Deposits of the Caribou Hills glaciation only locally retain a distinct hummocky morainal form, with filled kettle depressions and subdued knobs. Along the mountain fronts the marginal deposits of this glaciation reach an average altitude of slightly more than 3,000 feet.

With all due respect to Aaron, every era seems to have had its legion of wrongdoers and shortcutters who used whatever science was available to get an edge.

When strata are so unsymmetrically and abundantly folded that it becomes difficult or impossible to trace out the individual flexures and crumplings — the whole forming an irregular complex of folds — they are said to be contorted […]

Luxury did not spoil her; and any one that saw her in the soft furs of her winter wrappings, would have said that delicate cheek and frame were never made to know the unkindliness of harsher things.