Currently most geologists favor the theory that earth formed via accretion from a protoplanetary cloud about 4.57 billion years ago.
The material that formed the terrestrial planets like Earth contained a concentration of short-lived radionuclides that was high enough that the radiation emitted by their decay heated the bodies up to their melting temperature. An additional source of energy for Earth is believed to be the so-called "giant impact", the collision of the proto-Earth with a roughly Mars-sized protoplanet in the early history of our planet. It is thought to have resulted in the complete melting of the upper 100s of km of the Earth.
In the its molten stage the Earth completed its differentiation (separation of elements that chemically are unsoluable within each other in large quantities) into a metal core and a silicate mantle.
As the Earth is loosing heat into space the inner part of the metal core started to crystallize and now forms the (I) solid inner core.
(II) The outer metal core is still liquid and is believed to play a key role in generating the Earth's magnetic field.
(III) The mantle is the shell around the core which is currently not very well understood in terms of its exact composition and rheological (the way that the material reacts on stresses leading to deformation) behaviour. Most geologists agree that the whole mantle or at least a portion of it convects and by this process the mantle in mixed and portions of the mantle ascend to rather shallow (i.e. close to the surface) levels and undergo partial melting. Formally the mantle can be subdivided into several zones depending on the stability of certain mineral phases and one often finds the subdivision into upper and lower mantle at a depth of about 660 km.
(IV) The melt extracted from the mantle forms most of the oceanic crust that we see today and is the first step to the creation of continental crust as well. The formation of continental crust is far more controversial than that of oceanic crust but involves melt extraction from the mantle and several remelting events of the basalts that crystallized from these melts. The continental crust as we know it today is buoyant, i.e. it "floats" on the mantle because of its lower density and builds stable land masses whereas the oceanic crust is continuously recycled and sinks into the mantle in subduction zones.
Scientists believe that Earth has four layers (crust, mantle, outer core, inner core) based on seismic waves produced by earthquakes and volcanic activity. These waves travel through the Earth at different speeds and behave differently depending on the properties of the material they travel through, allowing scientists to infer the presence of distinct layers with varying densities and compositions. This model helps explain Earth's structure and how it influences geological processes.
when this earth cooled from being hot, all the Iron and Nickle get concentrated inside earth forming inner two layers Inner solid core and outer liquid core. Then with the passage of time earth solidifies gradually and mantle solidifies and now at this stage our crust the outer most part of earth look like its final product.
Scientists send seismic waves through the earth. These travel at different speed according to the density of the material that they travel through. When they bounce back, scientists use these data to guess what the earth is made up of.
Earth scientists use two different ways of classifying the Earth's layers because they have distinct properties and characteristics. The chemical composition provides information about the materials that make up the layers, while the mechanical properties inform us about how the layers behave under stress and pressure. Both classifications are important for understanding the Earth's structure and dynamics.
Scientists use seismic waves to study Earth's layers by analyzing how they travel through the different materials that make up the Earth. The speed and direction of seismic waves change as they encounter different densities and compositions in the layers of the Earth, providing valuable information about the structure of the planet's interior. By measuring the arrival times and characteristics of seismic waves at different locations, scientists can infer details about the depth, density, and composition of Earth's layers.
Crust
Shooting seismic waves into the planet
Scientists believe that Earth has four layers (crust, mantle, outer core, inner core) based on seismic waves produced by earthquakes and volcanic activity. These waves travel through the Earth at different speeds and behave differently depending on the properties of the material they travel through, allowing scientists to infer the presence of distinct layers with varying densities and compositions. This model helps explain Earth's structure and how it influences geological processes.
Scientists believe that the layers of the Earth were formed through a process called differentiation, where heavier materials sank towards the center, forming the core, while lighter materials rose to the surface, forming the crust. This process occurred early in Earth's history when the planet was still molten, allowing for the separation of materials based on their density.
Your mom made the earths layers
Type your answer here... D.Comparing the composition of the crust to other bodies in the solar system
they made one layer.. waited for that to dry, then kept making layers till it became this :) hope i helped you out haahaha
The oldest organisms can generally be found in the lower layers of rock, as these layers were formed earlier than the upper layers. By examining the relative positions of different rock layers, scientists can determine the ages of the organisms found within them.
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when this earth cooled from being hot, all the Iron and Nickle get concentrated inside earth forming inner two layers Inner solid core and outer liquid core. Then with the passage of time earth solidifies gradually and mantle solidifies and now at this stage our crust the outer most part of earth look like its final product.
Scientists send seismic waves through the earth. These travel at different speed according to the density of the material that they travel through. When they bounce back, scientists use these data to guess what the earth is made up of.
which layers of the earth have scientists been able to explore