Answer:
I would think it would be whatever part is on the outside.
Explanation:
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:
Temperatures
Explanation:
The Celsius scale is part of the metric system, otherwise known as the International System of Units (SI). Temperatures in Celsius can be expressed as a number of degrees followed by the symbols ℃, or simply C. The Celsius scale has 100 degrees between water boiling and freezing, while Fahrenheit has 180 degrees.
Heat it, oil it, then use a hammer. Bigger wrench with a coin underneath and bang the heck out of it.
Answer: Relative location will change depending on the person describing the location.
Explanation:
