Quick filters:
Clastic Stock Photos and Images
RF2PXRT65–Flysch is a series of marine sedimentary rocks that are predominantly clastic in origin and are characterized by the alternation of several lithologic
RF2T68166–Conglomerate is a clastic sedimentary rock. This sample comes from L'Ametlla de Mar, Tarragona province, Catalonia, Spain.
RMPFXPBD–. The nature and properties of soils; a college text of edaphology. Soils. 50 NATURE AND PROPERTIES OF SOILS importance. The type of farming and the crops grown on any area of alliwial soil will vary with climate, soil conditions, and markets. 29. Marine soils.^—^A great deal of the sediment carried away by stream action is eventiially deposited in the sea, the coarser fragments near the shore, the finer particles at a distance. Such material is largely clastic and if there have. Fig. 11.—^Block diagram showing how marine soils are formed and their relation to the uplands. The emerged coastal
RFKG68JG–macro shooting of natural mineral rock specimen - rough Shale stone on dark granite background
RF2WWTD0F–Close view of Arizona sandstone. Jerome, Arizona, USA, by Dominique Braud/Dembinsky Photo Assoc
RF2E52X8N–Backhoe bucket digging the soil at agriculture farm to make pond. Crawler excavator digging at shale layer. Excavating machine. Earth moving equipment
RF2F99BWW–Limestone is a sedimentary rock forms when layers of skeletal fragments of marine organisms such as coral, foraminifera & molluscs accumulates by sedi
RM2AKT0W2–Canadian mining journal January-June 1905 . region, whereas, the formation above it to the east was afine grained pyro-clastic rock which was submitted to Dr. A.W. G. Wilson, of McGill, for microscopic examination. Dr.Wilson reports the constituent minerals to be angular grainsof quartz, plagioclase and some orthoclase which is frequentlydecomposed to muscovite. Associated with these three miner-als are small grains of biotite, magnetite and secondary epi-dote, the whole being cemented together by chlorite. Therock has a dark green color with spots of black which the mi-croscope shows are aggr
RMRFNJ5B–close-up view conglomerate rock inside salnitre caves in Montserrat, Collbató, Catalonia, Spain
RMPEE0BJ–A quarry with red sandstone, Bad Karlshafen, Upper Weser Valley, Weser Uplands, Weserbergland, Reinhardswald, Hesse, Germany, Europe
RFPY0PA5–Sediments of various ancient environments take millions of years to lithify into the stratified layers we see in the rocky mountains.
RF2PXAAA4–Flysch is a series of marine sedimentary rocks that are predominantly clastic in origin and are characterized by the alternation of several lithologic
RF2T7A82K–Colorful sandstone. Sandstone is a clastic sedimentary rock composed of quartz grains. This photo was taken in Dead Sea, Jordan.
RMPFXP2R–. Geology of the Narragansett basin. Geology. RHODE ISLAND GOAL MEASURES. 165 G/ac/aJ drift as regards both attitude and alteration. They not only lie in less disturbed positions, but they preserve to a much greater degree their original clastic texture, and fossils are of frequent occurrence in them. An account of the* more typical exposures as they now exist follows: Leonards Corner quarries.—In tho southeastom triauglo formod by the roads, at an elevation of about 100 feet above the sea, is an exposure of pebbly sandstone on the site of a rock crusher. The strike here is about east-west and
RFMAPT9M–macro shooting of natural mineral rock specimen - raw Shale stone on white marble background
RFT85PKE–Exploration in a sandstone rock with a slope layer and intermediate banks of conglomerate, deposited close to the coast, with pyramids in the backgrou
RF2WWTEA4–Close view of Arizona sandstone. Jerome, Arizona, USA, by Dominique Braud/Dembinsky Photo Assoc
RF2EAE88K–Backhoe working by digging soil at construction site. Bucket teeth of backhoe digging soil. Crawler excavator digging on soil. Excavating machine.
