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Lithology also affects slope gradient, with badlands on Eocene marls showing rougher topography (30 40° average slope angle) than on Garumnian lutites (20 30°).
The travel distance of the collapsed debris in the deposit area was about 200 m, with an average slope angle of 21 degree.
(1) Slope angle Using the function of Mean in the ArcGIS Spatial Analyst model, an average slope angle was defined for each slope unit.
With a bedding structure, the slope aspect is 105°, and the average slope angle is 21°, similar to the dip of the bedrock.
It can be seen from the figure that the height of the main cliff was higher than 660 m, and the average slope angle was about 54 degree.
Using the same input contour line data from 1 10,000 maps, basic cone parameters such as cone height, basal and crater width have been measured in order to calculate parameters like Hco/Wco ratio and average slope angle.
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The ramp is inclined with an angle of 9° compatible with the observed average slope topography (note that the angles ∼15° 17° measured in the alcove would rather correspond to the scar inclination rather than to the surface of flow).
Stoss and lee face slope angles are given here referred to the horizontal (i.e., not corrected for the mean underlying bed slope angle).
The crater floor lies at 2928 m, and the rim lies 150-300 m above that, giving the walls an average slope of 34 35 degrees (close to the angle of repose).
The angle between the line describing the average slope during the diastolic phase of the cardiac cycle and the vertical, the middle cerebral artery standardized deceleration angle, was measured.
The main scarp closer to the ridge has a slope angle between 28° and 30° and average elevation of 3000 m above the basal level of VM, while the two secondary scarps amount to half that height.
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