The Fifth Avenue Presbyterian Church in Manhattan, New York City, USA. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-fifth-avenue-presbyterian-church-in-manhattan-new-york-city-usa-image545222015.html
RM2PK106R–The Fifth Avenue Presbyterian Church in Manhattan, New York City, USA.
Old and new on 5th Avenue in Manhattan, New York. Fifth Avenue Presbyterian Church with skyscraper in the background. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/old-and-new-on-5th-avenue-in-manhattan-new-york-fifth-avenue-presbyterian-church-with-skyscraper-in-the-background-image244328641.html
RMT5E3JW–Old and new on 5th Avenue in Manhattan, New York. Fifth Avenue Presbyterian Church with skyscraper in the background.
Princeton University, Sayle Hall Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/princeton-university-sayle-hall-image401523359.html
RM2E96Y3Y–Princeton University, Sayle Hall
New Jersey, Double Page Sheet No. 5 Map of Southwestern Red Sandstone Cartographic. Atlases, Maps. 1884 - 1889. Lionel Pincus and Princess Firyal Map Division. New Jersey, Geology , New Jersey Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/new-jersey-double-page-sheet-no-5-map-of-southwestern-red-sandstone-cartographic-atlases-maps-1884-1889-lionel-pincus-and-princess-firyal-map-division-new-jersey-geology-new-jersey-image484293176.html
RM2K3WCTT–New Jersey, Double Page Sheet No. 5 Map of Southwestern Red Sandstone Cartographic. Atlases, Maps. 1884 - 1889. Lionel Pincus and Princess Firyal Map Division. New Jersey, Geology , New Jersey
History of the state of New York, for the use of common schools, academies, normal and high schools, and other seminaries of instruction . UCTION. 9 1 rocks older than the coal formation, and terminating in thelowest member of that deposit, near the Pennsylvania line.They consist of the imstratitied crystalline or primary, thestratified non-fossiliferons, and the older secondary fossiliferousrocks. Red sandstone occurs in the southern portions borderingon Xew Jersey; the great metamorphic belt passes along theeastern line ; granite, with abundance of iron ore and limestone,is found in the nort Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/history-of-the-state-of-new-york-for-the-use-of-common-schools-academies-normal-and-high-schools-and-other-seminaries-of-instruction-uction-9-1-rocks-older-than-the-coal-formation-and-terminating-in-thelowest-member-of-that-deposit-near-the-pennsylvania-linethey-consist-of-the-imstratitied-crystalline-or-primary-thestratified-non-fossiliferons-and-the-older-secondary-fossiliferousrocks-red-sandstone-occurs-in-the-southern-portions-borderingon-xew-jersey-the-great-metamorphic-belt-passes-along-theeastern-line-granite-with-abundance-of-iron-ore-and-limestoneis-found-in-the-nort-image339180601.html
RM2AKR08W–History of the state of New York, for the use of common schools, academies, normal and high schools, and other seminaries of instruction . UCTION. 9 1 rocks older than the coal formation, and terminating in thelowest member of that deposit, near the Pennsylvania line.They consist of the imstratitied crystalline or primary, thestratified non-fossiliferons, and the older secondary fossiliferousrocks. Red sandstone occurs in the southern portions borderingon Xew Jersey; the great metamorphic belt passes along theeastern line ; granite, with abundance of iron ore and limestone,is found in the nort
The Fifth Avenue Presbyterian Church in Manhattan, New York City, USA. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-fifth-avenue-presbyterian-church-in-manhattan-new-york-city-usa-image545222016.html
RM2PK106T–The Fifth Avenue Presbyterian Church in Manhattan, New York City, USA.
Old and new on 5th Avenue in Manhattan, New York. Fifth Avenue Presbyterian Church with skyscraper in the background. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/old-and-new-on-5th-avenue-in-manhattan-new-york-fifth-avenue-presbyterian-church-with-skyscraper-in-the-background-image244328631.html
RMT5E3JF–Old and new on 5th Avenue in Manhattan, New York. Fifth Avenue Presbyterian Church with skyscraper in the background.
