Why was the capital of Georgia moved to the city of Louisville in 1796? A
The government wanted to improve trade by encouraging its citizens to move to the Atlantic Coast.
B
The state's previous capital city was destroyed by the British during the Revolutionary War.
с
The state expanded westward and this expansion was accompanied by a large population shift.
D
The government wanted to improve relations with the Cherokee by moving the capital from their land.

C. The state expanded westward and this expansion was accompanied by a large population shift.

Explanation:

The initial reason for moving the capital was to escape British forces that almost took control over Georgia's capital in early 178-s/

The capital of the states generally a place where a lot of Major businesses was established along with job opportunities that created with it. After moving the capital city, many citizens of Georgia decided to relocate westward and caused a massive population shift among the people who seek better employment.

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)

good question. i'll be looking into that. (this is a joke sir)