To answer this, think about the way water moves and how ice moves. Now think of steady fast-moving streams of water and massive hulking glaciers scraping across the land. Streams push sediments along and sort them into normalized groups. Sand is separated from stones of different sizes. Glacier pick up rocks in their slow progress and deposit them later as the ice melts. The streams' depositions are very regular; the glaciers' depositions are very irregular.
Till is deposited by glacial ice. Till is deposited almost exclusively in the ablation zone either by being plastered onto the underlying glacial bed by flowing ice or by sloughing off the glacier's surface as the ice melts. Till are generally unstratified and commonly consist of large rock fragments surrounded by a finer grained matrix of sand, silt, and clay.Outwash is Sand and gravel deposited by melt water. Outwash are typicaly well sorted and stratified so they differ sharply from tills, which are unsorted and unstratified
A large boulder left behind by a glacier and deposited among other rocks is called a "glacial erratic." These massive stones are often transported over long distances by glacial ice and can differ significantly in composition from the surrounding bedrock. When glaciers melt, these erratics become stranded as the ice retreats, providing important clues about past glacial activity and the geological history of an area.
In a magnetized material, the iron atoms align their magnetic fields in the same direction, creating a net magnetic field. This allows the material to attract or repel other magnets. In an unmagnetized material, the iron atoms have random magnetic orientations, resulting in no net magnetic field.
Density is dependent on two things - the volume of the object under consideration, and it's mass. For a given material, in order for the volume (the size) to change, so must the mass by a proportional amount. Therefore, for a specific material, changing the size of the sample does not affect the density in any way.
Yes, the DNA of two individual mosquitoes will differ due to genetic variation. Genetic differences arise from mutations, recombination, and other genetic processes, resulting in unique combinations of genetic material in each individual mosquito. This genetic diversity is what allows for adaptation to different environments and contributes to the survival of the species.
desert streams get flash floods more than the streams in the humid places.
Surface waste is really supplanted by extensive underground seepage. "vanish" (vanishing streams) and "return" (springs). Streams that stream on a superficial level and afterward apparently "vanish" subterranean. They may likewise vanish into cracks or blames in the bedrock close to the stream. A gushing stream gets water from the beginning, in this manner it extends downstream by getting further and more extensive. Influent streams are in parched territories and lose a ton of water through dissipation and drainage into the ground. ... Most influent streams lose the entirety of their water, evaporating before entering the ocean.
Till is deposited by glacial ice. Till is deposited almost exclusively in the ablation zone either by being plastered onto the underlying glacial bed by flowing ice or by sloughing off the glacier's surface as the ice melts. Till are generally unstratified and commonly consist of large rock fragments surrounded by a finer grained matrix of sand, silt, and clay.Outwash is Sand and gravel deposited by melt water. Outwash are typicaly well sorted and stratified so they differ sharply from tills, which are unsorted and unstratified
A large boulder left behind by a glacier and deposited among other rocks is called a "glacial erratic." These massive stones are often transported over long distances by glacial ice and can differ significantly in composition from the surrounding bedrock. When glaciers melt, these erratics become stranded as the ice retreats, providing important clues about past glacial activity and the geological history of an area.
Glaciers erode through the process of plucking and abrasion, which involves the ice picking up and grinding rocks as they move, creating U-shaped valleys and sharp peaks. Rivers erode through processes like hydraulic action and abrasion, carving V-shaped valleys and river channels. Glaciers tend to erode more material due to their larger size and slower movement compared to rivers.
The boulder on the lake shore of Indian Ponds likely formed from glacial activity during the last Ice Age, when glaciers transported and deposited large rocks and debris across various landscapes. As the glaciers melted, they left behind these erratics, which are boulders that differ from the local bedrock. Erosion and natural weathering processes may have further exposed and shaped the boulder, allowing it to become visible on the lake shore.
the material in the astehnosphere can flow slowly and the lithosphere flows on top of the astenosphere HOPE I HELPED!!
An inclearing check is a check that has been deposited into a bank account and is in the process of being cleared by the bank. It differs from a regular check in that a regular check has not yet been deposited or processed by the bank.
jet streams travel above global winds. might not be a straight forward answer, but its something.
by magic
An element is a pured substance and a pure substance is a material
An esker is a type of hill made up of glacial debris (sort of a moraine). They are generally found in areas that have had continental glaciation (past ice ages) and differ from the moraines seen at the edges of glacier ice sheet in that they are elongated in the direction of ice sheet flow. Esker is from old Irish meaning "ridge". A esker is commonly long and sinuous. see : http://en.wikipedia.org/wiki/Esker