe fact the inner core is largely Iron....
For one, the magnetic field changes continuously; this is not consistent with a permanent magnet.
if you are talking about the earth here is the answer. The earth is made up of many parts. The outside is called the crust the crust is the thinest part of the earth. The crust is made up of the continental crust and the oceanic crust. The oceanic crust is 3.0 grams/cm squared dense. The continental crust is 2.7 grams/cm squared dense. Other parts of the earths interior are the asthensophere "plastic mantle", stiffer mantle, outer core, and the inner core. We know that the outer core is liquid because a waves do not travel through it, and a waves only don't travel through liquid. These are the components that make up the earths interior.
if you are talking about the earth here is the answer. The earth is made up of many parts. The outside is called the crust the crust is the thinest part of the earth. The crust is made up of the continental crust and the oceanic crust. The oceanic crust is 3.0 grams/cm squared dense. The continental crust is 2.7 grams/cm squared dense. Other parts of the earths interior are the asthensophere "plastic mantle", stiffer mantle, outer core, and the inner core. We know that the outer core is liquid because a waves do not travel through it, and a waves only don't travel through liquid. These are the components that make up the earths interior.
i dont know what kiwi contains but it is a example of the earths layers. the skin would be the crust the pulp would be the mantel and the seeds would be the outer core and the middle part would be the inner core.
they take plants and animals to the lab and experiment
i dont know dhiss shidd mane..........................
Scientists have studied the Earth's core extensively using seismic waves and magnetic field measurements. The data show that the Earth's core is primarily made of molten iron and nickel, rather than a solid permanent magnet. Additionally, the Earth's magnetic field is generated by the movement of molten metals in the outer core, not by a single large permanent magnet in the core.
From the Wikipedia: "The outer core of the Earth is a fluid layer about 2,300 km ... thick" - With current technology, it isn't possible to go that deep AT ALL.If you just want a calculation based on a hypothetical machine, assume some speed, and then divide the distance by the speed.
the outer core is above earths solid inner core and below its mantle this is the outer part but not the crust and it would feel pretty warm to go through this area. ok well i hope this helped this is all i know.!:)