the molten iron core
The top layer is the crust, the next layer is the outer core, and the last layer is the inner core.
Temperature of about 5000 degrees Celsius Pressure of about 330GPa Radius of about 1200km It is solid It is a Nickel-Iron alloy Density of about 3000Kg/m^3
2 characteristics of the crust- the crust is composed of igneous, metamorphic, and sedimentary rock. It is the coolest layer for it is the first and farthest layer from the core.
The Outer Core is made up of a liquid iron and nickel alloy. This creates the earth's magnetic field. It is in a liquid form due to the intense heat given off by the inner core (which is 5500C due to the decay of radioactive elements such as uranium inside) It is roughly 2300 metres thick.
The core is extremely dense, heavy and very hot.
ur fricken mom
the molten iron core
displays all of the characteristics listed above
the molten iron core
The top layer is the crust, the next layer is the outer core, and the last layer is the inner core.
The core is a very dense region at the center of the earth that is composed largely of iron and, to a lesser extent, other metals such an nickel. The inner core is solid while the outer core is liquid. The liquid core convects and thus produces the earth's geodynamo.
the transistors were usedthe core memory was developedprogramming was in machine languagemagnetic taps and disc
litho = rocks It's everything outside the metallic core, up to the surface of the planet.
Lower mantle: Near outer coreInner core: Dense and solidOuter core: LiquidUpper mantle: Moves the crust
what is the lithshpere and describe it
Economists have identified regions of the world called core regions of economic development. The core regions are North America, Europe and Japan. China is not currently listed because it does not have the model as described below: The core regions have these characteristics; they have economic diversification; * The nations have a high standard of living; * They are leaders in technology;and * Productivity levels are high.