Answer:
(A) True
Explanation:
The Cascadia subduction zone is 1,100 kilometers long, and its characteristics of youthful oceanic plate and strong coupling with the overriding plate are similar to situations in southwestern Japan and southern Chile where very large earthquakes have occurred. The Cascadia subduction zone is a convergent plate boundary that stretches from Northern Vancouver Island to Cape Mendocino California, It results from the subduction of the Juan de Fuca Plate beneath the North American plate. The Cascadia subduction zone is stable with no significant seismic activity.
Answer:
Radioactive isotopes are unstable and will decay. ... The isotopes will decay into a stable isotope over time. Scientists can tell how old the rock was from looking at the radioactive isotope's half-life, which tells them how long it would take for there to be half the radioactive isotope and half the stable isotope.
Regions that are too hot or too cold, regions that are very mountaneous, deserts, etc.
Answer:
A
Explanation:
A thunderstorm only occurs in cumulonimbus cloud.
A change in the wind direction and high speed winds at high altitudes makes the air to swirl around horizontally
.
The air which rises from the ground tries to push up the air which is swirling around and tips it over.
The funnel of the air starts sucking up more warm air from the ground.
The funnel grows longer and longer and stretches to reach the ground and
when the funnel reaches the surface it becomes a tornado.