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Silicified limestone Stock Photos and Images
Outcrop of banded Chert, part of the Carboniferous, Pentre Chert formation, Halkyn, Wales, UK. January. The Chert is silicified Limestone, made up in part of micro organism Radiolaria. This is one of the rock types that is targetted for 'Fracking' with gas contained within fractures. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/outcrop-of-banded-chert-part-of-the-carboniferous-pentre-chert-formation-halkyn-wales-uk-january-the-chert-is-silicified-limestone-made-up-in-part-of-micro-organism-radiolaria-this-is-one-of-the-rock-types-that-is-targetted-for-fracking-with-gas-contained-within-fractures-image612140134.htmlRM2XFWAYJ–Outcrop of banded Chert, part of the Carboniferous, Pentre Chert formation, Halkyn, Wales, UK. January. The Chert is silicified Limestone, made up in part of micro organism Radiolaria. This is one of the rock types that is targetted for 'Fracking' with gas contained within fractures.
Thinly-bedded silicified Silurian limestones forming cliffs between Portrane and Donabate, County Dublin, Ireland Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-thinly-bedded-silicified-silurian-limestones-forming-cliffs-between-52984505.htmlRMD25J7N–Thinly-bedded silicified Silurian limestones forming cliffs between Portrane and Donabate, County Dublin, Ireland
Fragment of limestone rock with silicified marine fossils. Carboniferous period, central Russia Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/fragment-of-limestone-rock-with-silicified-marine-fossils-carboniferous-period-central-russia-image562175503.htmlRF2RJH8GF–Fragment of limestone rock with silicified marine fossils. Carboniferous period, central Russia
Doughnut shaped burr marking the site of an ancient tree, Fossil Forest, Lulworth Cove, Dorset, England Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-doughnut-shaped-burr-marking-the-site-of-an-ancient-tree-fossil-forest-31797870.htmlRMBRMEE6–Doughnut shaped burr marking the site of an ancient tree, Fossil Forest, Lulworth Cove, Dorset, England
Calcite or Quartz found at Rock Garden (Rock Zoo of Duqm or Duqm Stone Park), a famous tourist attraction of a 3 sqkm of rock formation, Duqm, Oman Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-calcite-or-quartz-found-at-rock-garden-rock-zoo-of-duqm-or-duqm-stone-171955686.htmlRMKYN76E–Calcite or Quartz found at Rock Garden (Rock Zoo of Duqm or Duqm Stone Park), a famous tourist attraction of a 3 sqkm of rock formation, Duqm, Oman
A weathered wooden stake used as a bollard on the quay in the harbour in Boscastle, with a water covered rock face. Cornwall.England.UK Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-weathered-wooden-stake-used-as-a-bollard-on-the-quay-in-the-harbour-in-boscastle-with-a-water-covered-rock-face-cornwallenglanduk-image466267715.htmlRF2J2G96B–A weathered wooden stake used as a bollard on the quay in the harbour in Boscastle, with a water covered rock face. Cornwall.England.UK
Carved millstones Hathersage Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-carved-millstones-hathersage-18340472.htmlRFB1RDCT–Carved millstones Hathersage
Detail of a millstone located beside the Holodomor Monument and Museum dedicated to the 1932-1933 famine in Kiev, Ukraine Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-detail-of-a-millstone-located-beside-the-holodomor-monument-and-museum-33226221.htmlRMBX1GAN–Detail of a millstone located beside the Holodomor Monument and Museum dedicated to the 1932-1933 famine in Kiev, Ukraine
The geology of Hardin County, and the adjoining part of Pope County . Quartz (Q), sphalerite (blende) (B) and calcite (Ca),Magnification 150 diameters. Illinois State Geological Survey Bulletin No. 41, Plate II-C. A. Veinlet of fluorite (P) containing later sulphides in silicified limestone(L). A transition zone into wall-rock material is indicated. The rock containsalso many specks, apparently of fluorite. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-geology-of-hardin-county-and-the-adjoining-part-of-pope-county-quartz-q-sphalerite-blende-b-and-calcite-camagnification-150-diameters-illinois-state-geological-survey-bulletin-no-41-plate-ii-c-a-veinlet-of-fluorite-p-containing-later-sulphides-in-silicified-limestonel-a-transition-zone-into-wall-rock-material-is-indicated-the-rock-containsalso-many-specks-apparently-of-fluorite-image338430762.htmlRM2AJGRTX–The geology of Hardin County, and the adjoining part of Pope County . Quartz (Q), sphalerite (blende) (B) and calcite (Ca),Magnification 150 diameters. Illinois State Geological Survey Bulletin No. 41, Plate II-C. A. Veinlet of fluorite (P) containing later sulphides in silicified limestone(L). A transition zone into wall-rock material is indicated. The rock containsalso many specks, apparently of fluorite.
. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 169 Oyat, Cyathophyllum dianthus, Goldfuss, Petref. 1826, p. 54, pi. 15, fig. 13 ; pi. 16, fig. 1. Hall, Geology of the Western District of New York, 1843, page 160, fig, 63,2. Tipper Ilelderbevg (Onond- aga) formation. (Murchison, SiL Research, page 690, pi. 16, figs. 12, 12a, 12 c.) Usually shows in large silicified bunches projecting from the weathered surfaces of the limestone rocks. The figure is a small portion of one of these masses of coral. Abundant Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-dictionary-of-the-fossils-of-pennsylvania-and-neighboring-states-named-in-the-reports-and-catalogues-of-the-survey-paleontology-169-oyat-cyathophyllum-dianthus-goldfuss-petref-1826-p-54-pi-15-fig-13-pi-16-fig-1-hall-geology-of-the-western-district-of-new-york-1843-page-160-fig-632-tipper-ilelderbevg-onond-aga-formation-murchison-sil-research-page-690-pi-16-figs-12-12a-12-c-usually-shows-in-large-silicified-bunches-projecting-from-the-weathered-surfaces-of-the-limestone-rocks-the-figure-is-a-small-portion-of-one-of-these-masses-of-coral-abundant-image216329676.htmlRMPFXJKT–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 169 Oyat, Cyathophyllum dianthus, Goldfuss, Petref. 1826, p. 54, pi. 15, fig. 13 ; pi. 16, fig. 1. Hall, Geology of the Western District of New York, 1843, page 160, fig, 63,2. Tipper Ilelderbevg (Onond- aga) formation. (Murchison, SiL Research, page 690, pi. 16, figs. 12, 12a, 12 c.) Usually shows in large silicified bunches projecting from the weathered surfaces of the limestone rocks. The figure is a small portion of one of these masses of coral. Abundant
Outcrop of banded Chert, part of the Carboniferous, Pentre Chert formation, Halkyn, Wales, UK. January. The Chert is silicified Limestone, made up in part of micro organism Radiolaria. This is one of the rock types that is targetted for 'Fracking' with gas contained within fractures. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/outcrop-of-banded-chert-part-of-the-carboniferous-pentre-chert-formation-halkyn-wales-uk-january-the-chert-is-silicified-limestone-made-up-in-part-of-micro-organism-radiolaria-this-is-one-of-the-rock-types-that-is-targetted-for-fracking-with-gas-contained-within-fractures-image612140140.htmlRM2XFWAYT–Outcrop of banded Chert, part of the Carboniferous, Pentre Chert formation, Halkyn, Wales, UK. January. The Chert is silicified Limestone, made up in part of micro organism Radiolaria. This is one of the rock types that is targetted for 'Fracking' with gas contained within fractures.
