Crustal example sentences

Related (9): mantle, lithosphere, subduction, uplift, erosion, mineralization, geochronology, geophysics, geology.

"Crustal" Example Sentences

1. The crustal rocks on the ocean floor are much younger than those on the continental shelf.
2. The crustal heating caused by the collision of two tectonic plates can create volcanic eruptions.
3. The study of crustal deformation provides valuable insights into the geologic history of a region.
4. The thickness of the Earth's crustal layer varies from about five to 40 kilometers.
5. The movement of magma from the Earth's mantle to the crustal surface is a key part of volcanic activity.
6. The discovery of a fault line can help geologists better understand the crustal structure of an area.
7. The uplift of a mountain range can result from crustal deformation over millions of years.
8. Crustal rocks can provide important clues about the composition and history of the Earth's lithosphere.
9. The composition of crustal rocks can vary greatly depending on their age and origin.
10. The crustal plates that make up the Earth's lithosphere move very slowly over time.
11. The formation of the Himalayas is a result of the collision of two crustal plates.
12. The Earth's crustal layer is constantly being reshaped by tectonic activity and erosion.
13. Crustal movements can cause earthquakes and tsunamis that have devastating effects on human populations.
14. The analysis of crustal seismic waves can help geologists determine the structure of the Earth's lithosphere.
15. The energy released during a crustal earthquake can be measured using seismographs.
16. The crustal rocks near the sites of former volcanic eruptions can contain valuable mineral deposits.
17. The study of crustal magnetism can help geologists better understand the history of the Earth's magnetic field.
18. The pattern of crustal deformation along a fault line can be used to infer the direction and magnitude of tectonic forces.
19. The accumulation of sedimentary rocks on the crustal surface can provide a record of past environmental conditions.
20. The movement of crustal plates can cause the formation of oceanic trenches and underwater mountain ranges.
21. The slow drift of crustal plates can gradually change the position of the Earth's continents over millions of years.
22. The crustal thickness of the Moon is much less than that of the Earth due to its smaller size.
23. The crustal rocks of the Canadian Shield are among the oldest on Earth, dating back billions of years.
24. The formation of the Andes Mountains is the result of crustal interactions between the South American and Nazca plates.
25. Crustal deformation caused by a large meteor impact can create structures such as craters and impact basins.
26. The crustal temperature of the Earth increases with depth, due to the heat generated by internal processes.
27. The rift valleys that form along divergent plate boundaries can provide valuable insights into the crustal structure of a region.
28. The thickness of the Earth's crustal layer is greatest beneath mountain ranges, where it can reach up to 70 kilometers.
29. The concentration of certain minerals in crustal rocks can be a valuable indicator of the location of mineral deposits.
30. The crustal movement associated with tectonic activity can cause the sudden uplift or subsidence of large areas of land.

Common Phases

1. The crustal composition of the Earth's lithosphere varies greatly.
2. The crustal thickness beneath the oceans is thinner than that beneath the continents.
3. The measurement of crustal deformation can help predict earthquakes.
4. The crustal structure of the Moon is much simpler than that of the Earth.
5. The study of crustal evolution is important in understanding the geological history of a region.
6. The crustal rocks of the Earth's mantle have a different chemical composition than the crustal rocks of the continental crust.
7. The crustal heat flux provides important information about the thermal state of the Earth's crust.
8. The process of ophiolite formation involves the emplacement of oceanic crustal material onto the continents.

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