RF2F99CA0–Rocks banding pattern of stratification in sedimentary rocks due to changes in texture or composition during deposition at Himalayas of Spiti . Sedime
RM2ANDB0E–A treatise on zoology . escribed, Rather, 1893), Silurian, Kurope,and probably N. America. Crown bent, in the transversal plane, backon the stem, which is then coiled around it in the opposite direction(Fig. LIX.). The coil could be tight, or could be uncoiled and the crownexposed ; the movement was ellectod by an clastic ligament towards theinner margin of the columnals, counteiact.fd by strong muscles towardsthe outer margin, the fulcrum being a transverse ridge. Columnals show THE CRINOIDEA H7 traces of orip;inal pentaTnerism, hut over the f^roater part of the stem arecresceiitic iii sectio
RMRFNHTY–close-up view conglomerate rock inside salnitre caves in Montserrat, Collbató, Catalonia, Spain
RMPEE0K4–A quarry with red sandstone, Bad Karlshafen, Upper Weser Valley, Weser Uplands, Weserbergland, Reinhardswald, Hesse, Germany, Europe
RFPY0TT6–Sediments of various ancient environments take millions of years to lithify into the stratified layers we see in the rocky mountains.
RF2PXKWT0–Flysch is a series of marine sedimentary rocks that are predominantly clastic in origin and are characterized by the alternation of several lithologic
RF2T680HM–Conglomerate is a clastic sedimentary rock. This photo was taken in L'Ametlla de Mar coast, Tarragona province, Catalonia, Spain.
RMPFN4E3–. The cyclopædia of anatomy and physiology. Anatomy; Physiology; Zoology. 690 UTERUS AND ITS APPENDAGES. mass, so that a muscular rather than a fibrous it may be easily detached and turned out of tissue results. A small quantity of clastic its investing capsule (/%. 475 ). fibre is also occasionally found in these ute- rine formations. Fig. 475. Fig. 474-.. Section of fibroid tumour of the uterus. (Ad Nat.) The structural variations observable in fibroid of the uterus, are dependent chiefly upon the peculiarities in arrangement of these component elements. In the more dense formations, the whi
RFKG68JJ–macro shooting of natural mineral rock specimen - raw Shale stone on dark granite background
RM2RA9NBM–Wildflowers growing on the cliff-face beside the main railway line at Dawlish, South Devon.
RF2DEKTKM–Gran Canaria, amazing sand stone erosion figures in ravines on Punta de las Arenas cape on the western part of the island, also called Playa de Artena
RF2WX2RB0–Close view of Arizona sandstone. Jerome, Arizona, USA, by Dominique Braud/Dembinsky Photo Assoc
RF2A5DG9B–watercolor illustration: Exploration in a sandstone rock with a slope layer and intermediate banks of conglomerate, deposited close to the coast, with
RF2F99C9J–Rocks banding pattern of stratification in sedimentary rocks due to changes in texture or composition during deposition at Himalayas of Spiti . Sedime
RM2AXHHK8–Geology . ckbeds of limestone (or chalk) occur in other parts of the series. In thevicinity of the shores, especially next to the Ouachita uplift, wherethe shore phases of the formation are best known, the formation isrelatively thin and mainly clastic. The Fredericksburg series ismuch less variable, both in thickness and composition, than the Trinityseries below, and contains more calcareous material. The Fredericksburg formation is overlain by the Washita, a serieswhich records an epoch of shoaling waters, though the sea was some- 1 Hill, op. cit., p. 129 et seq. 2 Idem. 3 Eldridge, Bull. 21
RMRFNJ0T–close-up view conglomerate rock inside salnitre caves in Montserrat, Collbató, Catalonia, Spain
RMPEE062–A quarry with red sandstone, Bad Karlshafen, Upper Weser Valley, Weser Uplands, Weserbergland, Reinhardswald, Hesse, Germany, Europe
RFPY0W17–Sediments of various ancient environments take millions of years to lithify into the stratified layers we see in the rocky mountains.
RFWB4B73–mineralogical specimen conglomerate of morion crystals, feldspar and mica isolated on gray background
RF2PXKWTD–Flysch is a series of marine sedimentary rocks that are predominantly clastic in origin and are characterized by the alternation of several lithologic
RMRP3X3R–Coastal, Erosion,crack,slump,debris, on the, beach, pipes, cracks, cliffs, lower, greensand, wealden, beds, geology, Compton, Bay, Isle of Wight, UK,
RF2REXPDX–Conglomerate is a clastic sedimentary rock composed of rounded clasts (pudding stone). This photo was taken in Menorca, Balearic Islands, Spain.