Sea cave in the cliffs between Portrane and Donabate, County Dublin, Ireland Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sea-cave-in-the-cliffs-between-portrane-and-donabate-county-dublin-52984653.htmlRMD25JD1–Sea cave in the cliffs between Portrane and Donabate, County Dublin, Ireland
Fragment of limestone rock with silicified marine fossils. Carboniferous period, central Russia Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/fragment-of-limestone-rock-with-silicified-marine-fossils-carboniferous-period-central-russia-image562175519.htmlRF2RJH8H3–Fragment of limestone rock with silicified marine fossils. Carboniferous period, central Russia
Calcite or Quartz found at Rock Garden (Rock Zoo of Duqm or Duqm Stone Park), a famous tourist attraction of a 3 sqkm of rock formation, Duqm, Oman Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-calcite-or-quartz-found-at-rock-garden-rock-zoo-of-duqm-or-duqm-stone-171955565.htmlRMKYN725–Calcite or Quartz found at Rock Garden (Rock Zoo of Duqm or Duqm Stone Park), a famous tourist attraction of a 3 sqkm of rock formation, Duqm, Oman
A weathered wooden stake used as a bollard on the quay in the harbour in Boscastle, with a water covered rock face. Cornwall.England.UK Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-weathered-wooden-stake-used-as-a-bollard-on-the-quay-in-the-harbour-in-boscastle-with-a-water-covered-rock-face-cornwallenglanduk-image466267725.htmlRF2J2G96N–A weathered wooden stake used as a bollard on the quay in the harbour in Boscastle, with a water covered rock face. Cornwall.England.UK
Accumulation of fossilized paleofauna in limestone. Brachiopods, rugoses, segments of sea lilies, needles of sea urchins. Carboniferous period, Russia Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/accumulation-of-fossilized-paleofauna-in-limestone-brachiopods-rugoses-segments-of-sea-lilies-needles-of-sea-urchins-carboniferous-period-russia-image554183566.htmlRF2R5H6P6–Accumulation of fossilized paleofauna in limestone. Brachiopods, rugoses, segments of sea lilies, needles of sea urchins. Carboniferous period, Russia
Carved millstones Hathersage Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-carved-millstones-hathersage-17850401.htmlRFB114A9–Carved millstones Hathersage
Millstone located at the entrance to the Holodomor Monument and Museum dedicated to the 1932-1933 famine in Kiev, Ukraine Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-millstone-located-at-the-entrance-to-the-holodomor-monument-and-museum-33222269.htmlRMBX1B9H–Millstone located at the entrance to the Holodomor Monument and Museum dedicated to the 1932-1933 famine in Kiev, Ukraine
. Transactions. GENESIS OF THE ORE-DEPOSITS AT BINGHAM, UTAH. 561. Fig. 8.—Chalcopyrite Developing in Marmorized Silicified Limestone. (Sp. H. B. 29; Without Analyzer, x 48-f.) From No. 1 Ore-Body, No. 6 Level, Highland Boy Mine. Chalcopyrite (Ch) invading limestone metamorphosed to siliceous marble made up of granular calcite (C) and quartz (Q). Chalcopyrite replaces calcite and quartz. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/transactions-genesis-of-the-ore-deposits-at-bingham-utah-561-fig-8chalcopyrite-developing-in-marmorized-silicified-limestone-sp-h-b-29-without-analyzer-x-48-f-from-no-1-ore-body-no-6-level-highland-boy-mine-chalcopyrite-ch-invading-limestone-metamorphosed-to-siliceous-marble-made-up-of-granular-calcite-c-and-quartz-q-chalcopyrite-replaces-calcite-and-quartz-image337146613.htmlRM2AGE9XD–. Transactions. GENESIS OF THE ORE-DEPOSITS AT BINGHAM, UTAH. 561. Fig. 8.—Chalcopyrite Developing in Marmorized Silicified Limestone. (Sp. H. B. 29; Without Analyzer, x 48-f.) From No. 1 Ore-Body, No. 6 Level, Highland Boy Mine. Chalcopyrite (Ch) invading limestone metamorphosed to siliceous marble made up of granular calcite (C) and quartz (Q). Chalcopyrite replaces calcite and quartz.
Millstone of Alphonse Daudet's windmill in Fontvieille, France Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-millstone-of-alphonse-daudets-windmill-in-fontvieille-france-21934113.htmlRMB7K555–Millstone of Alphonse Daudet's windmill in Fontvieille, France
. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 233 EUOM. Jacksonville road, (D3, 161)—II h?—Also in cross road south of Bath and W. of K. R., rather abundant in quarry, of prob- ably Calciferous age (D3, 183)—IIa?—Similar forms were obtained from the same great limestone formation in Canoe Valley, Blair Co. (C. E. HalPs Rt. Proc. A. P. S., Jan. 5, m^.—IIa? II h? Euomphalus, Chemung forms in lower 500' of Randall's Warren Section (I, p. 54.)—VIIIg. Euomphalus, very minute, silicified in vast numbers, (with Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-dictionary-of-the-fossils-of-pennsylvania-and-neighboring-states-named-in-the-reports-and-catalogues-of-the-survey-paleontology-233-euom-jacksonville-road-d3-161ii-halso-in-cross-road-south-of-bath-and-w-of-k-r-rather-abundant-in-quarry-of-prob-ably-calciferous-age-d3-183iiasimilar-forms-were-obtained-from-the-same-great-limestone-formation-in-canoe-valley-blair-co-c-e-halps-rt-proc-a-p-s-jan-5-miia-ii-h-euomphalus-chemung-forms-in-lower-500-of-randalls-warren-section-i-p-54viiig-euomphalus-very-minute-silicified-in-vast-numbers-with-image216290963.htmlRMPFTW97–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 233 EUOM. Jacksonville road, (D3, 161)—II h?—Also in cross road south of Bath and W. of K. R., rather abundant in quarry, of prob- ably Calciferous age (D3, 183)—IIa?—Similar forms were obtained from the same great limestone formation in Canoe Valley, Blair Co. (C. E. HalPs Rt. Proc. A. P. S., Jan. 5, m^.—IIa? II h? Euomphalus, Chemung forms in lower 500' of Randall's Warren Section (I, p. 54.)—VIIIg. Euomphalus, very minute, silicified in vast numbers, (with
Tree growing in outcrop of banded Chert, part of the Carboniferous, Pentre Chert formation, Halkyn, Wales, UK, January. The Chert is silicified Limestone, made up in part of micro organism Radiolaria. This is one of the rock types that is targetted for 'Fracking' with gas contained within fractures. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/tree-growing-in-outcrop-of-banded-chert-part-of-the-carboniferous-pentre-chert-formation-halkyn-wales-uk-january-the-chert-is-silicified-limestone-made-up-in-part-of-micro-organism-radiolaria-this-is-one-of-the-rock-types-that-is-targetted-for-fracking-with-gas-contained-within-fractures-image612140347.htmlRM2XFWB77–Tree growing in outcrop of banded Chert, part of the Carboniferous, Pentre Chert formation, Halkyn, Wales, UK, January. The Chert is silicified Limestone, made up in part of micro organism Radiolaria. This is one of the rock types that is targetted for 'Fracking' with gas contained within fractures.
