Wiki User
∙ 13y agoYou can calculate how large and how fast the asteroid was that caused the crater. You can work out when the impacts occured and get a rough idea of what space debris there has been and how it might have changed over time.
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∙ 13y agoStudying the depths and diameters of craters on the moon can provide information about the impact history of the moon, as larger and deeper craters usually result from more significant impact events. By analyzing these characteristics, scientists can infer the age of different features on the moon and better understand the frequency and size of past impact events that have shaped its surface.
Geologists use techniques such as seismic imaging to measure the speed and direction of seismic waves as they pass through different layers of the Earth. By analyzing how the waves travel through the Earth, geologists can infer the depths and properties of different layers. Other methods include studying rock samples brought to the surface by drilling or volcanic activity.
By comparing Earth's polar (12,714 km) and equatorial (12,756 km) diameters, we can infer that Earth is an oblate spheroid. The slight bulge at the equator is due to the centrifugal force caused by its rotation, resulting in a slightly flattened shape at the poles and a bulging equator.
The composition of a planet is determined by analyzing its density, mass, and atmosphere through techniques like spectroscopy and seismic studies. By studying the planet's physical attributes and chemical makeup, scientists can infer the materials it is made of, such as rock, metal, or gas.
Geologists use various pieces of evidence to infer impacts, including the presence of shock metamorphism (alteration of rocks due to high-pressure shock waves), impact breccias (rock fragments fused together by impact forces), tektites (glassy particles formed by impacts), and impact craters (circular depressions on the Earth's surface). They may also analyze geochemical anomalies and the distribution of impact-related minerals to support their conclusions.
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By studying the depth and diameters of the moon's craters, an impact specialist could determine the size of the object that hit the moon, give a good estimate of the velocity of the object, and approximate where it originated from in the sky.
The missing word is "can." The complete sentence is: "Studying you can infer how Pangaea split into continents."
How hot it is and how much it weighs.
Geologists use techniques such as seismic imaging to measure the speed and direction of seismic waves as they pass through different layers of the Earth. By analyzing how the waves travel through the Earth, geologists can infer the depths and properties of different layers. Other methods include studying rock samples brought to the surface by drilling or volcanic activity.
Studying primary source documents to infer the motives behind a historical figure's actions. Analyzing multiple accounts of an event to infer the most likely sequence of events. Examining archaeological findings to infer daily life practices of a past civilization.
By comparing Earth's polar (12,714 km) and equatorial (12,756 km) diameters, we can infer that Earth is an oblate spheroid. The slight bulge at the equator is due to the centrifugal force caused by its rotation, resulting in a slightly flattened shape at the poles and a bulging equator.
To infer about an area's past environment, you can examine geological formations, sediment layers, fossil records, and plant remains. By studying these elements, scientists can deduce information about past climates, landscapes, vegetation, and animal life of an area. These analyses help reconstruct the environmental history of a region.
Scientists use seismic waves from earthquakes to determine the depths of Earth's layers. The speed and behavior of these waves change as they pass through different materials, allowing scientists to infer the structure of Earth's interior. This technique, called seismic tomography, helps researchers map the boundaries between Earth's layers and understand their composition and properties.
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The reader can infer from the article by looking at various elements.
They can learn about conditions deep inside Earth, where these rocks formed. In addition, forces inside Earth sometimes blast rock to the surface from depths of more than 100 kilometers. These rocks provide clues about the interior.
infer means to guess