Why did the american colonies specialize in different economic activities? a) the british empire told them to specialize. b) the people in different areas liked different things. c) the geography and resources available were different. d) religions were different and put different restricions on their members.

♡ The Question/Task(s)! ♡  

-Why did the American colonies specialize in different economic activities?

*୨୧ ┈┈┈┈┈┈┈┈┈ ୨୧*  

♡ The Answer(s)! ♡  

-The geography and resources available were different.

I apologize in advance if this answer is incorrect! ♡  

*୨୧ ┈┈┈┈┈┈┈┈┈ ୨୧*  

♡ The Explanation(s)/Step-By-Step! ♡  

-No Explanation/Step-By-Step Provided!  

*୨୧ ┈┈┈┈┈┈┈┈┈ ୨୧*  

♡ Tip(s)! ♡  

-No Tips Provided!

the correct answer is "hematoma formation, with ligaments that are stretched, partially, of fully torn" ankle sprain are produced by an injury to the tough bands of tissue (ligaments) that surround and connect the bones of the leg to the foot. this causes several damage to the ankle including hematoma formation and ligament injury .

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)