Rock Garden (Rock Zoo of Duqm or Duqm Stone Park) is a famous tourist attraction of 3 sqkm of rock formations limestone and marine fossils, Duqm, Oman Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-rock-garden-rock-zoo-of-duqm-or-duqm-stone-park-is-a-famous-tourist-172032473.htmlRMKYTN4W–Rock Garden (Rock Zoo of Duqm or Duqm Stone Park) is a famous tourist attraction of 3 sqkm of rock formations limestone and marine fossils, Duqm, Oman
Top of a weathered grey wooden stake used as a bollard on the quay in the harbour in Boscastle, with a water covered rock face. Cornwall.England.UK Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/top-of-a-weathered-grey-wooden-stake-used-as-a-bollard-on-the-quay-in-the-harbour-in-boscastle-with-a-water-covered-rock-face-cornwallenglanduk-image466267719.htmlRF2J2G96F–Top of a weathered grey wooden stake used as a bollard on the quay in the harbour in Boscastle, with a water covered rock face. Cornwall.England.UK
Accumulation of fossilized paleofauna in limestone. Brachiopods, rugoses, segments of sea lilies, needles of sea urchins. Carboniferous period, Russia Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/accumulation-of-fossilized-paleofauna-in-limestone-brachiopods-rugoses-segments-of-sea-lilies-needles-of-sea-urchins-carboniferous-period-russia-image554183554.htmlRF2R5H6NP–Accumulation of fossilized paleofauna in limestone. Brachiopods, rugoses, segments of sea lilies, needles of sea urchins. Carboniferous period, Russia
Carved millstones Hathersage, Derbyshire, UK Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-carved-millstones-hathersage-derbyshire-uk-18340506.htmlRFB1RDE2–Carved millstones Hathersage, Derbyshire, UK
The geology of Hardin County, and the adjoining part of Pope County . A. Veinlet of fluorite (P) containing later sulphides in silicified limestone(L). A transition zone into wall-rock material is indicated. The rock containsalso many specks, apparently of fluorite.. B. Section in a small veinlet cutting an argillaceous limestone wall-rock,showing relationships between wall-rock material (W), fluorite (F), galena (G),and chalcopyrite (Ch). The wall-rock contact with fluorite is very irregular andvague, and the fluorite mass contains many minute fragments besides the largerremnants indicated. I Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-geology-of-hardin-county-and-the-adjoining-part-of-pope-county-a-veinlet-of-fluorite-p-containing-later-sulphides-in-silicified-limestonel-a-transition-zone-into-wall-rock-material-is-indicated-the-rock-containsalso-many-specks-apparently-of-fluorite-b-section-in-a-small-veinlet-cutting-an-argillaceous-limestone-wall-rockshowing-relationships-between-wall-rock-material-w-fluorite-f-galena-gand-chalcopyrite-ch-the-wall-rock-contact-with-fluorite-is-very-irregular-andvague-and-the-fluorite-mass-contains-many-minute-fragments-besides-the-largerremnants-indicated-i-image338430415.htmlRM2AJGRCF–The geology of Hardin County, and the adjoining part of Pope County . A. Veinlet of fluorite (P) containing later sulphides in silicified limestone(L). A transition zone into wall-rock material is indicated. The rock containsalso many specks, apparently of fluorite.. B. Section in a small veinlet cutting an argillaceous limestone wall-rock,showing relationships between wall-rock material (W), fluorite (F), galena (G),and chalcopyrite (Ch). The wall-rock contact with fluorite is very irregular andvague, and the fluorite mass contains many minute fragments besides the largerremnants indicated. I
Millstone of Alphonse Daudet's windmill in Fontvieille, France Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-millstone-of-alphonse-daudets-windmill-in-fontvieille-france-22250137.htmlRMB85G7N–Millstone of Alphonse Daudet's windmill in Fontvieille, France
Water flows down the multi coloured cliffs which line the south of the harbour at Boscastle in Cornwall.The strata is the visible part of the geologic Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/water-flows-down-the-multi-coloured-cliffs-which-line-the-south-of-the-harbour-at-boscastle-in-cornwallthe-strata-is-the-visible-part-of-the-geologic-image466891183.htmlRF2J3GMD3–Water flows down the multi coloured cliffs which line the south of the harbour at Boscastle in Cornwall.The strata is the visible part of the geologic
Accumulation of fossilized paleofauna in limestone. Brachiopods, rugoses, segments of sea lilies, needles of sea urchins. Carboniferous period, Russia Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/accumulation-of-fossilized-paleofauna-in-limestone-brachiopods-rugoses-segments-of-sea-lilies-needles-of-sea-urchins-carboniferous-period-russia-image554183575.htmlRF2R5H6PF–Accumulation of fossilized paleofauna in limestone. Brachiopods, rugoses, segments of sea lilies, needles of sea urchins. Carboniferous period, Russia
