The Magnuson-Stevens fishery conservation and management act rose which of the following

The correct answer to this open question is the following.

Although the question does not provide the needed options, we can comment on the following.

The Magnuson-Stevens Fishery Conservation and Management Act was an important piece of legislation passed in April 1976. It was created to order the proper exploitation of fisheries in the United States waters. It was important for the federal government to conserve and manage all these issues under one regulation so people and companies took care of the environment. Senators Ted Stevens and Warren G. Magnuson were the ones who sponsored the act.

well its is frequent rain

have a good day

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)