Techtonic plate movement forms land masses by three different movements or boundaries: 1. tranform boundaries- when plates slide BY one another 2. divergent boundaries- when plates slide APART fom one another 3.convergent boundaries- when plates slide TOWARDS one another Convergent boundaries can form a continental collision, when "plates crash or crunch together" forming a mountain range (over millions of years). a convergent boundary can also make an ocean trench when one plate slides under the other.
As the Earth moves the plates back and forth, the plates collide bending upward and with enought pressure, it creates a volcano.
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Tectonic activity, that is the shifting of Tectonic plates resulting in volcanoes and earthquakes are typically adapted to by human abandonment. Through knowledge and legislation, habitation is not permitted in the danger zone of volcanoes. Earthquake locations cannot be as easily pinpointed resulting in stronger construction requirements.
no
Tectonic plate motion.
The answer is that earthquakes and volcanoes are most frequent along Tectonic plate boundaries, these are the natural pieces that the continents and oceans are on.
Earhquakes and volcanoes are typically found near the edges of tectonic plates.
the tectonic plates shake under the earth causing earthquakes
Tectonic plates
something about tectonic plates.....
No. They are caused by the shifting of tectonic plates.
yes
Tectonic activity, that is the shifting of Tectonic plates resulting in volcanoes and earthquakes are typically adapted to by human abandonment. Through knowledge and legislation, habitation is not permitted in the danger zone of volcanoes. Earthquake locations cannot be as easily pinpointed resulting in stronger construction requirements.
no
Tectonic Plates are moving in all directions...
Around the edges of tectonic plates.
Tectonic activity has a number of consequences, which include continental drift, earthquakes, and volcanoes.
Tectonic plate motion.
Scientists observed that volcanoes and earthquakes occur at the edge of tectonic plates.