Carved millstones Hathersage Hope Valley Derbyshire Peak District uk Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-carved-millstones-hathersage-hope-valley-derbyshire-peak-district-18340949.htmlRFB1RE1W–Carved millstones Hathersage Hope Valley Derbyshire Peak District uk
Hathersage Mill stones Peak District National Park, Derbyshire Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-hathersage-mill-stones-peak-district-national-park-derbyshire-21327036.htmlRFB6KERT–Hathersage Mill stones Peak District National Park, Derbyshire
. Transactions. Fig. 8.—Chalcopyrite Developing in Marmorized Silicified Limestone. (Sp. H. B. 29; Without Analyzer, x 48-f.) From No. 1 Ore-Body, No. 6 Level, Highland Boy Mine. Chalcopyrite (Ch) invading limestone metamorphosed to siliceous marble made up of granular calcite (C) and quartz (Q). Chalcopyrite replaces calcite and quartz.. Fig. 9.—Intergrowth of Chalcopyrite and Pyrite Keplacing Quartz.(Sp. No. 103*> ; Without Analyzer, x 48.) From No. 4 Level, High-land Boy Mine.The chalcopyrite and pyrite (Ch) encircle and replace the quartz (Q) of anentirely silicified limestone. This sec Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/transactions-fig-8chalcopyrite-developing-in-marmorized-silicified-limestone-sp-h-b-29-without-analyzer-x-48-f-from-no-1-ore-body-no-6-level-highland-boy-mine-chalcopyrite-ch-invading-limestone-metamorphosed-to-siliceous-marble-made-up-of-granular-calcite-c-and-quartz-q-chalcopyrite-replaces-calcite-and-quartz-fig-9intergrowth-of-chalcopyrite-and-pyrite-keplacing-quartzsp-no-103gt-without-analyzer-x-48-from-no-4-level-high-land-boy-minethe-chalcopyrite-and-pyrite-ch-encircle-and-replace-the-quartz-q-of-anentirely-silicified-limestone-this-sec-image337146012.htmlRM2AGE950–. Transactions. Fig. 8.—Chalcopyrite Developing in Marmorized Silicified Limestone. (Sp. H. B. 29; Without Analyzer, x 48-f.) From No. 1 Ore-Body, No. 6 Level, Highland Boy Mine. Chalcopyrite (Ch) invading limestone metamorphosed to siliceous marble made up of granular calcite (C) and quartz (Q). Chalcopyrite replaces calcite and quartz.. Fig. 9.—Intergrowth of Chalcopyrite and Pyrite Keplacing Quartz.(Sp. No. 103*> ; Without Analyzer, x 48.) From No. 4 Level, High-land Boy Mine.The chalcopyrite and pyrite (Ch) encircle and replace the quartz (Q) of anentirely silicified limestone. This sec
Water flows down a multi coloured pocket in the cliffs which line the south of the harbour at Boscastle in Cornwall.The strata is the visible part of Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/water-flows-down-a-multi-coloured-pocket-in-the-cliffs-which-line-the-south-of-the-harbour-at-boscastle-in-cornwallthe-strata-is-the-visible-part-of-image466891187.htmlRF2J3GMD7–Water flows down a multi coloured pocket in the cliffs which line the south of the harbour at Boscastle in Cornwall.The strata is the visible part of
Hathersage Mill stones Peak District National Park, Derbyshire Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-hathersage-mill-stones-peak-district-national-park-derbyshire-21319191.htmlRFB6K4RK–Hathersage Mill stones Peak District National Park, Derbyshire
. Transactions. Fig. 9.—Intergrowth of Chalcopyrite and Pyrite Keplacing Quartz.(Sp. No. 103*> ; Without Analyzer, x 48.) From No. 4 Level, High-land Boy Mine.The chalcopyrite and pyrite (Ch) encircle and replace the quartz (Q) of anentirely silicified limestone. This section from a specimen from an upper levelshows evidences of superficial alteration not apparent in the reproduction. Themargins of the sulphide are tarnished, showing peacock ore. 562 GENESIS OF THE ORE-DEPOSITS AT BINGHAM, UTAH. r ? v^l F m. Fig. 10.—Specularite Replacing Calcite. (Sp. No. 313 ; Without Ana-lyzer, x 66-f.) Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/transactions-fig-9intergrowth-of-chalcopyrite-and-pyrite-keplacing-quartzsp-no-103gt-without-analyzer-x-48-from-no-4-level-high-land-boy-minethe-chalcopyrite-and-pyrite-ch-encircle-and-replace-the-quartz-q-of-anentirely-silicified-limestone-this-section-from-a-specimen-from-an-upper-levelshows-evidences-of-superficial-alteration-not-apparent-in-the-reproduction-themargins-of-the-sulphide-are-tarnished-showing-peacock-ore-562-genesis-of-the-ore-deposits-at-bingham-utah-r-vl-f-m-fig-10specularite-replacing-calcite-sp-no-313-without-ana-lyzer-x-66-f-image337145835.htmlRM2AGE8XK–. Transactions. Fig. 9.—Intergrowth of Chalcopyrite and Pyrite Keplacing Quartz.(Sp. No. 103*> ; Without Analyzer, x 48.) From No. 4 Level, High-land Boy Mine.The chalcopyrite and pyrite (Ch) encircle and replace the quartz (Q) of anentirely silicified limestone. This section from a specimen from an upper levelshows evidences of superficial alteration not apparent in the reproduction. Themargins of the sulphide are tarnished, showing peacock ore. 562 GENESIS OF THE ORE-DEPOSITS AT BINGHAM, UTAH. r ? v^l F m. Fig. 10.—Specularite Replacing Calcite. (Sp. No. 313 ; Without Ana-lyzer, x 66-f.)
