Answer:
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Sea Stack -</h2>
Thousands or even millions of years, in fact. Coastal erosion or the slow wearing of rock by water and wind over very long periods of time causes a stack to form. All sea stacks start out as part of nearby rock formations. Millennia of wind and waves hit the rock and break it down.
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Sea Cave - (one photo included for this only)</h2>
Sea caves or littoral caves are formed primarily from erosion caused by waves. They can be formed along the ocean coast and lakeshores where water impacts bedrock. Most sea caves are formed along weaknesses in the rock, such as faults, fractures, or bedding/foliation planes and can occur in nearly every type of rock.
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Sea Sand Dune -</h2>
Coastal dunes form when wet sand is deposited along the coast and dries out and is blown along the beach. Dunes form where the beach is wide enough to allow for the accumulation of wind-blown sand, and where prevailing onshore winds tend to blow sand inland.
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In order to answer this problem, we need to find a combination of length and width that would have an area of 65 feet^2 and 36 feet. So far, we know that 65=l*w and 36=2l+2w. The answer is the length is 5 and the width is 13. We can check our work.
5*13=65
2(5)+2(13)=10+26=36
In geography, the temperature in a given location is affected by different factors, mainly latitude, altitude, pressure, the weather, and ocean currents.
- Pressure – d. Affects temperature, moisture, and storm tracks. Pressure and temperature are directly linked: when one increases, so does the other, and vice versa. If cold air (which is dense and dry) encounters warm air, the warmer air will rise to the top because density makes cold air heavier. The air pressure at the surface will fall. This newly-formed low pressure system creates winds and storms.
- Geographic position – b. Local topography helps predict temperature and precipitation. It depends whether you are on a mountain, in the North pole, in the ocean, etc.
- Oceans – d. Sea surface temperature influences air temperature and evaporation rates. Sea surface temperature is where the water's temperature meets the air's temperature. As a result of a high difference between the two (as explained in 1.), storms or variations in the atmosphere can happen. Besides, warm water makes surface air warmer, which increases the temperature in nearby land areas, and vice versa.
- Mountains – c. Thinner air less able to hold heat makes climate colder. At high altitude, the air is less dense, which means it can't absorb and retain heat very well.
- Latitude – a. Affects temperature by influencing the seasonal range of solar intensity. This geographic coordinate helps determine how far north or south a particular point is on the surface of the earth, with the equator and the poles as reference points. All latitude lines are therefore parallel to the equator, which has more solar intensity. The higher the latitude (i.e., the closer you get to the poles) the lower the temperature, and vice versa.
There is a significant rain shadow effect east of the Rockies. One prime example is Denver. Over the course of a year it would typically receive ~20 inches of rain, but many locations to the west of the continental divide receive as much as 40 inches of rain a year. (It's important to note that the rain shadow effect only impacts storms and winds traveling against the mountains. If a storm travels south to north, the effect is severely diminished and can result in a situation where the lee side of the mountains receives more rainfall than the wind side of the mountains.
