high plains
The most well-known glacial feature on Kelleys Island would be the Glacial Grooves, located on the north side of the island. They were protected in the 1880's by deed and are generally recognized as the best examples of glacial action in the U S. There are numerous areas of glacial scratching and scouring on the island as well. If you search "Kelleys Island glacial grooves" you'll find several online pictures.
Glacial grooves in Antarctica can be found on exposed rock surfaces, typically on nunataks or other high points where glaciers have flowed over the rock and carved out grooves with their abrasive action.
Evidence of glacial erosion includes U-shaped valleys, striations or grooves on rocks caused by the movement of the glacier, glacial polish on rocks, and moraines (deposits of glacial till). These features indicate the past presence and movement of a glacier in the area.
Striations would most likely form on the surface of the bedrock under the glacial ice. Striations are caused by the movement of large rocks embedded in the base of a glacier scraping across the bedrock, resulting in long, parallel grooves being carved into the bedrock surface.
The Southern High Plains ecoregion in Texas is most likely to be affected by wind erosion due to its flat terrain, minimal vegetation cover, and high wind speeds. This region is characterized by extensive agricultural activities, which can leave large areas of soil vulnerable to erosion.
Alfred Wegener's glacial evidence primarily refers to the distribution of glacial deposits and striations found on continents that are now widely separated. He noted that regions like South America, Africa, India, and Australia displayed signs of ancient glaciation, indicating that these landmasses were once joined in a supercontinent called Pangaea during the late Paleozoic era. The alignment of glacial features, such as glacial till and grooves, further supported his theory of continental drift, suggesting that these continents moved away from the polar regions, where glaciers would have formed, to their current positions.
what weathering does is that weathering moves your soil or sediments and then when it hits a stream erosion happens and moves it down along the stream and then comes deposition and the sediment lands at a random spot.
Tire grooves channel and disperse the water on wet roads. If it weren't for grooves, your tires would be 'aquaplaning' on every patch of water, and not gripping the surface.
That is the Texas region along the Gulf Coast. It would be subject to hurricanes and flooding more so than the rest of the state. Changes from water and wind would happen very rapidly.
you would probably not have any grooves on your fingers then
Glacial periods, episode of glaciation, glacial age, etc. They all the same thing as an Ice Age. If you want something more specific, I would check websites that have information on weather and climates.
Not all tyres have grooves. Take the "slick" tyre - it does not have grooves. It is used always in racing (as it is illegal to use on most countries roads) and only in dry weather (permitting). "Normal" tyres have grooves, as a channel to expel water from the surface of the tyre. Without these "grooves", driving in the wet would be a hair-raising experience, as the tyre would aquaplane on the water giving the driver, no grip or control. This is also the reason that most countries have a limit on the tread depth, to ensure that the channels are large enough to expel any water away from the surface of the tyre.