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!
Answer:
1st female national president of ffa
Answer:
I the the answer is d.) the way someone looks at something but i'm not sure.
Explanation:
France in a country Europe has a population
Answer:
Air temperature and the Velocity of Air.
Explanation:
Wind chills is the measure of the temperature when the wind is blowing.So when the wind is blowing and if it comes in contact of our skin it draws heat from our body hence we feel cold more the speed of the wind more cold we feel.
So the two main variables that are used to measure the wind chill are Air Temperature in Fahrenheit and Wind speed in miles per hour.
