An earthquake or tremmor may happen if the slide is strong enough.
it has transform boundary
Where a tectonic plate slides past another.
earthquake
When one tectonic plate slides past another, it can create a transform boundary. At this boundary, the plates grind against each other, causing earthquakes due to built-up stress being released. This movement can also lead to the formation of features such as strike-slip faults.
Mountain building like the Himalayas. Or one plate slides under another.
The type of boundary where one tectonic plate slides under another is called a convergent boundary. This process is known as subduction, where one plate is forced beneath the other due to differences in density.
This happens at a plate boundary. The oceanic plate subducts (sinks) under the continental plate, because it is heavier. (the oceanic plate is made of basalt and the continental plate is made of granite.) This happens at a destructive plate margin. it is called this because part if the oceanic plate is destroyed, because it melts as it sinks.
When one tectonic plate slides under another, a subduction zone is formed. This process creates deep ocean trenches and can lead to the formation of volcanic arcs and earthquakes. The sinking plate eventually melts into the mantle, contributing to the recycling of Earth's crust.
Convergent boundaries occur at subduction zones, the point where one plate slides under another plate.
Convergent boundaries occur at subduction zones, the point where one plate slides under another plate.
When one tectonic plate slides past another, it can create a transform boundary. At this boundary, the plates grind against each other, causing earthquakes. The San Andreas Fault in California is a well-known example of a transform boundary.
It is where one plate slides past another plate, rubbing against it. One slides right, the other left. An example would be North America. Your Welcome.