At the top. "Altitude" means elevation or height above a surface, or above sea level.
Altitude is the height of a shape. The point where all altitudes of a closed shape meet is called the orthocenter. To FIND an altitude rest one flat side of the shape on the "ground" and measure straight up to the point furthest from the ground. In other words, measure at a right angle from the line segment forming one side across to a line segment or vertex on the opposite side. Example: Altitude of a square, measure any side -- the altitude of the "top" is the same height as any other side, since all sides are at right angles and the distance from the bottom to the top is the same anywhere on the square.
from left top to right bottom or right top to left bottom
The top of a mountain is called the summit.
A mesa is a flat-topped mountain.
No, a parallellogram has the same both "top" and "bottom" size. A trapezoid has diffrent both "top" and "bottom" size.
A mountain top is higher (greater) in altitude. That is the definition of altitude : height above a surface, or above sea level.
Air density is greater at the bottom of a mountain due to the higher atmospheric pressure caused by the weight of the air above. As you move higher up the mountain, the air becomes less dense because the pressure decreases with altitude.
on the bottom of the mountainbeacause you are more below air level
A mountain or a tall peak may have several different climate zones from bottom to top due to changes in altitude. As altitude increases, the temperature typically decreases, resulting in different climate zones such as tropical at the base, temperate in the middle, and alpine at the summit.
If the wet adiabatic lapse rate is 6 degrees per kilometer, the temperature decreases by 6 degrees for every kilometer gained in altitude. To find the temperature at the top of the mountain, you need to know the initial temperature at the base of the mountain and the altitude gained to the top of the mountain. Start with the base temperature and subtract 6 degrees for every kilometer of altitude gained.
The density of air is greater at ground level because of the weight of the air above pressing down. As you go higher in altitude, there is less air above exerting pressure, leading to lower air density at the top of a mountain.
Air pressure decreases as altitude increases, so at the top of a mountain, the air pressure is lower compared to the bottom of the mountain. This is because there is less air above pushing down on the air below at higher altitudes.
The atmospheric pressure will be greater at the base of the mountain because pressure decreases with increasing altitude due to the weight of the overlying air. This means that as you climb higher up a mountain, the pressure will decrease.
At the bottom. You can think of the air pressure at a given location as being the weight of all the air in a column above it. Thus, the higher you go, the less air there is above you, and thus the lower the air pressure. In the extreme, when you rise out of the athmosphere, there is no air above you at all, and the air pressure is effectively zero - a vacuum. Air pressure is greater at the bottom of a mountain.
An underwater mountain has height from the ocean bottom, the top and bottom of the mountain have depth from the surface of the water.
on the top of the mountain as pressure is greater so water will boil quicker
The air pressure is lower at the top of a mountain because there is less air above pressing down on it, resulting in lower atmospheric pressure. This is due to the decrease in the density of air molecules at higher altitudes.