Princeton University, Sayle Hall Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/princeton-university-sayle-hall-image401523362.html
RM2E96Y42–Princeton University, Sayle Hall
New Jersey, Double Page Sheet No. 6 Map of Central Red Sandstone Cartographic. Atlases, Maps. 1884 - 1889. Lionel Pincus and Princess Firyal Map Division. New Jersey, Geology , New Jersey Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/new-jersey-double-page-sheet-no-6-map-of-central-red-sandstone-cartographic-atlases-maps-1884-1889-lionel-pincus-and-princess-firyal-map-division-new-jersey-geology-new-jersey-image484294192.html
RM2K3WE54–New Jersey, Double Page Sheet No. 6 Map of Central Red Sandstone Cartographic. Atlases, Maps. 1884 - 1889. Lionel Pincus and Princess Firyal Map Division. New Jersey, Geology , New Jersey
. Historical collections of the state of New Jersey: past and present:. udson railroad, IGj miles inlength, commences at Jersey city, enters the county on the south-east, and terminates at Paterson, It will eventually be extendedinto the state of New York, and connect with the New York andErie railroad. The Morris canal, also, passes through the south-ern part of the county. In the northern part are large deposits ofvaluable iron ore, extensively used in the numerous ibrges of thatregion. There is an excellent quarry of red sandstone at the vil-lage of Little Falls. This county, although respe Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/historical-collections-of-the-state-of-new-jersey-past-and-present-udson-railroad-igj-miles-inlength-commences-at-jersey-city-enters-the-county-on-the-south-east-and-terminates-at-paterson-it-will-eventually-be-extendedinto-the-state-of-new-york-and-connect-with-the-new-york-anderie-railroad-the-morris-canal-also-passes-through-the-south-ern-part-of-the-county-in-the-northern-part-are-large-deposits-ofvaluable-iron-ore-extensively-used-in-the-numerous-ibrges-of-thatregion-there-is-an-excellent-quarry-of-red-sandstone-at-the-vil-lage-of-little-falls-this-county-although-respe-image336649406.html
RM2AFKKN2–. Historical collections of the state of New Jersey: past and present:. udson railroad, IGj miles inlength, commences at Jersey city, enters the county on the south-east, and terminates at Paterson, It will eventually be extendedinto the state of New York, and connect with the New York andErie railroad. The Morris canal, also, passes through the south-ern part of the county. In the northern part are large deposits ofvaluable iron ore, extensively used in the numerous ibrges of thatregion. There is an excellent quarry of red sandstone at the vil-lage of Little Falls. This county, although respe
The Fifth Avenue Presbyterian Church in Manhattan, New York City, USA. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-fifth-avenue-presbyterian-church-in-manhattan-new-york-city-usa-image545222055.html
RM2PK1087–The Fifth Avenue Presbyterian Church in Manhattan, New York City, USA.
Old and new on 5th Avenue in Manhattan, New York. Fifth Avenue Presbyterian Church with skyscraper in the background. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/old-and-new-on-5th-avenue-in-manhattan-new-york-fifth-avenue-presbyterian-church-with-skyscraper-in-the-background-image244328655.html
RMT5E3KB–Old and new on 5th Avenue in Manhattan, New York. Fifth Avenue Presbyterian Church with skyscraper in the background.
