Answer:
northwest
Explanation:
Both the Tug Hill Plateau and the Catskills are located in the northeastern part of the United States. Relative to each other though, the Tug Hill Plateau is located northwest of the Catskills, while the Catskills are located on the southeast of the Tug Hill Plateau.
The Tug Hill Plateau is a highland region. Despite the name it is not a plateau, but instead it is a cuesta. It is composed of sedimentary rocks. The regions has very beautiful surroundings and beautiful nature. It is one of the places in the United States with the most snowfall in winter.
The Catskills are mountains that are part of the Appalachian Mountain Range. They are not very high, instead they can be considered as small elevation mountains. The Catskills have very dense forests, and they have lot of rivers and streams cutting through them.
Both of these places are very attractive destination for the weekend or for vacations of the people of the surrounding area.
Temperatures at high latitudes are usually lower than temperatures near the equator because <span>the solar energy must be spread over a larger area.
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<span>In the tropics, places near the equator, temperature is high because there is a net energy surplus. Net energy surplus occurs because the amount of sunlight absorbed is larger than the amount of heat radiated.
In the polar regions, places near the pole or high latitudes, temperature is low because there is an annual energy deficit. The annual energy deficit occurs because the amount of heat radiated to space is larger than the amount of absorbed sunlight.</span>
Answer:
Time-space compression refers to the set of processes that cause the relative distances between places (i.e., as measured in terms of travel time or cost) to contract, effectively making such places grow “closer.” The idea of a “shrinking world” is not new and, in the face of rapid advances in travel, such as the jet ...
Answer:
The determination of the numerical age of an object.
Explanation:
Absolute dating determines the numerical age of an object.
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