This question can be answered as it concerns the Canadian Rocky Mountains, which are made of layered rock. Perhaps the answer can be applied to mountains made of layered rock in other parts of the world. As explained on page 157 of Ben Gadd's book Handbook of the Canadian Rockies (Corax Press, 1995), and explained in more detail on pages 449 and 450 of his Canadian Rockies Geology Road Tours (Corax Press, 2008), in all the higher peaks of the Canadian Rockies the layers lie nearly flat, not angling downward more than 10 or 20 degrees. The key principle here is that, within the Canadian Rockies at least, flat-lying layered rock erodes more slowly than rock in which the layers angle downward (the proper geological term for down-angling is "dip"). In the Canadian Rockies the rock has been extensively bent (folded) in some places and less so in others. So after millions of years of erosion here, areas of flat-lying rock now stand higher than areas of moderately dipping or steeply dipping rock. A mountain-size area with gentle dip becomes a higher mountain than a similar-sized area with steeper dip. A larger area of gentle dip (in the Canadian Rockies we have an area of 3000 square kilometres like that) becomes a whole group of higher mountains surrounded by lower ones in the adjacent areas of steeper dip. Why does flat-lying rock in the Canadian Rockies erode more slowly than moderately dipping or steeply dipping rock? The answer seems to involve rockslides. Moderately to steeply dipping rock layers slide downward when erosion by a river or a glacier cuts away at the lower edges of the layers. Pulled by gravity, slabs come loose and slide down to the valley floor, breaking up into rubble as they go. A little erosive work at the lower edges of the slabs can bring down a lot of rock -- right to ridgelines. In contrast, the same river or glacier cutting away against flat-lying layers does not produce such rockslides. The rock is not angled steeply enough to slide in the same way. Slides can occur, all right, but they are not as common as the ones caused by the undercutting of dipping layers, and they are seldom as large.
Some places are hotter than others due to factors such as proximity to the equator, elevation, ocean currents, and prevailing winds. These factors can influence the amount of sunlight received, the distribution of heat, and the overall climate of a region.
The main reason some places on Earth are warmer than others is due to variations in the amount of sunlight they receive. Factors such as latitude, altitude, proximity to bodies of water, and ocean currents also play a role in determining the temperature of a particular location.
Some good places for people who enjoy long periods of cold weather include places like Canada, Scandinavia, Alaska, and parts of Russia. These regions experience cold winters with snowy conditions that may appeal to individuals who prefer colder temperatures. Additionally, mountainous regions like the Alps or the Rocky Mountains can also offer extended winter seasons.
The terrain of the rainforest is typically characterized by dense vegetation, tall trees, and a diverse array of plant and animal species. It can be hilly or mountainous in some regions and flat in others, with a humid and wet climate that supports lush growth. The soil in rainforests is often nutrient-rich due to the rapid decomposition of organic matter.
Norway is the most mountainous Scandinavian country, with its rugged terrain and numerous peaks contributing to its reputation as having some of the most dramatic landscapes in the region.
Both. Not kidding -flat in the southwest and and very mountainous some places.
In many places it is.
Some places have more constant winds than others.
Some places have a more Germanic heritage than others.
Some of the mountainous regions there did contain lions, where they hunted near the rare watering places.
Some places do not, some places do, and others give you an option of whether you want it to or not.
In some places, but not in others.
some of the land is mountainous, but most is desert
Places can be wetter than others due to factors such as proximity to large bodies of water, prevailing wind patterns, topography, and climate. Areas near oceans or seas tend to be wetter because of increased moisture in the air, while mountainous regions can experience higher precipitation due to orographic lifting of air masses. Wind patterns can also bring moisture-laden air to some places, leading to increased rainfall.
it will be snowing in some places, but not snowing in others because that's how the world is we all have different weather its weird but yeah yanno
Africa is geographically diverse, with a range of landscapes that include both mountains and flat regions. Some areas, like the Atlas Mountains in North Africa and the East African Rift Valley, are mountainous, while others, such as parts of the Sahara Desert and savannahs in East Africa, are relatively flat.
In some places it is essential. Others it is detrimental.