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Middle creek wyoming Stock Photos and Images
RMRNYRFG–WYOMING - Colorful hot spring right next to the trail in the Middle Group of the Heart Lake Geyser Basin in the backcountry of Yellowstone.
RMM3G4D9–High elevation pastures are used by many species of wildlife in the summer. Sylvan Pass. Yellowstone National Park, Wyoming, USA
RFJGMAF2–View from the middle of Sunlight Bridge on the Chief Joseph Scenic Byway. The highest bridge in Wyoming spans the Sunlight Creek.
RFGGH15R–Moose stands in marshy stream along Middle Creek of Shoshone National Forest in Wyoming, USA.
RMC8B9C5–If ever there were an aptly named river, Firehole River is it. Considering the amount of runoff from the various hot springs, I wonder how that affects the fish population. Apparently not in a negative way judging by the number of fly fisherman I saw at any given time. I took this the morning we were supposed to hike to Fairy Falls, due to bear activity and lack of prepardness those plans changed. :)
RMBG5X1N–Native American deer hide painting of Sand Creek Massacre Colonel John Chivington 700 men killed maimed 133 friendly Cheyennes mostly women children
RFPEA1C6–The Grand Teton Mountains, Jackson Lake, and Willow Flats by moonlight with the Milky Way Galaxy.
RF2DGEJRY–This big guy was walking down the middle of the road to Slough Creek near Lamar Valley in Yelllowstone
RM2K15R9B–A small stream of melted snow flowing over the rocks below the Grand and Middle Tetons along the Avalanche Divide Trail. Grand Teton National Park, Wy
RMJ2HRB6–Popo Agie Wilderness, Wyoming. USA. Frosted grass along Middle Popo Agie River. Meadow in Tayo Park. Wind River Range. Shoshone National Forest. (Large format sizes available)
RMRNYRG7–WYOMING - Colorful hot spring right next to the trail in the Middle Group of the Heart Lake Geyser Basin in the backcountry of Yellowstone.
RM2AWPBW6–Geology and water resources of the Bighorn Basin, Wyoming . pper about 200 feet thick, of softer, purer,and more massive rock, which weathers into the characteristic pinnacled forms.The base of the formation is not distinct, and, although between this and the suc-ceeding Bighorn formation there is a hiatus representing Silurian and Devoniantimes, no unconformity is noticeable. On the northern side of Shell Creek Canyon the following fossils were collected byMr. Darton from the middle of the Madison formation:. RTiipidomella michelini,Spirifer centronatus, Seminula Tiumilis, Eumetria verneuilia
RMM3G4CP–High elevation pastures are used by many species of wildlife in the summer. Sylvan Pass. Yellowstone National Park, Wyoming, USA
RMCEBA8A–Yellowstone National Park was established in 1872 and covers 3,468 square miles. The largest supervolcano on the continent, Yellowstone Caldera, is inside the park and considered active. In 1988, one of the many seasonal forest fires burned over one third of the park.
RM2K15RRJ–A small creek flowing past Indian paintbrush wildflowers toward the Grand Teton in the South Fork of Cascade Canyon. Grand Teton National Park, Wyomin
RMRNYRHM–WY03821-00...WYOMING - Hiker passing a colorful hot spring, part of the Middle Group of the Heart Lake Geyser Basin in the backcountry of Yellowstone
RM2AWP97K–Geology and water resources of the Bighorn Basin, Wyoming . m. ? sandstone. -^ > BASAL WASATCH CONGLOMERATE LYING U NCON FORM ABLY ON LARAMIE SANDSTONE.At head of Dry Cottonwood Creek. 8TEATIGRAPHY TERTIARY ROCKS. 83 : Fossils from Middle ForTc of Owl Creek, Wyoming. Equiseuum sp., one fragment. Sapindus obiusifolius Lesquereux. Two or three Lygodium kaulfusii Herr (L. neuropteroides Lesq.). examples. Abundant. Cinchonidium, cf. C. ovata Lesquereux. Two or three Populus cuneata Newberry. Abundant. examples. Populus glandulifera Herr. Abundant. Carpi^es sp. Populus zaddachi Herr. Abundant.
RMCBYP2J–Yellowstone National Park was established in 1872 and covers 3,468 square miles. The largest supervolcano on the continent, Yellowstone Caldera, is inside the park and considered active. In 1988, one of the many seasonal forest fires burned over one third of the park.