![. A manual of zoology. Zoology. us MOLLUSCA arc o]icneil hv an clastic hinge ligaDioit usually placed dorsal to and be- hind ihc l"LiuL,'c. The shell is closed Ijy addiiitor iiiiisclfs which extend through the IkhIv from shell to shell, lea-inL^ their impressions on the inner surface (I'ig. 310). Usually there occur an anterior and a posterior adductor ciiually well developed (Ditnyaria); less frei|ueinly the anterior is rudimentary (Heteromyaria) or entirel)' disappears (Monomyaria). ^^'hen the muscles are relaxed the elastic ligament opens the 'al-es. The Inirroiloiil hinge is the ty Stock Photo](https://c8.alamy.com/comp/PG401D/a-manual-of-zoology-zoology-us-mollusca-arc-o-icneil-hv-an-clastic-hinge-ligadioit-usually-placed-dorsal-to-and-be-hind-ihc-lquotliulc-the-shell-is-closed-ijy-addiiitor-iiiiisclfs-which-extend-through-the-ikhiv-from-shell-to-shell-lea-inl-their-impressions-on-the-inner-surface-iig-310-usually-there-occur-an-anterior-and-a-posterior-adductor-ciiually-well-developed-ditnyaria-less-freiueinly-the-anterior-is-rudimentary-heteromyaria-or-entirel-disappears-monomyaria-hen-the-muscles-are-relaxed-the-elastic-ligament-opens-the-al-es-the-inirroiloiil-hinge-is-the-ty-PG401D.jpg ". A manual of zoology. Zoology. us MOLLUSCA arc o]icneil hv an clastic hinge ligaDioit usually placed dorsal to and be- hind ihc l"LiuL,'c. The shell is closed Ijy addiiitor iiiiisclfs which extend through the IkhIv from shell to shell, lea-inL^ their impressions on the inner surface (I'ig. 310). Usually there occur an anterior and a posterior adductor ciiually well developed (Ditnyaria); less frei|ueinly the anterior is rudimentary (Heteromyaria) or entirel)' disappears (Monomyaria). ^^'hen the muscles are relaxed the elastic ligament opens the 'al-es. The Inirroiloiil hinge is the ty Stock Photo")
RMPG401D–. A manual of zoology. Zoology. us MOLLUSCA arc o]icneil hv an clastic hinge ligaDioit usually placed dorsal to and be- hind ihc l"LiuL,'c. The shell is closed Ijy addiiitor iiiiisclfs which extend through the IkhIv from shell to shell, lea-inL^ their impressions on the inner surface (I'ig. 310). Usually there occur an anterior and a posterior adductor ciiually well developed (Ditnyaria); less frei|ueinly the anterior is rudimentary (Heteromyaria) or entirel)' disappears (Monomyaria). ^^'hen the muscles are relaxed the elastic ligament opens the 'al-es. The Inirroiloiil hinge is the ty
RFMAPTBA–macro shooting of natural mineral rock specimen - raw Conglomerate stone on white marble background
RM2RA9NC4–Wildflowers growing on the cliff-face beside the main railway line at Dawlish, South Devon.
