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Give relative ages of rocks. This is not the only clue to this question
Geologists study where intrusion and extrusion formed in relation to other rock layers. This helps geologists understand the relative ages of the different types of rock! Hope it helps;)😊
A fault must be younger than the rock it cuts through.
Geologists use instruments like GPS devices, tiltmeters, and creepmeters to monitor the upward movement along a fault. These tools help geologists measure ground deformation and track changes in fault activity over time.
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Geologists use a variety of techniques to study fault movements, such as mapping fault lines, analyzing the offset of rock layers, studying fault rocks, and using geophysical methods like seismic imaging. By analyzing these features and data, geologists can reconstruct the history of fault movements and better understand the behavior of faults.
Two things geologists study is the process that creates Earth's features and search for clues about Earth's history
Geologists refer to the angle that a fault makes with the horizontal as the "fault dip." This angle is measured from the horizontal plane down to the fault surface. The dip is an important aspect of fault geometry, influencing how stress is distributed in the Earth's crust and affecting earthquake mechanics.
Geologists have trouble explaining how fold and fault-block mountains came into being.
Yes, geologists use creep meters to measure the slow, continuous movement along a fault. Creep meters are sensitive instruments that can detect even small amounts of movement over time, helping geologists monitor fault activity and study the behavior of faults.
Geologists determine the age of a fault line primarily through relative dating techniques, such as examining the rock layers (stratigraphy) adjacent to the fault and identifying which layers have been displaced. They may also use radiometric dating methods on minerals or rocks within or near the fault to obtain absolute ages. Additionally, the analysis of fault-related features, such as offset river channels or specific geological formations, can provide insights into the timing of fault activity. Combining these approaches allows geologists to establish a more comprehensive timeline of fault development and movement.
geologist can predict earthquakes by the help of stress along a fault and energy along the fault