The concave slope form indicates that water does not

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The concave slope form indicates that water does not sink into the ground (allowing the out-and-down motion of creep), but rather it flows over the surface in small channels called rills. When rainfall (or snowmelt) encounters these slopes, it does not sink in. All of the rills (tiny gullies) provide evidence that water flows over the surface, eroding these small pathways for the water. Water flowing over the surface in these rills tends to create concave slope profiles where the rills get a bit less steep towards the bottom of the slope. This mirrors large river systems where the tendency is for the slope of the river to get less and less as it approaches the base level of an ocean or a lake.
Question 4 0.3 / 0.3 pts
You are on Thompsons Road, North Island of New Zealand, courtesy of Google Street view (Links to an external site.)Links to an external site. . This is another view (Links to an external site.)Links to an external site. of the slopes in the area. In both views, think about if the slope is flatter at the top or steeper? What is the form of that slope and what does it tell you about the dominant process ?

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