Seismic wave measurements, particularly the behavior of P-waves and S-waves as they travel through the Earth, provide insights into the outer core's size. P-waves can pass through both solids and liquids, while S-waves only travel through solids. The absence of S-waves in certain areas indicates that those regions are liquid, allowing scientists to infer the outer core's boundaries. By analyzing the travel times and paths of these waves, researchers can estimate the depth and size of the outer core.
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There is no distance between the two : the outer core is on top of the inner core of the Earth. The inner core is considered to be about 2440 km (1520 mi) in diameter, or the region up to about 1220 km from the center. The outer core extends about another 2266 km (1408 mi) outward, from around 1220 to 3486 km from the center. The outer core is therefore about 5150 km from the surface at sea level, this distance comprising the mantle (lower and upper) and the crust.
Yes, Jupiter is believed to have a dense core of rock and metal about the size of Earth. This core is thought to be surrounded by a thick layer of metallic hydrogen, followed by a gaseous outer layer.
A seismograph is used to sense seismic waves in the earth. The seismic waves are sent down by scientist and how fast and how straight the line is when the seismograph reads them is how they tell which mineral or if its a liquid or solid. Which is how they know about the inner and outter core, and the mantel.
The description matches the size and composition of the Earth's core. It consists of a solid inner core primarily composed of iron and nickel, with a diameter of about 1,220 km and surrounded by a liquid outer core.
The sizes of Earth's inner core, outer core, and mantle are determined through seismic studies, which analyze how seismic waves travel through the different layers of the Earth. Scientists study the speed of seismic waves and how they bend or refract as they travel through the Earth to determine the size and composition of these layers.
yes
The outer core lies at a depth from 2900 km to 5150 km.
The size of the earth is 2521 KM to 5150 KM.
No, the Earth's core is not the size of Mars. The core is actually divided into the outer core and inner core, the inner core being about the size of Earth's moon. Mars, on the other hand, has a much smaller core compared to Earth.
The moon's core is thought to be partially liquid, but not necessarily "large" compared to the moon's overall size. The liquid outer core is believed to be small relative to the size of the moon as a whole.
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The size and shape of the Earth's core can be used to measure its properties by studying seismic waves that pass through the Earth. By analyzing how these waves travel and are affected by the core's size and shape, scientists can determine important properties such as density, composition, and temperature of the core.
As the diameter of the liquid core increases, the size of the shadow zone decreases. This is because the larger diameter allows for more refraction of seismic waves, leading to less complete shadowing of seismic waves at certain distances.
The size of the moons electro-magnetic field is proportional to the composition of it's core(not unlike an iron core from a electromagnet), the insulation of the core to the outer surface(not unlike the outer windings of an electro-magnet) and whatever atmosphere it may have. It is approxamately 83% the size of the Earths electromagnetic-field.
An outer coat size of LARGE will fit chest measurements of 42" to 44".
The outer core is approximately 2,260 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.