Hathersage Mill stones Peak District National Park, Derbyshire Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-hathersage-mill-stones-peak-district-national-park-derbyshire-21327113.htmlRFB6KEXH–Hathersage Mill stones Peak District National Park, Derbyshire
On the structure and affinities of the genus Monticulipora and its sub-genera, with critical descriptions of illustrative species . c I r )kO I C. Fig. 17.—A, Tangential section of a completely silicified speciiv.en of Fistulipora Canadensis,Bill., from the .Corniferous Limestone of Ontario, enlarged seven times; E, Verticalsection of the same specimen, similarly enlarged ; c, Tangential section of a calcareousspecimen oiFistulipora Canadensis, Bill., from the Hamilton Group of Ontario, enlargedseven times; D, Vertical section of tlie same specimen, showing mural pores, simi-larly enlarged. w Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/on-the-structure-and-affinities-of-the-genus-monticulipora-and-its-sub-genera-with-critical-descriptions-of-illustrative-species-c-i-r-ko-i-c-fig-17a-tangential-section-of-a-completely-silicified-speciiven-of-fistulipora-canadensisbill-from-the-corniferous-limestone-of-ontario-enlarged-seven-times-e-verticalsection-of-the-same-specimen-similarly-enlarged-c-tangential-section-of-a-calcareousspecimen-oifistulipora-canadensis-bill-from-the-hamilton-group-of-ontario-enlargedseven-times-d-vertical-section-of-tlie-same-specimen-showing-mural-pores-simi-larly-enlarged-w-image338933838.htmlRM2AKBNFX–On the structure and affinities of the genus Monticulipora and its sub-genera, with critical descriptions of illustrative species . c I r )kO I C. Fig. 17.—A, Tangential section of a completely silicified speciiv.en of Fistulipora Canadensis,Bill., from the .Corniferous Limestone of Ontario, enlarged seven times; E, Verticalsection of the same specimen, similarly enlarged ; c, Tangential section of a calcareousspecimen oiFistulipora Canadensis, Bill., from the Hamilton Group of Ontario, enlargedseven times; D, Vertical section of tlie same specimen, showing mural pores, simi-larly enlarged. w
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. Osteology of Haplocanthosaurus : with description of a new species, and remarks on the probable habits of the Sauropoda and the age and origin of the Atlantosaurus beds. LOCANTHOSAURUS H3 in a layer of arenaceous shales there occurs a bed of Unios fi-om which were obtainedmost of the species described by Dr. C. A. White as coming from this locality, whilethe shales underlying the thick stratum of sandstone seen at the top of the escarp-ment forming the canon wall just to the left and in front of the tent containsnumerous small lenses of impure limestone filled with the silicified remains off Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/osteology-of-haplocanthosaurus-with-description-of-a-new-species-and-remarks-on-the-probable-habits-of-the-sauropoda-and-the-age-and-origin-of-the-atlantosaurus-beds-locanthosaurus-h3-in-a-layer-of-arenaceous-shales-there-occurs-a-bed-of-unios-fi-om-which-were-obtainedmost-of-the-species-described-by-dr-c-a-white-as-coming-from-this-locality-whilethe-shales-underlying-the-thick-stratum-of-sandstone-seen-at-the-top-of-the-escarp-ment-forming-the-canon-wall-just-to-the-left-and-in-front-of-the-tent-containsnumerous-small-lenses-of-impure-limestone-filled-with-the-silicified-remains-off-image370490781.htmlRM2CEN8NH–. Osteology of Haplocanthosaurus : with description of a new species, and remarks on the probable habits of the Sauropoda and the age and origin of the Atlantosaurus beds. LOCANTHOSAURUS H3 in a layer of arenaceous shales there occurs a bed of Unios fi-om which were obtainedmost of the species described by Dr. C. A. White as coming from this locality, whilethe shales underlying the thick stratum of sandstone seen at the top of the escarp-ment forming the canon wall just to the left and in front of the tent containsnumerous small lenses of impure limestone filled with the silicified remains off
Hathersage Mill stones Peak District National Park, Derbyshire Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-hathersage-mill-stones-peak-district-national-park-derbyshire-21319195.htmlRFB6K4RR–Hathersage Mill stones Peak District National Park, Derbyshire
. Annals of the New York Academy of Sciences. Science. 48 ANNALS NEW YORK ACADEMY OF SCIENCES formations, essentially a silicified dune deposit such as that at San Juan^ also by Tertiary limestone reefs, such-as that at Quebradillas and at Guanica, or by the still older igneous and clastic series, such as that at Anasco, or by massive intrusives of a strictly igneous habit, such as that at Maunabo. It would appear from this that the former outline of the island must have been more irregiilar than it is at present and that the distribution of marginal formations is also not as regular as has be Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annals-of-the-new-york-academy-of-sciences-science-48-annals-new-york-academy-of-sciences-formations-essentially-a-silicified-dune-deposit-such-as-that-at-san-juan-also-by-tertiary-limestone-reefs-such-as-that-at-quebradillas-and-at-guanica-or-by-the-still-older-igneous-and-clastic-series-such-as-that-at-anasco-or-by-massive-intrusives-of-a-strictly-igneous-habit-such-as-that-at-maunabo-it-would-appear-from-this-that-the-former-outline-of-the-island-must-have-been-more-irregiilar-than-it-is-at-present-and-that-the-distribution-of-marginal-formations-is-also-not-as-regular-as-has-be-image236507676.htmlRMRMNRXM–. Annals of the New York Academy of Sciences. Science. 48 ANNALS NEW YORK ACADEMY OF SCIENCES formations, essentially a silicified dune deposit such as that at San Juan^ also by Tertiary limestone reefs, such-as that at Quebradillas and at Guanica, or by the still older igneous and clastic series, such as that at Anasco, or by massive intrusives of a strictly igneous habit, such as that at Maunabo. It would appear from this that the former outline of the island must have been more irregiilar than it is at present and that the distribution of marginal formations is also not as regular as has be
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Carved Millstone Wheel Hathersage, Peak District National Park, Derbyshire Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-carved-millstone-wheel-hathersage-peak-district-national-park-derbyshire-17850338.htmlRFB11482–Carved Millstone Wheel Hathersage, Peak District National Park, Derbyshire
Carved millstones Hathersage, Derbyshire, UK Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-carved-millstones-hathersage-derbyshire-uk-26811315.htmlRFBFHA2Y–Carved millstones Hathersage, Derbyshire, UK
. The Canadian naturalist and geologist. Natural history -- Periodicals. 188 THE CANADIAN NATURALIST. [June appearance of the endorhin of silicified specimens when cleared of the limestone matrix by treatment with acid. Although the pores have been seen in this species only, yet it seems quite probable that they occur in all others of the genus. In the diagram fig. 5 the tubes are placed proportionately much farther apart than they are in any known species, in order to ex- hibit the structure with the greater clearness. The endorhin is drawn as if it were transparent to show the position of th Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-canadian-naturalist-and-geologist-natural-history-periodicals-188-the-canadian-naturalist-june-appearance-of-the-endorhin-of-silicified-specimens-when-cleared-of-the-limestone-matrix-by-treatment-with-acid-although-the-pores-have-been-seen-in-this-species-only-yet-it-seems-quite-probable-that-they-occur-in-all-others-of-the-genus-in-the-diagram-fig-5-the-tubes-are-placed-proportionately-much-farther-apart-than-they-are-in-any-known-species-in-order-to-ex-hibit-the-structure-with-the-greater-clearness-the-endorhin-is-drawn-as-if-it-were-transparent-to-show-the-position-of-th-image233521476.htmlRMRFWR0M–. The Canadian naturalist and geologist. Natural history -- Periodicals. 188 THE CANADIAN NATURALIST. [June appearance of the endorhin of silicified specimens when cleared of the limestone matrix by treatment with acid. Although the pores have been seen in this species only, yet it seems quite probable that they occur in all others of the genus. In the diagram fig. 5 the tubes are placed proportionately much farther apart than they are in any known species, in order to ex- hibit the structure with the greater clearness. The endorhin is drawn as if it were transparent to show the position of th
