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.
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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The slope of a volcano refers to the incline or angle of the sides of the volcanic edifice. It is typically measured as the ratio of the vertical rise in elevation to the horizontal distance covered along the volcano's flank. The slope of a volcano can vary widely depending on factors such as the type of volcanic activity, the composition of the volcanic materials, and the overall geological setting. Understanding the slope of a volcano is crucial for assessing potential hazards such as landslides, pyroclastic flows, and lava flows.
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 slope of a volcano refers to the steepness of its sides, usually measured in degrees or as a ratio of vertical elevation to horizontal distance. Steep slopes can be indicative of a more explosive eruption potential, while gentle slopes often result in less violent eruptions. The slope of a volcano can have implications for the speed and direction of lava flows during an eruption.
very or highly viscous magmas formed it
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.