The community of knoxville is seeking to increase tourism in the area. as a result, the city government decides to form a team to explore the different alternatives and provide more information on their benefits and potential downfalls. which type of team is this?

advice team

Explanation:

What is the role of an advice team ?

-Advice team is a team that will sit down with a particular company that is faced with an issue , you explain the problem to them ,they analyse it and do their own research on what you can do to resolve this problem

-They then come up with best possible solutions or steps towards those possible solutions, they will then walk with you step by step through the resolution process.

-They will communicate with other departments who could be of a great assistance in your problem and compile everything in a form of a report writing,they track each and ever step and record it .

-They keep guiding you and giving you all the necessary support with their advice on what you need to do next.

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)