the magma growing in size and large cracks forming
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∙ 14y agoWell 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.
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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Shield volcanoes have a gentle slope with a base that is typically around 5-10 degrees. This gentle slope is a result of the lava flows that build up gradually over time, creating the wide, shield-like shape characteristic of this type of volcano.
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 excessive saturation of the soil, leading to loss of strength and increased pore water pressure. This can be triggered by factors such as heavy rainfall, poor drainage, or improper construction practices that disturb the natural slope stability.
You can conclude that there is an increased risk of a landslide occurring in the area due to the changing slope of the land. The larger tremors indicated by the seismometer could be causing destabilization of the ground, further increasing the risk of a landslide. It would be advisable to take precautionary measures to ensure safety in the area.
A cinder cone or cinder volcano is a steep hill of volcanic debris that gradually builds up from a volcanic vent. It can be on the slope of a larger stratavolcano or shield volcano.