In order to find how many miles can Sara drive on 12,3 gallons, we need to find how how many gallons of gas will suffice for 1 mile.
3,2/ 70= how many gallons of gas are used per mile
Then we divide our answer with 12.3 and get how many miles sarah can drive.
The volcano is an elevated structure through which the flows out and cools down and forms a rock
the volcano is of 3 types
Active volcano
dormant volcano
Extinct volcano
when there is a large amount of gas released from the volcano it indicated that the volcano may erupt in the future as the gas may be released from any chemical reaction the stopping of the gas shows the chemical reaction which took place is over or slowed down but it denotes in the near future the volcano my erupt and can cause destruction
hence it is concluded that the dormant volcano can become active with the passage of time
learn more about volcanoes here
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Answer: Adiabatic temperature gradient is the rate of change in temperature due to pressure under adiabatic conditions.
Explanation:
The rate of change of temperature due to pressure under adiabatic conditions is referred to as adiabatic temperature gradient.
In practice, since in the sea the pressure changes can be considered proportional to depth changes, the adiabatic temperature gradient is usually given as rate of change per unit depth, instead of per unit pressure and for practical purposes and calculations, the unit of depth is often chosen as 1000 m.
The natural and non-natural heat transfer influence the process of adiabatic temperature gradient.
The mT and the cP air masses are total contrasts from one another. The mT air masses represents the maritime tropical air masses, while the cP air masses represent the continental air masses.
- The mT air masses form over the seas/oceans in the tropical regions, while the cP air masses form over the land in the polar regions.
- The mT air masses have very high humidity as they form above water, while the cP air masses have low humidity as they form over land.
- The mT air masses are warm because they form in the low latitudes, while the cP air masses are cold as they form in the higher latitudes.
- The mT air masses have low air pressure, while the cP air masses have high air pressure.
- In general, the mT air masses bring in warm and wet weather, while the cP air masses bring in cold and dry weather.
