the magma growing in size and large cracks forming
Well slope intercept form is y=mx+b and slope equation can be the same formula, except it might be interpreted in a different way. although, i may be wrong.
he he he... you dont :)
The larger the absolute value of the slope if, the more vertical, or steeper, the line is. A horizontal line has slope 0, a line that is just a very little bit steep, might have slope, 1/10, a line that is very steep might have slope 10/1 or 10, or even 1000000 and as that number gets bigger and bigger, the line becomes almost vertical. For practical purposes, the slope, or steepness, of the line can be determined by rise over run, or, with a 0/0 intercept, then y over x, or, y1-y2 over x1-x2.
m is a Latin variable and it represents slope. Therefore, y=ax will not make sense because the a might represent area.
If two lines in a plane are perpendicular, then one of the following applies:1) Either one line is horizontal (slope zero) and the other is vertical (slope undefined), 2) Or the product of their slopes is equal to -1. For example, one line might have a slope of 2, and the other, -1/2.
the philosophy of the lava supposodely forms from the specific material of the slope
Standing on the top of a concave slope means you can not see down to the bottom due to the bulge in the middle. A concave slope starts gently and gets steeper, once over the bulge, near the bottom. Standing on a concave slope means that you can see the bottom of the slope. A concave slope starts off steeply and becomes less steep near the bottom.
A shield volcano has very broad, gentle slopes.
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huge gently slopes
The slope of any flowing surface like lava, ash, pebbles is called the "angle of repose."
The slope of any flowing surface like lava, ash, pebbles is called the "angle of repose."
The slope of any flowing surface like lava, ash, pebbles is called the "angle of repose."
The slope of any flowing surface like lava, ash, pebbles is called the "angle of repose."
The major internal cause of slope failure is gravity.
If your tiltmeter tells you that the slope of the land is changing and your seismometer indicates that tremors are getting larger, you can conclude that the area is seeing some volcanic activity. A bulge may be forming that will eventually be the site of a volcano.