The Earth's core is that portion of the Earth which is composed primarily of iron (86 %) and Nickel (10 %) with a mixture of other elements making up the remainder.
The Earth's core is split into two. The outer core, which is a liquid and the inner core, which is a solid.
The Earth's core has a radius of approximately 3470 kmA with a total volume of 1.7502x1011 km3
This is separated into the inner and outer core with dimensions as follows:
The inner core has a radius of 1220 kmA extending from the centre of the Earth approximately 6370 km below Earth's surface to 5150 km below the surface (the change from inner to outer core is marked by a density change known as the Lehmann discontinuity). The inner core has a total volume of 7.4207x109 km3.
The outer core is approximately 2260 km thick extending from 5150 km below Earth's surface to 2890 km (the core mantle boundary or Gutenberg discontinuity) The outer core has a volume of 1.6760x1011 km3.
Geophysicists believe that convection currents in the liquid outer core are responsible for Earth's magnetic field. It is also thought that the very high difference in temperature between the outer core and the mantle is responsible for the creation of deep mantle plumes which in turn cause hot spot volcanism such as that occurring in Iceland and Hawaii. There is however some debate about the existence of deep mantle plumes occurring within the geophysics community.
For more information on the Earth's core, please see the related links.
Source:
A - Wilson, M. (2000). Igneous Petrogenesis - A Global Tectonic Approach. Chapmen & Hall, London.
The Earth's core is divided into two parts: the outer core, which ranges from about 2,200 to 3,200 kilometers (1,367 to 1,988 miles) below the Earth's surface, and the inner core, which extends from about 3,200 to 5,150 kilometers (1,988 to 3,200 miles) deep. The inner core is believed to be a solid ball of iron-nickel alloy, while the outer core is thought to be in a liquid state.
The earth's inner core is 3160 kilometers beneath the earths surface. The inner core is a solid ball of nickel-iron alloy.
The inner core of the Earth is thought to be a solid sphere made primarily of iron and nickel, with temperatures reaching up to 5,700 degrees Celsius.
Oh, dude, the inner mantle is definitely hotter than the outer mantle. Like, we're talking about temperatures reaching up to 4000°C in the inner mantle compared to a measly 500-900°C in the outer mantle. So, if you're looking for a hot spot, the inner mantle is where it's at.
The layer just above the Earth's center is the outer core. It is composed of molten iron and nickel, and it surrounds the solid inner core. The outer core is responsible for generating the Earth's magnetic field.
the inner part of earths core
The radious of the inner core is 1,220km(760miles).
The inner core Is solid and the outer core in liquid
Yes earths inner core is a dense ball of metal earths outer core is a layer of molten (melted) metal
The immense pressure from the layers outside of the inner core.
iron and nickel is the answer and so is the inner core. the inner and the outer and together but the outer core is liquid and the inner core is solid
The solid inner and liquid outer core.
The Earth's core is divided into two parts: the outer core, which ranges from about 2,200 to 3,200 kilometers (1,367 to 1,988 miles) below the Earth's surface, and the inner core, which extends from about 3,200 to 5,150 kilometers (1,988 to 3,200 miles) deep. The inner core is believed to be a solid ball of iron-nickel alloy, while the outer core is thought to be in a liquid state.
8 feet deep
They go faster through the inner core than the liquid outer core
The earths inner core is thought to be approximately 5778 K (5505 °C)
a solid ball of iron