Princeton University, Sayle Hall Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/princeton-university-sayle-hall-image401523364.html
RM2E96Y44–Princeton University, Sayle Hall
New Jersey, Double Page Sheet No. 7 Map of Northeastern Red Sandstone Cartographic. Atlases, Maps. 1884 - 1889. Lionel Pincus and Princess Firyal Map Division. New Jersey, Geology , New Jersey Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/new-jersey-double-page-sheet-no-7-map-of-northeastern-red-sandstone-cartographic-atlases-maps-1884-1889-lionel-pincus-and-princess-firyal-map-division-new-jersey-geology-new-jersey-image484289923.html
RM2K3W8MK–New Jersey, Double Page Sheet No. 7 Map of Northeastern Red Sandstone Cartographic. Atlases, Maps. 1884 - 1889. Lionel Pincus and Princess Firyal Map Division. New Jersey, Geology , New Jersey
History of Union and Middlesex Counties, New Jersey with Biographical Sketches of many of their Prominent Men . changes somewhat to a gravelly loam on the bor-ders of Clark and Cranford townships. There aremany large drift bowlders deposited all along theSpringfield road in the valley of the Blue Hills, andwhen broken up are in demand for building purposes.They are mostly a granite intermixed with horn-blende and the red sandstone. This township is wellwatered, and has many facilities for manufacturing. Organization.—Westfield frontier included in 1699all back of the Elizabethtown borough, bei Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/history-of-union-and-middlesex-counties-new-jersey-with-biographical-sketches-of-many-of-their-prominent-men-changes-somewhat-to-a-gravelly-loam-on-the-bor-ders-of-clark-and-cranford-townships-there-aremany-large-drift-bowlders-deposited-all-along-thespringfield-road-in-the-valley-of-the-blue-hills-andwhen-broken-up-are-in-demand-for-building-purposesthey-are-mostly-a-granite-intermixed-with-horn-blende-and-the-red-sandstone-this-township-is-wellwatered-and-has-many-facilities-for-manufacturing-organizationwestfield-frontier-included-in-1699all-back-of-the-elizabethtown-borough-bei-image342816699.html
RM2AWMJ5F–History of Union and Middlesex Counties, New Jersey with Biographical Sketches of many of their Prominent Men . changes somewhat to a gravelly loam on the bor-ders of Clark and Cranford townships. There aremany large drift bowlders deposited all along theSpringfield road in the valley of the Blue Hills, andwhen broken up are in demand for building purposes.They are mostly a granite intermixed with horn-blende and the red sandstone. This township is wellwatered, and has many facilities for manufacturing. Organization.—Westfield frontier included in 1699all back of the Elizabethtown borough, bei
The Fifth Avenue Presbyterian Church in Manhattan, New York City, USA. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-fifth-avenue-presbyterian-church-in-manhattan-new-york-city-usa-image545222051.html
RM2PK1083–The Fifth Avenue Presbyterian Church in Manhattan, New York City, USA.
Old and new on 5th Avenue in Manhattan, New York, USA. Fifth Avenue Presbyterian Church with skyscraper in the background. Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/old-and-new-on-5th-avenue-in-manhattan-new-york-usa-fifth-avenue-presbyterian-church-with-skyscraper-in-the-background-image244328620.html
RMT5E3J4–Old and new on 5th Avenue in Manhattan, New York, USA. Fifth Avenue Presbyterian Church with skyscraper in the background.
Princeton University, Sayle Hall Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/princeton-university-sayle-hall-image401523389.html
RM2E96Y51–Princeton University, Sayle Hall
. Annual report of the Board of Regents of the Smithsonian Institution. Smithsonian Institution; Smithsonian Institution. Archives; Discoveries in science. AMERICAN GEOLOGY EATONIAN ERA. 1820-1829. 275 He remarked on the disappearance of the primitive rocks soon after leaving1 Philadelphia and the appearance of the transition limestone, ^J-. with occasional protrnsions through this limestone of amphibolite. He also made reference to the red sandstone of Pennsylvania, New Jersey, and Maryland and the calcareous breccia found on the Potomac. Please note that these images are extracted from scan Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/annual-report-of-the-board-of-regents-of-the-smithsonian-institution-smithsonian-institution-smithsonian-institution-archives-discoveries-in-science-american-geology-eatonian-era-1820-1829-275-he-remarked-on-the-disappearance-of-the-primitive-rocks-soon-after-leaving1-philadelphia-and-the-appearance-of-the-transition-limestone-j-with-occasional-protrnsions-through-this-limestone-of-amphibolite-he-also-made-reference-to-the-red-sandstone-of-pennsylvania-new-jersey-and-maryland-and-the-calcareous-breccia-found-on-the-potomac-please-note-that-these-images-are-extracted-from-scan-image236108430.html
