The size of the sediment would decrease further downstream (where there is a greater volume of water) as there is more energy in the flow. Therefore more erosion will occur and the sediment will rub together with other materials i.e other rocks or the river bed (this is called attrition). The sediment will therefore reduce in size but there will be a greater amount of it. (The amount of sediment is called the discharge.)
...what readings? current? voltage? power? lux?
cari diri r. aku pun selok ugop ni
desert streams get flash floods more than the streams in the humid places.
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.
Strata can differ in terms of their composition, thickness, and arrangement. Composition refers to the types of sediments or rocks found in the strata, such as sandstone or shale. Thickness relates to the depth or vertical extent of the strata, which can vary depending on the deposition environment. Arrangement refers to the way strata are stacked or layered, which can be horizontal, tilted, or folded.
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.
A deceleration graph typically shows a decreasing function where the value of deceleration is decreasing over time. This is in contrast to an acceleration graph, where the value of acceleration is typically constant or increasing over time. The deceleration graph would show negative values as the object slows down.
Yes, streams can be man-made, often referred to as artificial or constructed streams. These are created for various purposes, including irrigation, drainage, flood control, or aesthetic enhancement in landscaping. Man-made streams can mimic natural ones, incorporating features like banks, vegetation, and flow patterns to support local ecosystems. However, their ecological impact can differ significantly from natural streams.
jet streams travel above global winds. might not be a straight forward answer, but its something.
at the time of decreasing lamp voltage as the temperature is already high the gas in the lamp is already in ionized state leading to different resistance ,but when increasing voltage the gas is not in ionized state it ready to ionize ,so there is slightly variation in resistance . :)
advanced in technology and an increasing demand for manufactured goods
Erosion moves sediment to new locations