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Gypsiferous Stock Photos and Images
RMW6CFF7–AERIAL VIEW. Large field (length: 750m) of sinkholes (diameter: up to 30m) in a gypsiferous rock. Les Gypsières, Valloire, Savoie, France.
RMPPDB62–NAVARRE. LAS BARDENAS REALES. Steppe landscape southeast of Navarra, between the Ebro and Aragón rivers. It is divided into the Bárdena Blanca, whitish territory by the abundance of gypsiferous marls and gypsum and the Bárdena Negra, with vegetation of Aleppo, Juniper and Kermes oak tree.
RM2AJ234A–The five great monarchies of the ancient eastern world; or, The history, geography, and antiquites of Chaldaea, Assyria, Babylon, Media, and Persia . at except in the immediate vicinity of thehills north and south, and along the courses of theKhabour, the Belik, and their aflluents, there is littlenatural fertility, and cultivation is difficult. Thesoil too is often gypsiferous; and its salt and nitrousexudations destroy vegetation ; ^ while at the same ?• Aiiiswurth, 1. s. c. I ?* Ibid. p. 51. 3 Layard, p. 304. j ^ Jbid. p. 324. Chap. I. VOLCANIC HILL OF KOUKAB. 237 time the streams and sprin
RMRMKTDT–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. Km. Fig. 19. Locality map of sampling sites at Berg River mouth, west Cape coast. Both samples are rather gypsiferous, though this would seem to be a secondary feature derived from the overlying Holocene estuary. Present-day environments in the estuary are markedly hypersaline, and some areas are utilized for salt production. However, the foraminifera of the latest Pleistocene Unit III reveal a much more normal marine environment. Cibicides lobatulus (Walker & Jacob) occurs in fairly small number
RMRMNP8W–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. OSTRACODA FROM QUATERNARY COASTAL SEQUENCES 105 gypsiferous beds at the top. We have indicated these changes in Figure 17, but can only speculate that they were contemporaneous with the same part of the cycle at Draaihoek. Ostracod abundances (Fig. 20) are generally lower than found at Draaihoek (< 50 valves/10 g), with the notable exception of the fresh- water sands immediately below the gypsiferous beds (500 valves/10 g), where there is a marked influx in numbers of Sarscypridopsis reniformis (p
RMRE9FRD–. Contributions to the geography of the United States, 1923-1924. Geology; Mines and mineral resources. EB-OSIOISr BY SOLUTION AND FILL. 109 SOLUTION CAVITIES. SOLUBLE ROCKS. It is significant that much of the material penetrated in the well whose record is given above is soluble. According to this record the drill went through 1,378 feet of limestone, 87 feet of gypsum, 99 feet of rock salt, and 342 feet of insoluble material. The Big lime is underlain by another group of gypsiferous red beds and a still older massive limestone, and much soluble material occurs in the rocks younger than those
![. Bulletin of the Geological Society of America. Geology. Figuee 1.—Gateway of Garden of the Gods, Colorado Springs, Colorado Pikes Peak in western distance; "gateway" is of lower Wyoming red grits ; white ledge is "creamy sandstone " (Tensleep) at top of lower Wyoming; gypsum bed at top of upper Wyoming in foreground. Figure 2.—Gateway ok Perry Park, south of Denver, Colorado Vertical beds of lower Wyoming red grits in foreground; two sandstones of "Dakota'- in distance, surmounting slopes of Morrison shales and gypsiferous red beds GATEWAY OF GARDEN OF THE GODS AND O Stock Photo](https://c8.alamy.com/comp/RGGWMJ/bulletin-of-the-geological-society-of-america-geology-figuee-1gateway-of-garden-of-the-gods-colorado-springs-colorado-pikes-peak-in-western-distance-quotgatewayquot-is-of-lower-wyoming-red-grits-white-ledge-is-quotcreamy-sandstone-quot-tensleep-at-top-of-lower-wyoming-gypsum-bed-at-top-of-upper-wyoming-in-foreground-figure-2gateway-ok-perry-park-south-of-denver-colorado-vertical-beds-of-lower-wyoming-red-grits-in-foreground-two-sandstones-of-quotdakota-in-distance-surmounting-slopes-of-morrison-shales-and-gypsiferous-red-beds-gateway-of-garden-of-the-gods-and-o-RGGWMJ.jpg ". Bulletin of the Geological Society of America. Geology. Figuee 1.—Gateway of Garden of the Gods, Colorado Springs, Colorado Pikes Peak in western distance; "gateway" is of lower Wyoming red grits ; white ledge is "creamy sandstone " (Tensleep) at top of lower Wyoming; gypsum bed at top of upper Wyoming in foreground. Figure 2.—Gateway ok Perry Park, south of Denver, Colorado Vertical beds of lower Wyoming red grits in foreground; two sandstones of "Dakota'- in distance, surmounting slopes of Morrison shales and gypsiferous red beds GATEWAY OF GARDEN OF THE GODS AND O Stock Photo")