Carved millstones Hathersage, Derbyshire, UK Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-carved-millstones-hathersage-derbyshire-uk-26811387.htmlRFBFHA5F–Carved millstones Hathersage, Derbyshire, UK
. Annals of the New York Academy of Sciences. Science. 66 ANNALS NEW YORK ACADEMY OF SCIENCES. Silicified specimens of Enterolasma strictum are very abundant in the New Scotland limestone, but they are not sufficiently well preserved to use in grinding, or in cutting sections. Numerous specimens of various sizes and ages have been carefully studied. The general manner of development is found to agree with that observed in the Ordovicic and Siluric corals. The septa unite at the center more distinctly than in any of the preceding species. The pseudocolumella thus formed is not exactly solid, bu Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annals-of-the-new-york-academy-of-sciences-science-66-annals-new-york-academy-of-sciences-silicified-specimens-of-enterolasma-strictum-are-very-abundant-in-the-new-scotland-limestone-but-they-are-not-sufficiently-well-preserved-to-use-in-grinding-or-in-cutting-sections-numerous-specimens-of-various-sizes-and-ages-have-been-carefully-studied-the-general-manner-of-development-is-found-to-agree-with-that-observed-in-the-ordovicic-and-siluric-corals-the-septa-unite-at-the-center-more-distinctly-than-in-any-of-the-preceding-species-the-pseudocolumella-thus-formed-is-not-exactly-solid-bu-image236534410.htmlRMRMR21E–. Annals of the New York Academy of Sciences. Science. 66 ANNALS NEW YORK ACADEMY OF SCIENCES. Silicified specimens of Enterolasma strictum are very abundant in the New Scotland limestone, but they are not sufficiently well preserved to use in grinding, or in cutting sections. Numerous specimens of various sizes and ages have been carefully studied. The general manner of development is found to agree with that observed in the Ordovicic and Siluric corals. The septa unite at the center more distinctly than in any of the preceding species. The pseudocolumella thus formed is not exactly solid, bu
![. Bulletins of American paleontology. . PLASTIC SCREEN FIG.I— LUCITE ETCHING TRAY Fig. 1. Sketch of a plexiglass and plastic screen acid-resisting etching rack for treatment of small, differentially silicified blocks of limestone.. 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.. Paleontological Research Institution (Ithaca, N. Y. ); Columbia University. Ithaca, N. Y. , Paleontological Research Institution [etc. ] Stock Photo](https://c8.alamy.com/comp/RG9WC0/bulletins-of-american-paleontology-plastic-screen-figi-lucite-etching-tray-fig-1-sketch-of-a-plexiglass-and-plastic-screen-acid-resisting-etching-rack-for-treatment-of-small-differentially-silicified-blocks-of-limestone-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-paleontological-research-institution-ithaca-n-y-columbia-university-ithaca-n-y-paleontological-research-institution-etc-RG9WC0.jpg ". Bulletins of American paleontology. . PLASTIC SCREEN FIG.I— LUCITE ETCHING TRAY Fig. 1. Sketch of a plexiglass and plastic screen acid-resisting etching rack for treatment of small, differentially silicified blocks of limestone.. 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.. Paleontological Research Institution (Ithaca, N. Y. ); Columbia University. Ithaca, N. Y. , Paleontological Research Institution [etc. ] Stock Photo")
. Bulletins of American paleontology. . PLASTIC SCREEN FIG.I— LUCITE ETCHING TRAY Fig. 1. Sketch of a plexiglass and plastic screen acid-resisting etching rack for treatment of small, differentially silicified blocks of limestone.. 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.. Paleontological Research Institution (Ithaca, N. Y. ); Columbia University. Ithaca, N. Y. , Paleontological Research Institution [etc. ] Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletins-of-american-paleontology-plastic-screen-figi-lucite-etching-tray-fig-1-sketch-of-a-plexiglass-and-plastic-screen-acid-resisting-etching-rack-for-treatment-of-small-differentially-silicified-blocks-of-limestone-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-paleontological-research-institution-ithaca-n-y-columbia-university-ithaca-n-y-paleontological-research-institution-etc-image233786784.htmlRMRG9WC0–. Bulletins of American paleontology. . PLASTIC SCREEN FIG.I— LUCITE ETCHING TRAY Fig. 1. Sketch of a plexiglass and plastic screen acid-resisting etching rack for treatment of small, differentially silicified blocks of limestone.. 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.. Paleontological Research Institution (Ithaca, N. Y. ); Columbia University. Ithaca, N. Y. , Paleontological Research Institution [etc. ]
. Bulletin of the Natural Histort Museum. Geology series. 162 S. 0.6. Carinal Ridge Autozooecial rows Median Ridge Fig. 103 Goniocladia cellidifera (Etheridge, 1873b). Graph of apertural spacing. vertical median wall from which autozooecia are budded; Fenestella and Pohpom have no such median wall. Autozooecia in these two genera are budded from a basal wall. Stratigraphical range. Lower Carboniferous. Distribution. British Isles. PALAEOECOLOGY OF THE COUNTY FERMANAGH BRYOZOAN FAUNA The silicified Visean fauna found towards the top of the Glencar Limestone has proved to be very diverse. It has Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-of-the-natural-histort-museum-geology-series-162-s-06-carinal-ridge-autozooecial-rows-median-ridge-fig-103-goniocladia-cellidifera-etheridge-1873b-graph-of-apertural-spacing-vertical-median-wall-from-which-autozooecia-are-budded-fenestella-and-pohpom-have-no-such-median-wall-autozooecia-in-these-two-genera-are-budded-from-a-basal-wall-stratigraphical-range-lower-carboniferous-distribution-british-isles-palaeoecology-of-the-county-fermanagh-bryozoan-fauna-the-silicified-visean-fauna-found-towards-the-top-of-the-glencar-limestone-has-proved-to-be-very-diverse-it-has-image233869698.htmlRMRGDK56–. Bulletin of the Natural Histort Museum. Geology series. 162 S. 0.6. Carinal Ridge Autozooecial rows Median Ridge Fig. 103 Goniocladia cellidifera (Etheridge, 1873b). Graph of apertural spacing. vertical median wall from which autozooecia are budded; Fenestella and Pohpom have no such median wall. Autozooecia in these two genera are budded from a basal wall. Stratigraphical range. Lower Carboniferous. Distribution. British Isles. PALAEOECOLOGY OF THE COUNTY FERMANAGH BRYOZOAN FAUNA The silicified Visean fauna found towards the top of the Glencar Limestone has proved to be very diverse. It has
. Annals of the New York Academy of Sciences. Science. 312 IRVING. depth. In the Doyle vertical lateral enrichments occur and also in the Metallic Streak Mine on the ridge south of Calam- ity Creek. The ore is essentially a silicified mass of brecciated limestone fragments, which are stained with iron oxide and which contain calcite in the lower grade ores. The general run of ore, how- ever, is hardly to be distinguished from the limestone except that'it is very slightly darker and is very hard, being an almost complete replacement of the limestone. Porphyry is not present in these verticals. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annals-of-the-new-york-academy-of-sciences-science-312-irving-depth-in-the-doyle-vertical-lateral-enrichments-occur-and-also-in-the-metallic-streak-mine-on-the-ridge-south-of-calam-ity-creek-the-ore-is-essentially-a-silicified-mass-of-brecciated-limestone-fragments-which-are-stained-with-iron-oxide-and-which-contain-calcite-in-the-lower-grade-ores-the-general-run-of-ore-how-ever-is-hardly-to-be-distinguished-from-the-limestone-except-thatit-is-very-slightly-darker-and-is-very-hard-being-an-almost-complete-replacement-of-the-limestone-porphyry-is-not-present-in-these-verticals-image236515499.htmlRMRMP5X3–. Annals of the New York Academy of Sciences. Science. 312 IRVING. depth. In the Doyle vertical lateral enrichments occur and also in the Metallic Streak Mine on the ridge south of Calam- ity Creek. The ore is essentially a silicified mass of brecciated limestone fragments, which are stained with iron oxide and which contain calcite in the lower grade ores. The general run of ore, how- ever, is hardly to be distinguished from the limestone except that'it is very slightly darker and is very hard, being an almost complete replacement of the limestone. Porphyry is not present in these verticals.
