can someone pls answer this for me
The Alps in Europe is a glaciated region known for its numerous glaciers and ice fields. These glaciers have shaped the dramatic landscape and provided valuable water resources to surrounding areas.
They are found on alpine topography and glaciated uplands.
an icy puddle.
Some common plants in the mountainous region of Macedonia include oak trees, beech trees, juniper bushes, and various herbaceous plants like thyme, sage, and mountain tea. These plants are adapted to the colder climate and rocky terrain commonly found in this region.
can someone pls answer this for me
The Alps in Europe is a glaciated region known for its numerous glaciers and ice fields. These glaciers have shaped the dramatic landscape and provided valuable water resources to surrounding areas.
Features to look for in a mountainous region to determine if it had been glaciated by alpine glaciers include U-shaped valleys, sharp ridge lines, cirques, hanging valleys, moraines, and erratic boulders. These features are characteristic of glacial erosion and deposition and can help identify past glaciation.
The glaciated cloud (i.e. cloud contains ice crystals, not just super cooled liquid) appears filmy, or diffuse, with indistinct cloud edges. Non glaciated occurs more during the storm development stage where towering cumulus full of water droplets look very crisp at the edges as they mushroom out from the updraft.
west region plants
A fjord is a valley whose characteristic shape was created by a glacier, so it is a valley after it was glaciated.
No, Mt Tambora is not glaciated. Mount Tambora is not very tall and is in a very warm climate zone.
what kinds of plants are there on the pacific region
The plant genus that dominated glaciated regions during the late Paleozoic and early Mesozoic was Glossopteris. These plants were mainly gymnosperms that thrived in the ancient supercontinent of Gondwana. Their dominance in these regions is thought to be due to their adaptability to a range of environmental conditions.
More lakes
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A glaciated mountain valley typically has a U-shaped profile with steep, smooth walls and a flat bottom due to the scouring action of the glacier. In contrast, a mountain valley that was not glaciated usually has a V-shaped profile with more rugged and uneven walls, shaped primarily by flowing water and tectonic forces.