No. Fossils tell us about what was living at or near the earths surface in the past, they do not tell us about the Earth's interior. When studying the Earth's interior, geologists look at micro gravity variations (which tell us about density differences in deep rocks), magnetic variations (which tell us a bit about the deep rocks composition) and most importantly seismic records (which tell us about the physical properties of the deep rocks). We also look for deep rocks that have been brought to the surface during the collision of continents (the roots of mountains) and volcanic events (such as diamond pipes).
The Earth's gravitational field helps us understand its interior structure by revealing variations in density and composition. Stronger gravitational pull indicates denser materials, while weaker pull points to less dense regions. These variations help scientists infer the distribution of materials like rocks and metals within the Earth.
The Earth's core is about 7 times the density of the surface rock. That means, a person in a deep mineshaft is getting closer to more mass. Therefore, density is relative to the depth of the earth by the correlation this has on a person's weight.
density tells us how packed the object is
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The speed of the waves that travel through the interior can tell the density of each layer of the Earth. Some waves can make it through certain layers, but not others.
No. Fossils tell us about what was living at or near the earths surface in the past, they do not tell us about the Earth's interior. When studying the Earth's interior, geologists look at micro gravity variations (which tell us about density differences in deep rocks), magnetic variations (which tell us a bit about the deep rocks composition) and most importantly seismic records (which tell us about the physical properties of the deep rocks). We also look for deep rocks that have been brought to the surface during the collision of continents (the roots of mountains) and volcanic events (such as diamond pipes).
Seismic wave studies have helped scientists determine the structure of Earth's interior by observing how these waves travel and get refracted or reflected by different layers beneath the surface. By analyzing the speed, direction, and behavior of seismic waves, scientists can infer the composition, density, and temperature of Earth's various layers, such as the crust, mantle, and core, providing valuable insights into the structure and dynamics of our planet's interior.
The Earth's gravitational field helps us understand its interior structure by revealing variations in density and composition. Stronger gravitational pull indicates denser materials, while weaker pull points to less dense regions. These variations help scientists infer the distribution of materials like rocks and metals within the Earth.
Seismic waves tell us about the Earth's interior by their behavior and speed. They reveal information such as the density, composition, and state of materials within the Earth. By analyzing the travel time and behavior of seismic waves, scientists can infer details about the structure and properties of Earth's interior layers.
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If you wish me to tell you a fact about the Earth, then i will happily oblige: The Earth is currently the only planet known to man that has an environment capable of producing life.One important fact about Earth is that the planet has the greatest density than all others.
Shadows can provide information about the depth and direction of geological features, such as mountain ranges or volcanic peaks, on the surface of the Earth. By studying the lengths and angles of shadows, geologists can infer the approximate shape and elevation of land formations, helping to better understand the Earth's interior composition and structure.
dust and ice and other partcials
The speed of the waves that travel through the interior can tell the density of each layer of the Earth. Some waves can make it through certain layers, but not others.
Astronomers use complex calculations to determine celestial bodies' distance.They've stated that the sun is 150 million kilometers far away from the Earth.
The Earth's core is about 7 times the density of the surface rock. That means, a person in a deep mineshaft is getting closer to more mass. Therefore, density is relative to the depth of the earth by the correlation this has on a person's weight.