energy capturing bike Do you think this system would be a good solution for the rescue team? Why or why not?

The correct answer to this open question is the following.

Although you did not include further references such as any text, case, lecture, or article, doing some research trying to help you we can comment on the following.

I think this system of energy capturing bicycle would be a good solution for the rescue team in some cases, depending on the circumstances and the kind of land to use the bicycle.

The energy capturing bicycle works the following way. It was devised by Denmark inventors, specifically the wheel. Indeed, it is called the Copenhagen wheel. When riding the bicycle, the rider generates energy by spinning the wheel, making the generator that is included in the wheel to move. This makes the batery to be charged. So if the rider -for whatever reason- needs more power, it can use the reservoir of energy in the bicycle.

using the scientific method.

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)