RF2JBC336–Gran Canaria, amazing sand stone erosion figures in ravines on Punta de las Arenas cape on the western part of the island, also called Playa de Artena
RF2WXN61Y–Close view of Arizona sandstone. Jerome, Arizona, USA, by Dominique Braud/Dembinsky Photo Assoc
RFMNK974–Afromontane forest growing next to exposed sedimentary sandstone formations in the Drakensberg at Giants Castle nature reserve
RF2F99BPT–Rocks banding pattern of stratification in sedimentary rocks due to changes in texture or composition during deposition at Himalayas of Spiti . Sedime
RM2AJ3XPT–India rubber world . makesgaskets of any size or shape with-out waste. A RUBBER PACKING with one ormore plies of pliable sheet metal in-sertion. Forsyth Combination Packing willsatisfactorily withstand the heat of hiohpressure steam, and is not so liable to blowout as ordinary packings. It is practicallya metal packing with clastic surfaces. Apractical trial of Forsyth Combination Pack-ing invariably results in a strong endorse-ment of it. CAUTIOIN As the exclusive manufacturers of sheet metal insertion rubber packingand gasket tubing, under a patent issued April ii, 1899, to James Bennett For
RMRFNHPJ–close-up view conglomerate rock inside salnitre caves in Montserrat, Collbató, Catalonia, Spain
RMPEE0D5–A quarry with red sandstone, Bad Karlshafen, Upper Weser Valley, Weser Uplands, Weserbergland, Reinhardswald, Hesse, Germany, Europe
RFPY0TN1–Sediments of various ancient environments take millions of years to lithify into the stratified layers we see in the rocky mountains.
RFWB4BM8–mineralogical specimen conglomerate of morion crystals, feldspar and mica isolated on gray background
RF2PXKWR8–Flysch is a series of marine sedimentary rocks that are predominantly clastic in origin and are characterized by the alternation of several lithologic
RMRP3X2D–Coastal, Erosion, debris, on the, beach, pipes, cracks, cliffs, lower, greensand, wealden, beds, geology, Compton, Bay, Isle of Wight, UK,
RF2T7A80K–Sandstone is a clastic sedimentary rock composed of quartz grains. This sample comes from Sierra de Albarracín, Teruel, Aragón, Spain..
RMPG3NP7–. A manual of zoology. Zoology. 42 S ARTHROrODA Yet all Rhvnchota may he recognized by the sucking proboscis (fig. 47S'), consistint; of the grooved laluum in which the neeilledil^e mantlililes and maxillx play. The wing structures atlord tlie basis of division into three sub orders. Sub Order I. IIEMIPTKRA (Heterop- tcra) .nlcrior wings hcmclytra, i.e., lealh- erv at base, soft and clastic al lip (tig. 479); between the benielvlra is a conspicuous triangular scutelUini (.f) covering more or less of the dorsal surface. Hcmclytra ard scutellum occasionally disa|>pcar. A further characterist
RFMAPTE6–macro shooting of natural mineral rock specimen - rough sandstone stone on white marble background
RF2JBC19K–Gran Canaria, amazing sand stone erosion figures in ravines on Punta de las Arenas cape on the western part of the island, also called Playa de Artena
RF2WX2RDY–Close view of Arizona sandstone. Jerome, Arizona, USA, by Dominique Braud/Dembinsky Photo Assoc
RF2F99C77–Strata of Mudrocks, it is a silicicastic sedimentary rock include siltstone, claystone, mudstone, slate & shale formed by accumulated sedimentation th
RM2AN740J–Annual report of the United States Geological Survey to the Secretary of the Interior . e layer 575 feet. The clastic series of the Mountain mine may be said to eud here, the entire thick-ness (Nos. 603-607 and 599) being approximately 700 feet. 10. Next east is No. 608. Quartz-porphyry tuff. The microscope shows this to beplainly clastic and to contain microlitic fragments, cryptocrystalliuo granular frag-ments (chert?), rounded volcanic quartzes, and fragments! feldspars. There areinterbedded with this material a few thin layers of siliceous argillite. 11. No. 609. Also a quartz-porphyry tuf
RMRFNHK6–close-up view conglomerate rock inside salnitre caves in Montserrat, Collbató, Catalonia, Spain
RMJ3GP7W–Old walls built with red sandstone from the Weserbergland, Krukenburg Castle, Helmarshausen, Bad Karlshafen, Hesse, Germany, Europe
RFPY0TR6–Sediments of various ancient environments take millions of years to lithify into the stratified layers we see in the rocky mountains.
RFWB45BR–intergrowth of unusual flat and fibrous feldspar and morion crystals isolated on white background
RF2PXAA9X–Flysch is a series of marine sedimentary rocks that are predominantly clastic in origin and are characterized by the alternation of several lithologic
Search Results for Clastic Stock Photos and Images (1,523)
Page 6 of 16