<u>A) Possible trigger for this tsunami:</u>
The reason which might be possible for the tsunami is massive sea waves of water which are resulted from the under sea earthquakes which struck in the gulf of Alaska triggered tsunami.
<u>B) Officials those who doesn’t prepare the public for the possible disaster:</u>
The officials should make the people aware about the disaster and should evacuate the people from that area to avoid any loss of damage to life and property.
<u>C) Is preparations are adequate to prevent a catastrophe for the Pacific Northwest:</u>
No, the state has not done enough to prevent the damage and people are till now building in this potential danger zones.
Answer:
Subsidence is so slow that there seems to have been no depression of the upper surface of the lithosphere, so depositional environments are mostly the
same as those in surrounding areas; the succession is just thicker. These
successions are also more complete, however—there are fewer and smaller
diastems—so at times the basin must have remained under water while surrounding areas were emergent. (A diastem is a brief interruption in
sedimentation, with little or no erosion before sedimentation resumes.)
Size, shape: rounded, equidimensional, hundreds of kilometers across
Sediment fill: shallow-water cratonal sediments (carbonates, shales, sandstones),
thicker and more complete than in adjacent areas of the craton but still
relatively thin, hundreds of meters.
Hopefully that helps!
I might be wrong but I think the answer is
Continental deflection
Answer:
Desert
Explanation:
Deserts typically receive very little precipitation.
