All things

I had this lined up as part of a draft for Rocktalk, but with only a week left at the j-o-b, I’ll use it here:

Nature will be reported. All things are engaged in writing their history. The planet, the pebble, goes attended by its shadow. The rolling rock leaves its scratches on the mountain; the river, its channel in the soil; the animal, its bones in the stratum; the fern and leaf their modest epitaph in the coal. The falling drop makes its sculpture in the sand or the stone. Not a foot steps into the snow, or along the ground, but prints in characters more or less lasting, a map of its march. Every act of the man inscribes itself in the memories of his fellows and in his own manners and face. The air is full of sounds; the sky, of tokens; the ground is all memoranda and signatures; and every object covered over with hints, which speak to the intelligent …. In nature, this self-registration is incessant, and the narrative is the print of the seal.

The complete works of Ralph Waldo Emerson: Representative Men [Vol. 4] Emerson, Ralph Waldo, 1803-1882., Emerson, Edward Waldo, 1844-1930.

field work

The impressive Blanca Massif, northeast of Alamosa, Colorado, is part of the Sangre de Cristo range and rises to Blanca Peak at 14,351 ft (4374 m). Glacial activity during the Pleistocene epoch played a significant role in shaping the landscape of the massif. Glaciers carved U-shaped valleys, cirques, and moraines, creating a distinctive topography. In stark contrast, the flat San Luis Valley itself is caused by gradual sediment in-filling of the down-dropped fault block basin. January ©2019 hopkins/neoscenes.
The impressive Blanca Massif, northeast of Alamosa, Colorado, is part of the Sangre de Cristo range and rises to Blanca Peak at 14,351 ft (4374 m). Glacial activity during the Pleistocene epoch played a significant role in shaping the landscape of the massif. Glaciers carved U-shaped valleys, cirques, and moraines, creating a distinctive topography. In stark contrast, the flat San Luis Valley itself is caused by gradual sediment in-filling of the down-dropped fault block basin. January ©2019 hopkins/neoscenes.

late snow

late snow, Boulder, Colorado, April 2013

Wake up to another snow-fall. It’s Tuesday, I’ve got class, and have to take the bus in rather than cycling. It’s too slick for experimental commuter riding today.

snow-shoeings

Can’t think of a better place to be than here at the ski house with my godson Simon, my old friend Bill, and a few other folks. Chorizo and eggs for breakfast, then everybody else heads out to ski. I stay at the house and do some snow-shoeing through the deep snow in the ‘back 40,’ and otherwise, chill out.

This is the way I enter the New Year, the warm Sith hat thanks to Zander.