Answer:
True
Explanation:
I think this is true, hope this helped
This example illustrates the principle of <u>"sensory adaptation".</u>
Sensory adaptation is characterized as the decreased sensitivity to a stimulus as a result of consistent presentation to that upgrade. Brain cells start to flame when they get on another upgrade in your condition as motioned by your tactile organs (your ears, eyes, nose, etc.).The consistent loud sound of a running forced air system, for example, appears to be disturbing when it is first turned on. Be that as it may, inside 60 minutes, you'll in all likelihood have overlooked that sound and never again see it. Along these lines, if that stimulus stays unaltered in the earth, at that point the mind cells start to flame altogether less in light of that stimulus, and the outcome is an absence of regard for that specific stimulus.
Absent-Mindness: we may not remember information we are given when our minds are occupied elsewhere. For example you may have trouble remembering the lecture material in history class if you are staring out the window.
Transience: this means that our memories often fade over time. For example you are more likely to remember an episode of your favorite television program right after you see it but as time passes you’re most likely to forget the details of that program.
Misattribution: this happens when we miss remember the source of information. For example, you may remember a story but not remember who told you the story.
The water cycle has no starting point. But, we'll begin in the oceans, since that is where most of Earth's water exists. The sun, which drives the water cycle, heats water in the oceans. Some of it evaporates<span> as vapor into the air. Ice and snow can </span>sublimate<span> directly into water vapor. Rising air currents take the vapor up into the </span>atmosphere<span>, along with water from </span>evapo-transpiration<span>, which is water transpired from plants and evaporated from the soil. The vapor rises into the air where cooler temperatures cause it to </span>condense<span> into clouds. Air currents move clouds around the globe, cloud particles collide, grow, and fall out of the sky as </span>precipitation<span>. Some precipitation falls as snow and can accumulate as </span>ice caps and glaciers<span>, which can store frozen water for thousands of years. Snow packs in warmer climates often thaw and melt when spring arrives, and the melted water flows overland as </span>snow melt<span>. Most precipitation falls back into the oceans or onto land, where, due to gravity, the precipitation flows over the ground as </span>surface runoff<span>. A portion of runoff enters rivers in valleys in the landscape, with </span>stream flow<span> moving water towards the oceans. Runoff, and groundwater seepage, accumulate and are </span>stored as freshwater<span> in lakes. Not all runoff flows into rivers, though. Much of it soaks into the ground as </span>infiltration<span>. Some water infiltrates deep into the ground and replenishes </span>aquifers<span> (saturated subsurface rock), which store huge amounts of freshwater for long periods of time. Some infiltration stays close to the land surface and can seep back into surface-water bodies (and the ocean) as </span>groundwater discharge<span>, and some ground water finds openings in the land surface and emerges as freshwater </span>springs<span>. Over time, though, all of this water keeps moving, some to reenter the ocean, where the water cycle "ends" ... oops - I mean, where it "begins." Hope this helped!!</span>
