it is either highland or high-lattitude
You can adjust to the climate of a mountain to live on top of it by staying warm when cold weather comes (such as building a fire).
A vertical climate a climate affected by altitude (usually found on a mountain). One example is that on a mountain the higher up you go the colder the climate (or temperature) is.
because the earth has many layers and so the closer you are up torwards the sky, the weather changes and so does the climate
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.
the climate gets colder. you will find that it could be a lovely day at hte bottom of a mountain but, if it is high enough, there could be a storm brewing at the top. It also gets very windy on a lot of mountains
at the bottom of the mountain the climate is warm allowing much vegetation to be grown. as you climb farther up the climate and temperature drops allowing not much vegetation at all to grow.
at the bottom of the mountain the climate is warm allowing much vegetation to be grown. as you climb farther up the climate and temperature drops allowing not much vegetation at all to grow.
yes. on the coast there is mediteran climate, in the mountain region there is a mountain climate and in the inland is a continental climate. there are no hurricanes, huge floods or something.
The address of the Mountain Top Historical Society Inc is: 18 Powell St, Mountain Top, PA 18707-1138
The top of the mountain is typically known as the 'peak' or 'summit'.
The climate changes dramatically as you move up a tall mountain. Climate determines the distribution of species on the mountain.
The climate on the ocean side of a mountain is typically cooler and moister due to the mountain blocking warm, dry air from reaching that side. This can result in more precipitation and lower temperatures compared to the other side of the mountain.