RMRM3JKX–. Annual report of the Board of Regents of the Smithsonian Institution. Smithsonian Institution; Smithsonian Institution. Archives; Discoveries in science. AMERICAN GEOLOGY EATONIAN ERA. 1820-1829. 275 He remarked on the disappearance of the primitive rocks soon after leaving1 Philadelphia and the appearance of the transition limestone, ^J-. with occasional protrnsions through this limestone of amphibolite. He also made reference to the red sandstone of Pennsylvania, New Jersey, and Maryland and the calcareous breccia found on the Potomac. Please note that these images are extracted from scan
The Peninsula New York Hotel and Fifth Avenue Presbyterian Church on 5th Ave in New York City, USA Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/the-peninsula-new-york-hotel-and-fifth-avenue-presbyterian-church-on-5th-ave-in-new-york-city-usa-image244328608.html
RMT5E3HM–The Peninsula New York Hotel and Fifth Avenue Presbyterian Church on 5th Ave in New York City, USA
Princeton University, Sayle Hall Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/princeton-university-sayle-hall-image401523387.html
RM2E96Y4Y–Princeton University, Sayle Hall
. A brief general account of fossil fishes : the Triassic fishes of New Jersey. Fishes, Fossil; Paleontology. 40 ANNUAL REPORT OF has less resemblance than any other fossil of the Old Red Sand- stone to< anything that now exists. When first brought to view by the single blow of a hammer, there appeared on a ground of light-colored limestone [i. e., sandstone], the effigy of a creature, fashioned apparently out of jet, with a body covered with plates, two powerful-looking arms articulated at the shoulders, a head as entirely lost in the trunk as that of the ray (or skate), and a long angular Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/a-brief-general-account-of-fossil-fishes-the-triassic-fishes-of-new-jersey-fishes-fossil-paleontology-40-annual-report-of-has-less-resemblance-than-any-other-fossil-of-the-old-red-sand-stone-tolt-anything-that-now-exists-when-first-brought-to-view-by-the-single-blow-of-a-hammer-there-appeared-on-a-ground-of-light-colored-limestone-i-e-sandstone-the-effigy-of-a-creature-fashioned-apparently-out-of-jet-with-a-body-covered-with-plates-two-powerful-looking-arms-articulated-at-the-shoulders-a-head-as-entirely-lost-in-the-trunk-as-that-of-the-ray-or-skate-and-a-long-angular-image234277362.html
RMRH474J–. A brief general account of fossil fishes : the Triassic fishes of New Jersey. Fishes, Fossil; Paleontology. 40 ANNUAL REPORT OF has less resemblance than any other fossil of the Old Red Sand- stone to< anything that now exists. When first brought to view by the single blow of a hammer, there appeared on a ground of light-colored limestone [i. e., sandstone], the effigy of a creature, fashioned apparently out of jet, with a body covered with plates, two powerful-looking arms articulated at the shoulders, a head as entirely lost in the trunk as that of the ray (or skate), and a long angular
. A brief general account of fossil fishes : the Triassic fishes of New Jersey. Fishes, Fossil; Paleontology. 42 ANNUAL REPORT OF. Fig. 4. Coccosteus decipiens Ag. Lower Old Red Sandstone; Scotland. Lateral aspect, restored by Dr. R. H. Traquair. X JA- hugest of all Palaeozoic fishes, Dinichthys and Titanichthys, which occur in the uppermost Devonian of Ohio and neighboring States. The length of these creatures has been estimated at upwards of fifteen or twenty feet, and the solidity of their armor- plating has never been surpassed amongst fishes. Over the back and head the bones were in place Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/a-brief-general-account-of-fossil-fishes-the-triassic-fishes-of-new-jersey-fishes-fossil-paleontology-42-annual-report-of-fig-4-coccosteus-decipiens-ag-lower-old-red-sandstone-scotland-lateral-aspect-restored-by-dr-r-h-traquair-x-ja-hugest-of-all-palaeozoic-fishes-dinichthys-and-titanichthys-which-occur-in-the-uppermost-devonian-of-ohio-and-neighboring-states-the-length-of-these-creatures-has-been-estimated-at-upwards-of-fifteen-or-twenty-feet-and-the-solidity-of-their-armor-plating-has-never-been-surpassed-amongst-fishes-over-the-back-and-head-the-bones-were-in-place-image234277324.html
