Seismic waves
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).
Geologists are not primarily map makers, but they often use maps as important tools in their work. Geologists study the Earth's structure, composition, and history, which may involve creating maps to visualize and communicate their findings. Geographic information systems (GIS) are commonly used by geologists to help create detailed geological maps.
Geologists record the seisemic waves and study how they travel through Earth. different types of waves behave differently. The speed of the waves and the paths they take reveal the structure of the planet. That's all I know................................
Earth is estimated to be around 4.5 billion years old, based on radiometric dating of meteorites and rocks from Earth's surface. Geologists have used various dating methods to determine the age of Earth, including studying the decay of radioactive isotopes in rocks and minerals.
Scientists who make maps of the Earth's surface are called cartographers. They analyze geographic data and use specialized software to create accurate representations of different locations on Earth. Their maps are used for various purposes, including navigation, urban planning, and resource management.
Geologists learn about Earth's interior using indirect evidence from seismic waves, magnetic field data, and rock samples from volcanoes and deep drilling. These methods help provide insights into the composition, structure, and properties of Earth's interior layers.
Rock samples and Indirect evidence from seismic waves Direct evidence from rocks samples and indirect samples from seismic waves my science teacher told me
False. Geologists do not rely on evidence from fossils to study Earth's interior. Instead, they use seismic waves, drilling samples, and other direct methods to gather information about the Earth's interior, such as its composition and structure. Fossils are used by paleontologists to study ancient life forms and environments, not the Earth's interior.
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).
Mining provides access to samples from deep within the Earth's crust, allowing scientists to study the composition, structure, and properties of rocks and minerals that are not typically exposed at the surface. By analyzing these samples, geologists can gain insights into the Earth's interior processes, such as plate tectonics, mantle convection, and mineral formation. Additionally, mining operations generate seismic data that can be used to create 3D models of subsurface structures, helping to further our understanding of the Earth's interior.
Uniformitarian geologists will use this method to determine which layer of rock formed at which time period of earth's history, and the order of the formation.
indirect
Earthquakes occur frequently. They create different types of waves that travel through the earth at a variety of speeds. Certain waves are also reflected and refracted by some materials. As a result it is possible to tell where boundaries are between two different types of materials. By knowing the speed the various waves travel through the various materials, it is also possible to know the density of various materials. Geologists know the material ejected by volcanoes of various types. The density in the center of the earth is the same as a mixture of iron and nickel. Just above the center of the earth is heavy material, but is a guess!
Geologists are not primarily map makers, but they often use maps as important tools in their work. Geologists study the Earth's structure, composition, and history, which may involve creating maps to visualize and communicate their findings. Geographic information systems (GIS) are commonly used by geologists to help create detailed geological maps.
Seismic waves are used indirectly I have a question for you is this from a chapter 9 science packet section one because I have the same.
The deep interior of the Earth can be mapped using seismic waves. Natural earthquakes produce seismic signals which penetrate the Earth. Timing the arrival of these waves at various sites round the world, gives indication of the shape and the wave velocity in the Earths interior. Rather similar to the way a CAT scan can reveal the interior of a person.
Geologists record the seisemic waves and study how they travel through Earth. different types of waves behave differently. The speed of the waves and the paths they take reveal the structure of the planet. That's all I know................................