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|    Message 6,842 of 8,931    |
|    Dan Richter to All    |
|    ES Picture of the Day 04 2022    |
|    04 Oct 22 12:01:12    |
      MSGID: 1:317/3 633c74e9       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.                      Quechee Gorge in East Central Vermont               October 04, 2022               PattiW_IMG_0088 (003)a               PattiW_IMG_0084 (003)a               Photographer: Patti Weeks               Summary Author: Patti Weeks               The Quechee Gorge is a 165-feet deep (50 m), 1-mile long (1.6 km)        narrow chasm on the Ottauquechee River. As Vermont’s deepest gorge,        it is nicknamed by locals as “ Vermont’s Grand Canyon.” It was        formed following the retreat of the massive Pleistocene        Laurentide Ice Sheet, which covered all of present-day Canada and        much of the northern United States, between 95,000 to 20,000 years ago.               When the ice sheet began its retreat about 18,000 years ago, the        Ottauquechee River re-emerged and began to flow east again, but was        redirected from the Connecticut River to the newly-formed narrow        Glacial Lake Hitchcock, which ran nearly 200 miles (320 km) from        what is now northern Vermont to central Connecticut. A glacial        terminal moraine (near present day Hartford, Connecticut) called        the Rocky Hill Dam, blocked the flow of the Connecticut River for        approximately 4,000 years, during which the Ottauquechee River filled        the lake with 170 feet (52 m) of sand, mud and silt. When the dam        eventually broke, the river made a sharp turn to the south, rapidly        cutting through the soft mud. Geologist Frederick Larsen estimated        that this initial erosion occurred in less than a week. The river has        been slowly carving through the hard Devonian age schist and        quartzite bedrock, the Gile Mountain Formation, ever since —        for the past 13,000 years.               Now, the Quechee Gorge is a tourist attraction. The Ottauquechee River        is also rated as a Class III+(V) whitewater river for 3.7 miles        (6.0 km). According to a report by American Whitewater, the water        level was low (<30 cfs) most of this past summer. Bottom photo shows        whitewater details. Even at its best whitewater level, however, there        is a challenging rapid area called “Well Enough.” After a thorough        scouting, you might need to leave “well enough” alone and just portage.        The second photo, focusing nearly straight down into the gorge from the        bridge, shows some large rocks that could make rafting navigation        challenging, whether the water covers them or not. Photos taken on July        19, 2022.                      Quechee Gorge, Vermont Coordinates: 43.6374, -72.4085                     Related EPODs               Quechee Gorge in East Central Vermont Limestone Stratification        near Modica, Sicily Strawberry Moon and Etna Exhaust Kodachrome        Basin State Park, Utah Idaho’s Gravity-Defying Balanced Rock        Eastern Flank of Mt. Etna        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 31 weeks, 1 day, 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: 229/112 113 317 400 426 428 470 664 700 292/854 298/25 305/3       SEEN-BY: 317/3 320/219 396/45       PATH: 317/3 229/426           |
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