RMRH4738–. A brief general account of fossil fishes : the Triassic fishes of New Jersey. Fishes, Fossil; Paleontology. 42 ANNUAL REPORT OF. Fig. 4. Coccosteus decipiens Ag. Lower Old Red Sandstone; Scotland. Lateral aspect, restored by Dr. R. H. Traquair. X JA- hugest of all Palaeozoic fishes, Dinichthys and Titanichthys, which occur in the uppermost Devonian of Ohio and neighboring States. The length of these creatures has been estimated at upwards of fifteen or twenty feet, and the solidity of their armor- plating has never been surpassed amongst fishes. Over the back and head the bones were in place
. A brief general account of fossil fishes : the Triassic fishes of New Jersey. Fishes, Fossil; Paleontology. 52 ANNUAL REPORT OF lump of clay perforated by several round holes. On the rising of the water at the next rainy season the Lepidosiren pushes out the plug and soon emerges from its burrow. The breeding season begins soon after the escape of the fish.". Fig. 7. Dipterus valenciennesi Sedgw. and Murch. Lower Old Red Sandstone; Scotland. Lateral aspect, restored. X 3A- (From Dean.). Please note that these images are extracted from scanned page images that may have been digitally enh Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/a-brief-general-account-of-fossil-fishes-the-triassic-fishes-of-new-jersey-fishes-fossil-paleontology-52-annual-report-of-lump-of-clay-perforated-by-several-round-holes-on-the-rising-of-the-water-at-the-next-rainy-season-the-lepidosiren-pushes-out-the-plug-and-soon-emerges-from-its-burrow-the-breeding-season-begins-soon-after-the-escape-of-the-fishquot-fig-7-dipterus-valenciennesi-sedgw-and-murch-lower-old-red-sandstone-scotland-lateral-aspect-restored-x-3a-from-dean-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enh-image234277283.html
RMRH471R–. A brief general account of fossil fishes : the Triassic fishes of New Jersey. Fishes, Fossil; Paleontology. 52 ANNUAL REPORT OF lump of clay perforated by several round holes. On the rising of the water at the next rainy season the Lepidosiren pushes out the plug and soon emerges from its burrow. The breeding season begins soon after the escape of the fish.". Fig. 7. Dipterus valenciennesi Sedgw. and Murch. Lower Old Red Sandstone; Scotland. Lateral aspect, restored. X 3A- (From Dean.). Please note that these images are extracted from scanned page images that may have been digitally enh
. A brief general account of fossil fishes : the Triassic fishes of New Jersey. Fishes, Fossil; Paleontology. Pig. 2. Cephalaspis murchisoni Egert. Silurian and Lower Devonian; Hereford- shire. Lateral aspect, restored by Dr. A. S. Woodward. X %•. Fig- 3- Pteraspis rosirata Ag. Lower Old Red Sandstone; Great Britain, view of partially restored fish. X ZA- Side TremataspiSj together with the remarkable forms described with- in recent years from the Scottish Silurian, grouped by Dr. Tra- quair under the name of Anaspida. Of the above mentioned forms, only the genus Cephalaspis appears to have be Stock Photohttps://www.alamy.com/licenses-and-pricing/?v=1https://www.alamy.com/a-brief-general-account-of-fossil-fishes-the-triassic-fishes-of-new-jersey-fishes-fossil-paleontology-pig-2-cephalaspis-murchisoni-egert-silurian-and-lower-devonian-hereford-shire-lateral-aspect-restored-by-dr-a-s-woodward-x-fig-3-pteraspis-rosirata-ag-lower-old-red-sandstone-great-britain-view-of-partially-restored-fish-x-za-side-tremataspisj-together-with-the-remarkable-forms-described-with-in-recent-years-from-the-scottish-silurian-grouped-by-dr-tra-quair-under-the-name-of-anaspida-of-the-above-mentioned-forms-only-the-genus-cephalaspis-appears-to-have-be-image234277338.html
RMRH473P–. A brief general account of fossil fishes : the Triassic fishes of New Jersey. Fishes, Fossil; Paleontology. Pig. 2. Cephalaspis murchisoni Egert. Silurian and Lower Devonian; Hereford- shire. Lateral aspect, restored by Dr. A. S. Woodward. X %•. Fig- 3- Pteraspis rosirata Ag. Lower Old Red Sandstone; Great Britain, view of partially restored fish. X ZA- Side TremataspiSj together with the remarkable forms described with- in recent years from the Scottish Silurian, grouped by Dr. Tra- quair under the name of Anaspida. Of the above mentioned forms, only the genus Cephalaspis appears to have be
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