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But the effort pays, for with a feel for deep time comes a sense of its great power: Given enough time, almost anything energetically possible can happeneven at very large scales.
And so it goes with the bending of seemingly rigid rocks, the cutting of majestic canyons, the raising and erasing of entire mountain ranges, the opening and closing of globe-girdling oceans, and the incessant splitting and regrouping of the dancing continents.
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Geologic understanding requires careful attention to time as well as three-dimensional space, so we'd better stop here first.
The pink feldspar bands in the severely deformed metamorphic rock at right (a mylonite from the Homestake Shear Zone in the northern Sawatch Range) show the kind of internal folding you'd expect from warm taffy, but this rock didn't actually melt.
The wavy fabric indicates solid flow at mid-crustal temperatures of 400-500C.
If you're unfamiliar with geologic time terminology and abbreviations, take that detour now.
With over 50 million modern human lifetimes elapsed since the planet formed around 4.5 Ga, geologic or deep time is, to say the least, difficult to grasp.
The planet's had ample time for all of this, even if it's out of our ken.