RMRNYRJC–WY03822-00...WYOMING - Hiker passing a colorful hot spring, part of the Middle Group of the Heart Lake Geyser Basin in the backcountry of Yellowstone
RM2AWP9H8–Geology and water resources of the Bighorn Basin, Wyoming . ection with the present investigation. The rocks consist largely of volcanicbreccias and lava flows interbedded with sandstones and shales which have a thicknessof many thousand feet. They overlap unconformably all the older rocks, outcrop-ping along the western side of the Bighorn basin, as shown in the cross sections(PL IV, p. 8). On the northern side of the Middle Fork of Owl Creek, near its head,fossil leaves were discovered by Mr. N. H. Darton, which have been identified by Mr.Knowlton, as follows: U. S, G EOLOGICAL SURVEY PROFES
RMRFRNGT–. Carnegie Institution of Washington publication. . Figs. 428—431.—Echmatemys shaughnessiana. Carapace and plastron ot type. 428. Carapace. Xj. Parts restored are shown by interrupted lines. 429. Plastron. Xj- 4^0. I'pper surface of front lobe of plastron. Xl- 431. Tpper surface of border of hinder lobe of plastron. XI. the Brido-er deposits of Wyoming, in 1872, on Cottonwood Creek, therefore about the middle of stage B. The type of the species is now in the possession of the Museum of Natural History and bears the number 1069. A further description is here turnisht as well as figures of both
![. The age of mammals in Europe, Asia and North America. Mammals, Fossil; Paleontology. KEY TO MAP PT. Puerro, Torrpjon, tind Wasatch of San Juan basin. New Moxico Basal und lower Eocene. BH. Wasatch of Bighorn Baain. Wyoming. Lower Eocene. W. Wasatch (typical). Evanaton. Wy- ominft Lower Eocene. WB. Wind Ilivcr, Wyoming Lower Eocene. H. Huerfano. Colorado Lower and middle Eocene. B. Bridgcr, Wyoming Middle Eocene. "WK. ?? Washakie." Wyoming Middle ami upper Eocene. U. Uinta. Utah Middle and upper Eocene. 12. White River deposits along Swift Current Creek, Assinihoia, Canada Lctwer tH Stock Photo](https://c8.alamy.com/comp/RR0M04/the-age-of-mammals-in-europe-asia-and-north-america-mammals-fossil-paleontology-key-to-map-pt-puerro-torrpjon-tind-wasatch-of-san-juan-basin-new-moxico-basal-und-lower-eocene-bh-wasatch-of-bighorn-baain-wyoming-lower-eocene-w-wasatch-typical-evanaton-wy-ominft-lower-eocene-wb-wind-ilivcr-wyoming-lower-eocene-h-huerfano-colorado-lower-and-middle-eocene-b-bridgcr-wyoming-middle-eocene-quotwk-washakiequot-wyoming-middle-ami-upper-eocene-u-uinta-utah-middle-and-upper-eocene-12-white-river-deposits-along-swift-current-creek-assinihoia-canada-lctwer-th-RR0M04.jpg ". The age of mammals in Europe, Asia and North America. Mammals, Fossil; Paleontology. KEY TO MAP PT. Puerro, Torrpjon, tind Wasatch of San Juan basin. New Moxico Basal und lower Eocene. BH. Wasatch of Bighorn Baain. Wyoming. Lower Eocene. W. Wasatch (typical). Evanaton. Wy- ominft Lower Eocene. WB. Wind Ilivcr, Wyoming Lower Eocene. H. Huerfano. Colorado Lower and middle Eocene. B. Bridgcr, Wyoming Middle Eocene. "WK. ?? Washakie." Wyoming Middle ami upper Eocene. U. Uinta. Utah Middle and upper Eocene. 12. White River deposits along Swift Current Creek, Assinihoia, Canada Lctwer tH Stock Photo")
RMRR0M04–. The age of mammals in Europe, Asia and North America. Mammals, Fossil; Paleontology. KEY TO MAP PT. Puerro, Torrpjon, tind Wasatch of San Juan basin. New Moxico Basal und lower Eocene. BH. Wasatch of Bighorn Baain. Wyoming. Lower Eocene. W. Wasatch (typical). Evanaton. Wy- ominft Lower Eocene. WB. Wind Ilivcr, Wyoming Lower Eocene. H. Huerfano. Colorado Lower and middle Eocene. B. Bridgcr, Wyoming Middle Eocene. "WK. ?? Washakie." Wyoming Middle ami upper Eocene. U. Uinta. Utah Middle and upper Eocene. 12. White River deposits along Swift Current Creek, Assinihoia, Canada Lctwer tH
RMRCEKHC–. Dinocerata : a monograph of an extinct order of gigantic mammals. Dinocerata; Mammals, Fossil; Paleontology; Paleontology. SYNOPSIS. 213 The type specimen (number 1037) of this species was discovered by Messrs. J. W. Chew and B. D. Smith, near Bitter Creek, Wyoming, in 1872. This specimen consists of upper premolars, molars, and a radius. The geological horizon is in the Bridger beds of the Middle Eocene. The known remains of this species are preserved in the Museum of Yale College. Tinoceras latum, Marsh, n. s. Woodcuts: 189 and 190, below.. Please note that these images are extracted from
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