In this passage, what happens to Smith and his family? A. They are moved to another plantation.

B. They are broken apart when Smith is sold to another owner.

C. They are granted their freedom by a generous owner.

" At the close of that year I was sold to a Thomas Stanton, and had to be separated from my wife and one daughter, who was about one month old. He resided at Stonington-point. To this place I brought with me from my last master's, two johannes, three old Spanish dollars, and two thousand of coppers, besides five pounds of my wife's money. This money I got by cleaning gentlemen's shoes and drawing boots, by catching musk-rats and minks, raising potatoes and carrots, &c. and by fishing in the night, and at odd spells."

B.

Explanation:

I choosed B just because of the fact where it said "I was sold to a Thomas Stanton" plus it added that it separated him from his wife and daughter.

c. taught scientists many new things about the earth, but not other planets.

explanation:

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)