The Carolinas was a large area with two different regions. In 1712 it officially split into North Carolina and South Carolina True

False

True.

Explanation:

Prior to the spilt of Carolinas into North Carolina and South Carolina, the two regions also had distinct geography and history. The southern region of Carolina experienced large influx of planters and slaves because of its profitable rice cultivation. The number of African slaves grew tremendously and also became the majority.

On the other hand, the first inhabitants of the Northern part of Carolina were mostly former slaves from Chesapeake. They were mostly small farmers and didn't practice slavery.

Thus, In 1712 the Carolinas officially split into North Carolina and South Carolina because of their contrasting nature.

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the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)