. The Canadian naturalist and geologist. Natural history -- Periodicals. 11.. 10. 10. R. Canadensis (Billings). 11. R. Iowensis (Owen). 12. R. Jonesii (Billings). I have not the least doubt, are the grooves of three of the stolons. The absence of the fourth stolon may be accounted for in this way. Among the detached silicified tubes of R. occidentalis which are found in the sediment left at the bottom of the vessel, after dissolving specimens of limestone holding these fossils in acid, numerous specimens have been collected with only three stolons in contact with the plate or at the end of the Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-canadian-naturalist-and-geologist-natural-history-periodicals-11-10-10-r-canadensis-billings-11-r-iowensis-owen-12-r-jonesii-billings-i-have-not-the-least-doubt-are-the-grooves-of-three-of-the-stolons-the-absence-of-the-fourth-stolon-may-be-accounted-for-in-this-way-among-the-detached-silicified-tubes-of-r-occidentalis-which-are-found-in-the-sediment-left-at-the-bottom-of-the-vessel-after-dissolving-specimens-of-limestone-holding-these-fossils-in-acid-numerous-specimens-have-been-collected-with-only-three-stolons-in-contact-with-the-plate-or-at-the-end-of-the-image233521437.htmlRMRFWPY9–. The Canadian naturalist and geologist. Natural history -- Periodicals. 11.. 10. 10. R. Canadensis (Billings). 11. R. Iowensis (Owen). 12. R. Jonesii (Billings). I have not the least doubt, are the grooves of three of the stolons. The absence of the fourth stolon may be accounted for in this way. Among the detached silicified tubes of R. occidentalis which are found in the sediment left at the bottom of the vessel, after dissolving specimens of limestone holding these fossils in acid, numerous specimens have been collected with only three stolons in contact with the plate or at the end of the
. British Antarctic expedition, 1907-9, under the command of E.H. Shackleton : reports on the scientific investigations ; geology. Scientific expeditions; Natural history; Geology; Paleontology; Petrology; Ice. No. 24-, 12 dianis Fig. 3 Erratic, tape Royds. Dolomitised and partially gilicified oolitic limestone.. No. 240. x 28 diams Fig. -t Erratic, (ape Royds. Dolomitised and partialh silicified oolitic limestone. [To face p. 200. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illu Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/british-antarctic-expedition-1907-9-under-the-command-of-eh-shackleton-reports-on-the-scientific-investigations-geology-scientific-expeditions-natural-history-geology-paleontology-petrology-ice-no-24-12-dianis-fig-3-erratic-tape-royds-dolomitised-and-partially-gilicified-oolitic-limestone-no-240-x-28-diams-fig-t-erratic-ape-royds-dolomitised-and-partialh-silicified-oolitic-limestone-to-face-p-200-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illu-image234268896.htmlRMRH3TA8–. British Antarctic expedition, 1907-9, under the command of E.H. Shackleton : reports on the scientific investigations ; geology. Scientific expeditions; Natural history; Geology; Paleontology; Petrology; Ice. No. 24-, 12 dianis Fig. 3 Erratic, tape Royds. Dolomitised and partially gilicified oolitic limestone.. No. 240. x 28 diams Fig. -t Erratic, (ape Royds. Dolomitised and partialh silicified oolitic limestone. [To face p. 200. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illu
. Annual report of the Regents. New York State Museum; Science. 144 NEW YORK STATE MUSEUM Distinguishing characters. Corallites in juxtaposition or separated by cellular interspaces; larg-e meshes of the network irregular, greatly varying in size; corallites oval in cross-section, united by their narrower sides; epitheca with fine lines of growth and occa- sionally strong wrinkles. Found in the Lockport limestone at Lockport (Hall), and Niagara. When silicified, the coral may be well preserved, but otherwise it is usually almost destroyed or replaced by various minerals. Genus heliolites Guett Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annual-report-of-the-regents-new-york-state-museum-science-144-new-york-state-museum-distinguishing-characters-corallites-in-juxtaposition-or-separated-by-cellular-interspaces-larg-e-meshes-of-the-network-irregular-greatly-varying-in-size-corallites-oval-in-cross-section-united-by-their-narrower-sides-epitheca-with-fine-lines-of-growth-and-occa-sionally-strong-wrinkles-found-in-the-lockport-limestone-at-lockport-hall-and-niagara-when-silicified-the-coral-may-be-well-preserved-but-otherwise-it-is-usually-almost-destroyed-or-replaced-by-various-minerals-genus-heliolites-guett-image236185397.htmlRMRM74TN–. Annual report of the Regents. New York State Museum; Science. 144 NEW YORK STATE MUSEUM Distinguishing characters. Corallites in juxtaposition or separated by cellular interspaces; larg-e meshes of the network irregular, greatly varying in size; corallites oval in cross-section, united by their narrower sides; epitheca with fine lines of growth and occa- sionally strong wrinkles. Found in the Lockport limestone at Lockport (Hall), and Niagara. When silicified, the coral may be well preserved, but otherwise it is usually almost destroyed or replaced by various minerals. Genus heliolites Guett
. British Antarctic expedition, 1907-9, under the command of E.H. Shackleton : reports on the scientific investigations ; geology. Scientific expeditions; Natural history; Geology; Paleontology; Petrology; Ice. 28 diams.. Fig. 1 Erratic, tape Royds. Etched with Hydrofluoric acid. Dolomitised and silicified oolitic limestone with banded agate structure in matrix. Fig. 2 Stranded Moraine, East Fork. Fenar Glacier. Dense limestone with volcanic fragments, quartz, and fresh sponge spicule. m c No. HIT. 28 diams. Please note that these images are extracted from scanned page images that may have bee Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/british-antarctic-expedition-1907-9-under-the-command-of-eh-shackleton-reports-on-the-scientific-investigations-geology-scientific-expeditions-natural-history-geology-paleontology-petrology-ice-28-diams-fig-1-erratic-tape-royds-etched-with-hydrofluoric-acid-dolomitised-and-silicified-oolitic-limestone-with-banded-agate-structure-in-matrix-fig-2-stranded-moraine-east-fork-fenar-glacier-dense-limestone-with-volcanic-fragments-quartz-and-fresh-sponge-spicule-m-c-no-hit-28-diams-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-bee-image234268874.htmlRMRH3T9E–. British Antarctic expedition, 1907-9, under the command of E.H. Shackleton : reports on the scientific investigations ; geology. Scientific expeditions; Natural history; Geology; Paleontology; Petrology; Ice. 28 diams.. Fig. 1 Erratic, tape Royds. Etched with Hydrofluoric acid. Dolomitised and silicified oolitic limestone with banded agate structure in matrix. Fig. 2 Stranded Moraine, East Fork. Fenar Glacier. Dense limestone with volcanic fragments, quartz, and fresh sponge spicule. m c No. HIT. 28 diams. Please note that these images are extracted from scanned page images that may have bee
