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Usage Examples
Filter by Meaning The study of diastrophism helps us understand the dynamic nature of the Earth's surface.
Diastrophism can cause both gradual and sudden changes in the Earth's surface.
The geologist explained the process of diastrophism.
The diastrophism that occurred in the past created the valleys and plateaus.
Diastrophism has a significant impact on the natural environment.
Diastrophism can result in the formation of valleys and canyons.
The diastrophism of the tectonic plates is responsible for earthquakes.
The impact of diastrophism on the climate change cannot be ignored.
The formation of the Grand Canyon is due to diastrophism.
The island of Iceland is a result of diastrophism and volcanic activity.
The earthquake was caused by diastrophism in the Earth's crust.
Diastrophism can also refer to the slow sinking or rising of land over time.
Understanding diastrophism is crucial for predicting earthquakes and other natural disasters.
The gradual movement of tectonic plates due to diastrophism can cause changes in the landscape over millions of years.
Diastrophism can change the shape of coastlines.
Geologists use the principles of diastrophism to map the earth's surface.
The theory of plate tectonics explains the process of diastrophism.
The geologist studied the diastrophism of the region.
The shifting of tectonic plates due to diastrophism can create new land masses.
The diastrophism caused the formation of the Himalayas.
Diastrophism causes the formation of mountains.
The uplift of the Himalayas is an example of diastrophism.
The study of diastrophism has helped us discover important resources such as oil and minerals.
The evidence of diastrophism can be seen in the rock formations.
The effects of diastrophism can be seen in the formation of mountains and the shifting of tectonic plates.
The San Andreas fault in California is a well-known example of diastrophism.
The geological process of diastrophism is a significant contributor to the formation of the earth's crust.
Diastrophism is responsible for the creation of mountain ranges.
Diastrophism can cause the formation of mountains.
The mining company used diastrophism expertise to determine the best location for a new underground mine.
Diastrophism can cause the formation of rift valleys, such as the Great Rift Valley in Africa.
The effects of diastrophism can be seen in the exposed rock layers of the cliff face.
The seismologists employed diastrophism concepts to study the impact of earthquakes on infrastructure.
The San Andreas Fault is a classic example of diastrophism.
The effects of diastrophism can be seen in the rock layers of the Grand Canyon.
Diastrophism has resulted in the creation of many mountain ranges.
Diastrophism is one of the factors that geologists consider when evaluating the potential for oil and gas deposits in sedimentary rocks.
The geologist explained how diastrophism can cause changes to the earth's surface.
The theory of plate tectonics explains the occurrence of diastrophism in the earth's crust.
Diastrophism has played a key role in the evolution of life on earth, as changes in the earth's surface can have a significant impact on the environment.
The San Andreas Fault in California is a major site of diastrophism.
The effects of diastrophism can be observed in the formation of various geological features like plateaus and ridges.
The geologist could identify the different types of diastrophism in the rock formations.
The environmental engineers consulted diastrophism knowledge to evaluate the environmental impact of a proposed construction project.
The geologist was studying the effects of diastrophism on the landscape.
Diastrophism can cause the formation of fault lines.
The impact of diastrophism on the earth's crust is a fascinating subject for scientists.
Diastrophism plays a crucial role in shaping the Earth's surface.
The geologist studied the diastrophism in the area to determine the potential for oil reserves.
The study of diastrophism is important for predicting natural disasters such as earthquakes and tsunamis.
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