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|    EARTH    |    Uhh, that 3rd rock from the sun?    |    8,931 messages    |
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|    Message 7,083 of 8,931    |
|    Dan Richter to All    |
|    ES Picture of the Day 24 2022    |
|    24 Nov 22 11:01:06    |
      MSGID: 1:317/3 637fb163       PID: hpt/lnx 1.9.0-cur 2019-01-08       TID: hpt/lnx 1.9.0-cur 2019-01-08        EPOD - a service of USRA              The Earth Science Picture of the Day (EPOD) highlights the diverse processes       and phenomena which shape our planet and our lives. EPOD will collect and       archive photos, imagery, graphics, and artwork with short explanatory       captions and links exemplifying features within the Earth system. The       community is invited to contribute digital imagery, short captions and       relevant links.                      Below the Wasatch Range’s Storm Mountain               November 24, 2022                      RayB_bigcott832c_19oct22 (002)               RayB_bigcott837c_19oct22 (003)               Photographer: Ray Boren               Summary Author: Ray Boren               Geologic forces spanning millions of years — from estuarine        deposits and metamorphic pressures to mountain building and        never-ending erosion — are exposed in beautiful Big Cottonwood        Canyon, a cleft in the Wasatch Range southeast of Salt Lake City,        Utah. Accessible examples of these phenomena are found alongside a        graceful curve in the canyon highway below ominously named Storm        Mountain. Here, tinted in shades of oxidized red and darker black, are        layered Big Cottonwood Formation rocks, as illustrated in the first        photo, taken on October 19, 2022.               The eye-catching outcrops at Storm Mountain include quartzite,        a dense, quartz-rich sandstone, and argillite, a clay-rich        mudstone. The layers were originally laid down over 720 million years        ago, during the Neoproterozoic. They were subsequently uplifted,        folded and steeply tilted beginning about 75 million years ago,        creating this rugged landscape. The quartzites were originally        deposited in rivers and tidal channels, while the argillite comes from        calmer deposits — both evidence of an ancient, seaside estuary that        preceded the mountains themselves.               A second photograph, taken the same day from below an overhang in the        rocks and above the curving highway, partly shows Storm Mountain’s        steep, craggy face, to the left. The peak rises some 2,100 feet (700        meters) above the canyon, topping out at 9,528 feet (2,904 meters)        above sea level. The perspective also hints at the season under        way: The leaves of stream-side mountain maples, cottonwoods, oaks and        other deciduous trees and bushes have turned autumnal shades of red and        yellow, for their production of chlorophyll has ceased with the        arrival of fall’s cooler temperatures and shorter days.                      Big Cottonwood Canyon, Utah Coordinates: 40.6373 -111.6330                     Related EPODs               Below the Wasatch Range’s Storm Mountain Beautiful Alpine Lakes        in the Sierra Nevada Range Quechee Gorge in East Central Vermont        Limestone Stratification near Modica, Sicily Strawberry Moon        and Etna Exhaust Kodachrome Basin State Park, Utah        More...              Geography Links               * Atlapedia Online        * CountryReports        * GPS Visualizer        * Holt Rinehart Winston World Atlas        * Mapping Our World        * Perry-Castañeda Library Map Collection        * Types of Land        * World Mapper              -        Earth Science Picture of the Day is a service of the Universities        Space Research Association.              https://epod.usra.edu               --- up 38 weeks, 3 days, 21 minutes        * Origin: -=> Castle Rock BBS <=- Now Husky HPT Powered! (1:317/3)       SEEN-BY: 15/0 106/201 114/705 123/120 153/7715 226/30 229/110 111       SEEN-BY: 229/112 113 114 317 400 426 428 470 664 700 292/854 298/25       SEEN-BY: 305/3 317/3 320/219 396/45       PATH: 317/3 229/426           |
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