. British Antarctic expedition, 1907-9, under the command of E.H. Shackleton : reports on the scientific investigations ; geology. Scientific expeditions; Natural history; Geology; Paleontology; Petrology; Ice. Fig. 1 Erratic, tape Royds. Etched with Hydrofluoric acid. Dolomitised and silicified oolitic limestone with banded agate structure in matrix. Fig. 2 Stranded Moraine, East Fork. Fenar Glacier. Dense limestone with volcanic fragments, quartz, and fresh sponge spicule. m c No. HIT. 28 diams. Nil 111? 90 diams. Fig. :! Farthest South. December 20, 1908. In siln Stained with Lemberg's solu Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/british-antarctic-expedition-1907-9-under-the-command-of-eh-shackleton-reports-on-the-scientific-investigations-geology-scientific-expeditions-natural-history-geology-paleontology-petrology-ice-fig-1-erratic-tape-royds-etched-with-hydrofluoric-acid-dolomitised-and-silicified-oolitic-limestone-with-banded-agate-structure-in-matrix-fig-2-stranded-moraine-east-fork-fenar-glacier-dense-limestone-with-volcanic-fragments-quartz-and-fresh-sponge-spicule-m-c-no-hit-28-diams-nil-111-90-diams-fig-!-farthest-south-december-20-1908-in-siln-stained-with-lembergs-solu-image234268862.htmlRMRH3T92–. British Antarctic expedition, 1907-9, under the command of E.H. Shackleton : reports on the scientific investigations ; geology. Scientific expeditions; Natural history; Geology; Paleontology; Petrology; Ice. Fig. 1 Erratic, tape Royds. Etched with Hydrofluoric acid. Dolomitised and silicified oolitic limestone with banded agate structure in matrix. Fig. 2 Stranded Moraine, East Fork. Fenar Glacier. Dense limestone with volcanic fragments, quartz, and fresh sponge spicule. m c No. HIT. 28 diams. Nil 111? 90 diams. Fig. :! Farthest South. December 20, 1908. In siln Stained with Lemberg's solu
. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 169 Oyat, Cyathophyllum dianthus, Goldfuss, Petref. 1826, p. 54, pi. 15, fig. 13 ; pi. 16, fig. 1. Hall, Geology of the Western District of New York, 1843, page 160, fig, 63,2. Tipper Ilelderbevg (Onond- aga) formation. (Murchison, SiL Research, page 690, pi. 16, figs. 12, 12a, 12 c.) Usually shows in large silicified bunches projecting from the weathered surfaces of the limestone rocks. The figure is a small portion of one of these masses of coral. Abundant Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-dictionary-of-the-fossils-of-pennsylvania-and-neighboring-states-named-in-the-reports-and-catalogues-of-the-survey-paleontology-169-oyat-cyathophyllum-dianthus-goldfuss-petref-1826-p-54-pi-15-fig-13-pi-16-fig-1-hall-geology-of-the-western-district-of-new-york-1843-page-160-fig-632-tipper-ilelderbevg-onond-aga-formation-murchison-sil-research-page-690-pi-16-figs-12-12a-12-c-usually-shows-in-large-silicified-bunches-projecting-from-the-weathered-surfaces-of-the-limestone-rocks-the-figure-is-a-small-portion-of-one-of-these-masses-of-coral-abundant-image231901749.htmlRMRD8119–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 169 Oyat, Cyathophyllum dianthus, Goldfuss, Petref. 1826, p. 54, pi. 15, fig. 13 ; pi. 16, fig. 1. Hall, Geology of the Western District of New York, 1843, page 160, fig, 63,2. Tipper Ilelderbevg (Onond- aga) formation. (Murchison, SiL Research, page 690, pi. 16, figs. 12, 12a, 12 c.) Usually shows in large silicified bunches projecting from the weathered surfaces of the limestone rocks. The figure is a small portion of one of these masses of coral. Abundant
. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 233 EUOM. Jacksonville road, (D3, 161)—II h?—Also in cross road south of Bath and W. of K. R., rather abundant in quarry, of prob- ably Calciferous age (D3, 183)—IIa?—Similar forms were obtained from the same great limestone formation in Canoe Valley, Blair Co. (C. E. HalPs Rt. Proc. A. P. S., Jan. 5, m^.—IIa? II h? Euomphalus, Chemung forms in lower 500' of Randall's Warren Section (I, p. 54.)—VIIIg. Euomphalus, very minute, silicified in vast numbers, (with Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/a-dictionary-of-the-fossils-of-pennsylvania-and-neighboring-states-named-in-the-reports-and-catalogues-of-the-survey-paleontology-233-euom-jacksonville-road-d3-161ii-halso-in-cross-road-south-of-bath-and-w-of-k-r-rather-abundant-in-quarry-of-prob-ably-calciferous-age-d3-183iiasimilar-forms-were-obtained-from-the-same-great-limestone-formation-in-canoe-valley-blair-co-c-e-halps-rt-proc-a-p-s-jan-5-miia-ii-h-euomphalus-chemung-forms-in-lower-500-of-randalls-warren-section-i-p-54viiig-euomphalus-very-minute-silicified-in-vast-numbers-with-image231926780.htmlRMRD94Y8–. A dictionary of the fossils of Pennsylvania and neighboring states named in the reports and catalogues of the survey ... Paleontology. 233 EUOM. Jacksonville road, (D3, 161)—II h?—Also in cross road south of Bath and W. of K. R., rather abundant in quarry, of prob- ably Calciferous age (D3, 183)—IIa?—Similar forms were obtained from the same great limestone formation in Canoe Valley, Blair Co. (C. E. HalPs Rt. Proc. A. P. S., Jan. 5, m^.—IIa? II h? Euomphalus, Chemung forms in lower 500' of Randall's Warren Section (I, p. 54.)—VIIIg. Euomphalus, very minute, silicified in vast numbers, (with
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