Slip-off slopes are formed through the process of erosion, typically by the continuous downhill movement of soil and rock material due to gravity. As water flows downhill, it carries sediment with it, gradually eroding the slope and creating a gentle, concave shape. The material at the top of the slope is more prone to erosion, leading to a buildup of sediment at the base, which contributes to the formation of the slip-off slope. Over time, this process can result in the development of a distinct feature known as a slip-off slope.
Some where in there, keep looking and you will find it.
negative reciprocal slopes ---> the lines are perpendicular equal slopes ---> the lines are parallel
If the lines are perpendicular, their slopes are negative reciprocals.If the lines are perpendicular, their slopes are negative reciprocals.If the lines are perpendicular, their slopes are negative reciprocals.If the lines are perpendicular, their slopes are negative reciprocals.
slip one purl wise .. in another words put your needle in the stitch as if your are going to purl and then just slip it off without actually purling
In that case, the product of the slopes is equal to minus 1.
When alluvium is deposited on the inside of meanders. It is deposited because velocity is slower there
thalweg >>> depositon >> inner bend
Deposition, slip off slopes for river beaches and finely ground stones being deposed by the sea :)
asked more chidi abra
If the gable is formed by the two slopes and a horizontal line, it is called a gable roof.
a warm dry wind coming off the lee slopes of a mountain range,ecspecially off the northern slopes of the alps.
by strike-slip fault
shield volcano
Talus slopes are broken rocks formed by gravity and the convergent boundary. Ex: Devils Lake Gorge.
it is a shield volcano
Shear Stress
"fohn " is not a word. You may mean "foehn" - a warm dry wind coming off the lee slopes of a mountain range, especially off the northern slopes of the Alps.