RMRGGWMJ–. Bulletin of the Geological Society of America. Geology. Figuee 1.—Gateway of Garden of the Gods, Colorado Springs, Colorado Pikes Peak in western distance; "gateway" is of lower Wyoming red grits ; white ledge is "creamy sandstone " (Tensleep) at top of lower Wyoming; gypsum bed at top of upper Wyoming in foreground. Figure 2.—Gateway ok Perry Park, south of Denver, Colorado Vertical beds of lower Wyoming red grits in foreground; two sandstones of "Dakota'- in distance, surmounting slopes of Morrison shales and gypsiferous red beds GATEWAY OF GARDEN OF THE GODS AND O
RMRJY6Y7–. Atoll research bulletin. Coral reefs and islands; Marine biology; Marine sciences. Fig. 4. Gypsiferous units in Core 3, showing Beds G-J (cf. Fig. 8). H, I and J are more than half seed gypsum. Lighter laminae are highest in gypsum; darkest ones have conspicuous slime of clay and organic residues. Bar of 2 cm measures dry, compacted thickness.. Fig. 5.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Smithsonian Instituti
![. Bulletins of American paleontology. Horizon of Yawger's Woods and Field below Woods North of O'Connor's Q'y 1^ LdJ z Orth. interslriatm Whit, sulcata Cobleskill Light, impure l's Gypsiferous shale Onondaga l's Oriskany s's ,-, • , e , £ve-n-be,Ided Fs °?****y Sandstone. Unexposed -- Cobleskill ferGray, impure ia limestone Sawyer Creek and Thompson Q'y Onondaga l's Banded l's Stromatopora bed Heavy bedded fossiliferous-1': =bp^ Impure, drab l's Unexposed Cobleskill Strom'a Gray, impure l's g Irregularly bed- 59 ded limestone —"=^ Gypsu CORRELATION OF THE MORE IMPORTANT SHURIC ROCK OUTCR Stock Photo](https://c8.alamy.com/comp/RG9MWP/bulletins-of-american-paleontology-horizon-of-yawgers-woods-and-field-below-woods-north-of-oconnors-qy-1-ldj-z-orth-interslriatm-whit-sulcata-cobleskill-light-impure-ls-gypsiferous-shale-onondaga-ls-oriskany-ss-e-ve-n-beided-fs-y-sandstone-unexposed-cobleskill-fergray-impure-ia-limestone-sawyer-creek-and-thompson-qy-onondaga-ls-banded-ls-stromatopora-bed-heavy-bedded-fossiliferous-1-=bp-impure-drab-ls-unexposed-cobleskill-stroma-gray-impure-ls-g-irregularly-bed-59-ded-limestone-quot=-gypsu-correlation-of-the-more-important-shuric-rock-outcr-RG9MWP.jpg ". Bulletins of American paleontology. Horizon of Yawger's Woods and Field below Woods North of O'Connor's Q'y 1^ LdJ z Orth. interslriatm Whit, sulcata Cobleskill Light, impure l's Gypsiferous shale Onondaga l's Oriskany s's ,-, • , e , £ve-n-be,Ided Fs °?****y Sandstone. Unexposed -- Cobleskill ferGray, impure ia limestone Sawyer Creek and Thompson Q'y Onondaga l's Banded l's Stromatopora bed Heavy bedded fossiliferous-1': =bp^ Impure, drab l's Unexposed Cobleskill Strom'a Gray, impure l's g Irregularly bed- 59 ded limestone —"=^ Gypsu CORRELATION OF THE MORE IMPORTANT SHURIC ROCK OUTCR Stock Photo")
RMRG9MWP–. Bulletins of American paleontology. Horizon of Yawger's Woods and Field below Woods North of O'Connor's Q'y 1^ LdJ z Orth. interslriatm Whit, sulcata Cobleskill Light, impure l's Gypsiferous shale Onondaga l's Oriskany s's ,-, • , e , £ve-n-be,Ided Fs °?****y Sandstone. Unexposed -- Cobleskill ferGray, impure ia limestone Sawyer Creek and Thompson Q'y Onondaga l's Banded l's Stromatopora bed Heavy bedded fossiliferous-1': =bp^ Impure, drab l's Unexposed Cobleskill Strom'a Gray, impure l's g Irregularly bed- 59 ded limestone —"=^ Gypsu CORRELATION OF THE MORE IMPORTANT SHURIC ROCK OUTCR
RMRG9MX3–. Bulletins of American paleontology. gull Jfm. pal'.,, ir-oi, X[, Mo- 1§, pi: Union Springs and Frontenac Island â Heavy-bedded St. varistriata Alternating light and dark beds with Sp. van'i. Horizon of Yawger's Woods and Field below Woods North of O'Connor's Q'y 1^ LdJ z Orth. interslriatm Whit, sulcata Cobleskill Light, impure l's Gypsiferous shale Onondaga l's Oriskany s's ,-, ⢠, e , £ve-n-be,Ided Fs °?****y Sandstone. Unexposed -- Cobleskill ferGray, impure ia limestone Sawyer Creek and Thompson Q'y Onondaga l's Banded l's Stromatopora bed Heavy bedded fossiliferous-1': =bp^ Impure,
Search Results for Gypsiferous Stock Photos and Images (20)
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