Interpersonal relationships can develop a unique language, thus creating a ‘culture’ of two

The best answer to this question: Interpersonal relationships can develop a unique language, thus creating a "culture" of two, would be: true.

Explanation:

Although the term "culture" relates to many more factors than just language, the fact that two people develop such a unique language, so unique that it only involves the two of them, means that they share a series of conditions that allow them to do so. In this respect, that language makes them both unique and differentiates them from other people, or groups. It shows that these individuals that share an interpersonal relationship also share common customs, traditions, beliefs, and thus from that they can also generate a common language with which only the two of them will understand each other. That´s why the answer is true.

the most likely outcome of fewer loon territories is that hawks would increase in proportion because the benefit of victory would be greater. hawks and loons are natural rivals of resources and victories in the game, since the lakes drying up affected the loons, the hawks would be benefited from the drought.

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)