Discuss the paleogeography of the Early Paleozoic. How did this paleogeography differ from present-day geography? What will be an ideal response?
The Early Paleozoic continents were different from the present-day continents. Many of the
tectonic features that we recognize today were the result of later tectonic events. The
continents in the Early Paleozoic were in different latitudes than present-day continents
resulting in different climate conditions. Early Paleozoic paleography consisted of six major
continents dispersed around the world at low latitudes. Water circulated freely among the
ocean basics, and the polar regions were mostly ice-free. Epeiric seas covered many of the
continents.
You might also like to view...
List three variations in buffering.
What will be an ideal response?
Numerical weather prediction models begin with an __________ and produce a __________
a. prog; analysis b. prog; meteogram c. meteogram; prog d. analysis; prog
Which statement is true about the lithosphere?
A) The lithosphere is thickest at the mid-ocean ridges because of the quantity of magma that flows up to the surface. B) The lithosphere gets thicker as distance from the ridge increases, because it cools and the boundary between the lithosphere and asthenosphere occurs at greater depth. C) The lithosphere maintains its thickness as distance from the ridge increases, because the boundary between the lithosphere and asthenosphere remains at a constant temperature and depth. D) The lithosphere gets thinner as distance from the ridge increases, because decompression melting occurs with decreased pressure.
Thunderheads are cumulonimbus clouds
Indicate whether the statement is true or false