by studying seismic wave travel times, scientist have determined that the lithosphere, which includes the crust and the top of the upper mantle is made up primaraly of the ingenueos rocks granite, basalt and peridotite
Scientists study the mantle indirectly by analyzing seismic waves from earthquakes, studying volcanic eruptions, and examining rock samples brought to the surface by volcanic activity. By combining these methods, scientists can gain valuable insights into the composition, temperature, and behavior of the Earth's mantle.
Why do scientists look to the ocean floor to research the mantle? Because magma from the mantle flows out of active volcanoes on the ocean floor. These underwater volcanoes have given scientists many clues about the composition of the mantle.
The composition and structure of the Earth are determined through various methods, including seismic studies, rock samples, and geophysical surveys. Scientists use these techniques to analyze the Earth's layers, such as the crust, mantle, and core, and understand the distribution of different materials and structures within the planet.
Scientists have used seismic waves from earthquakes to study the Earth's interior. By analyzing how these waves travel through the Earth, scientists have been able to determine the density and composition of different layers like the crust, mantle, and core. Additionally, studies of meteorites and laboratory experiments have provided further insights into the Earth's composition.
Scientists study the mantle by analyzing seismic waves and volcanic activity. By measuring the speed and direction of seismic waves as they travel through the mantle, researchers can infer properties like temperature and composition. They also study the rocks and minerals brought up by volcanoes to gain insights into the composition and behavior of the mantle.
by studying seismic wave travel times, scientist have determined that the lithosphere, which includes the crust and the top of the upper mantle is made up primaraly of the ingenueos rocks granite, basalt and peridotite
mantle
hard rock
seismometers
Scientists study the mantle indirectly by analyzing seismic waves from earthquakes, studying volcanic eruptions, and examining rock samples brought to the surface by volcanic activity. By combining these methods, scientists can gain valuable insights into the composition, temperature, and behavior of the Earth's mantle.
They can do this by how and how quickly seismic waves can move through the mantle.
the mantle
Why do scientists look to the ocean floor to research the mantle? Because magma from the mantle flows out of active volcanoes on the ocean floor. These underwater volcanoes have given scientists many clues about the composition of the mantle.
Why do scientists look to the ocean floor to research the mantle? Because magma from the mantle flows out of active volcanoes on the ocean floor. These underwater volcanoes have given scientists many clues about the composition of the mantle.
The mantle is 82% of Earth's volume. It is composed of ultramafic rock called peridotite, which is hot enough to flow.
The composition and structure of the Earth are determined through various methods, including seismic studies, rock samples, and geophysical surveys. Scientists use these techniques to analyze the Earth's layers, such as the crust, mantle, and core, and understand the distribution of different materials and structures within the planet.
Scientists have used seismic waves from earthquakes to study the Earth's interior. By analyzing how these waves travel through the Earth, scientists have been able to determine the density and composition of different layers like the crust, mantle, and core. Additionally, studies of meteorites and laboratory experiments have provided further insights into the Earth's composition.