Faults.
cracks in the ground caused by earthquakesFaults. Cracks in the earths crust usually caused by earthquakes are called faults.No, their not! Faults are to do with tectonic plates, earthquake cracks are called earthquake cracks.
Cracks in the Earth's crust are called faults. These fractures occur when the Earth's lithosphere is subjected to stress, causing rocks to break and slide along the fault line. Faults can vary in size and orientation, and the movement along them can lead to earthquakes.
places where groundwater bubbles or flows out of cracks in the rock is called springs.
Cracks in the moon's bedrock are called "faults" or "fractures." These features are caused by stress and movement within the lunar surface, much like on Earth.
The type of weathering that occurs when water expands inside the cracks of rocks when it freezes is called frost wedging. As water freezes, it expands, putting pressure on the surrounding rock and causing it to fragment and break apart over time. This process is a common form of mechanical weathering in cold environments.
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Earthquakes
These are called veins
cracks in the ground caused by earthquakesFaults. Cracks in the earths crust usually caused by earthquakes are called faults.No, their not! Faults are to do with tectonic plates, earthquake cracks are called earthquake cracks.
Trenches if they are in zones of subduction. Falt lines are in areas of shifting plates (rubbing against or parallel)
Cracks in the Earth's crust are called faults. These fractures occur when the Earth's lithosphere is subjected to stress, causing rocks to break and slide along the fault line. Faults can vary in size and orientation, and the movement along them can lead to earthquakes.
Cracks in the ice sheet, which covers 98% of the continent, are called crevasses.
Cracks in the Earth's crust are faults.
They are called Crevices.
places where groundwater bubbles or flows out of cracks in the rock is called springs.
When rainwater seeps through cracks in rocks, it is called infiltration.
The force of expanding water in the cracks and pores of rock is an example of physical weathering. As water freezes and expands in these spaces, it exerts pressure on the surrounding rock, causing it to weaken and fracture over time.