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In the most plausible Lewis structure of XeOF2, there are
Shoreline Glacier
A glacier that extends to the sea at its terminus, often calving icebergs into the water.
Glaciers
Large, slow-moving masses of ice that form from the accumulation and compaction of snow on mountains or near the poles.
Smooth Troughs
Gently sloping depressions or valleys often found on the ocean floor, formed by sedimentation or tectonic activities.
Marine Sediments
Particles of organic and inorganic matter that accumulate in a loose, unconsolidated form on the ocean floor.
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