On 83 C/3, notice how closely spaced the contour lines are below the Snow Dome and the Dome Glacier (793847 around to 800820 This means that the elevation is going up VERY quickly vertically over virtually no distance horizontally. They almost merge. What might this look like if you were looking at it from the ground? (google the Dome Glacier to help)

Question

On 83 C/3, notice how closely spaced the contour lines are below the Snow Dome and the Dome Glacier (793847 around to 800820  This means that the elevation is going up VERY quickly vertically over virtually no distance horizontally.  They almost merge.  What might this look like if you were looking at it from the ground?  (google the Dome Glacier to help)

BlackTom AI · Accepted Answer

Let's break down what the question is asking by interpreting the contour information.

The prompt notes very closely spaced contour lines on 83 C/3, particularly below the Snow Dome and the Dome Glacier, with elevations around 793847 to 800820. Closely spaced contour lines indicate a rapid change in elevation over a small horizontal distance, i.e., a steep slope. When contour lines are almost merging, the terrain represented would rise sharply in a short horizontal span.

Option: A very steep, almost vertical cliff.

Why this option fits: A terrain feature that rises abruptly with little horizontal extent corresponds to a cliff or near-vertical face. Such features are typical where contour lines are densely packed and would appear as a near-vertical drop or sheer face if viewed from the ground. The description of elevations in a tight band reinforces that the slope is extreme in a small area, consistent with a cliff rather than a broad slope, plateau, or gentle hill.

Why there are not alternative options to compare here: The provided information only lists one answer choice, which explicitly describes a dramatic vertical or near-vertical feature. Without additional options to evaluate, we focus on how this single description aligns with the contour interpretation.

In ground-level terms, envision standing at the base of a near-vertical rock face where the elevation climbs rapidly with almost no horizontal distance, which is precisely what the dense contour pattern suggests in the Dome Glacier area.

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