At times, all the world's continents have been glaciated.
A feature called 'inselberg' is often accepted as evidence of ancient glaciation unless some other explanation is more credible.
braided streams
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.
A moraine is any glacially formed accumulation of unconsolidated glacial debris (soil and rock) that occurs in currently glaciated and formerly glaciated regions on Earth (i.e. a past glacial maximum), through geomorphological processes.
Glaciated Appalachian Plateau, Unglaciated Appalachian Plateau, Lake Plains. Till Plains, Lexington Plain
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.
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.
Sandy soil is commonly found in areas with low precipitation and high temperatures, such as deserts and coastal regions. It can also be found in regions with ancient sandy deposits, like river valleys and glaciated areas.
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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.
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.