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Paleolithic era. Archeological Site of Atapuerca. 'Railway Trench' (Trinchera del Ferrocarril) where various fossil sediments were discovered. Topographic and stratigraphic marks. Excavation square technique and archaeological test pits. Province of Burgos, Castile and Leon, Spain. Unesco World Heritage Site. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/paleolithic-era-archeological-site-of-atapuerca-railway-trench-trinchera-del-ferrocarril-where-various-fossil-sediments-were-discovered-topographic-and-stratigraphic-marks-excavation-square-technique-and-archaeological-test-pits-province-of-burgos-castile-and-leon-spain-unesco-world-heritage-site-image187020114.htmlRMMT7E1P–Paleolithic era. Archeological Site of Atapuerca. 'Railway Trench' (Trinchera del Ferrocarril) where various fossil sediments were discovered. Topographic and stratigraphic marks. Excavation square technique and archaeological test pits. Province of Burgos, Castile and Leon, Spain. Unesco World Heritage Site.
Paleolithic era. Archeological Site of Atapuerca. 'Railway Trench' (Trinchera del Ferrocarril) where various fossil sediments were discovered. Topographic and stratigraphic marks. Excavation square technique and archaeological test pits. Province of Burgos, Castile and Leon, Spain. Unesco World Heritage Site. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/paleolithic-era-archeological-site-of-atapuerca-railway-trench-trinchera-del-ferrocarril-where-various-fossil-sediments-were-discovered-topographic-and-stratigraphic-marks-excavation-square-technique-and-archaeological-test-pits-province-of-burgos-castile-and-leon-spain-unesco-world-heritage-site-image231217568.htmlRMRC4TA8–Paleolithic era. Archeological Site of Atapuerca. 'Railway Trench' (Trinchera del Ferrocarril) where various fossil sediments were discovered. Topographic and stratigraphic marks. Excavation square technique and archaeological test pits. Province of Burgos, Castile and Leon, Spain. Unesco World Heritage Site.
![. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 04 THE CAUDONIFEROUS. in the labyrlnthudonts of the Carboaifeious. On aiiotlier slab there seems to have been a soft place where the legs of the anunal have sunk deeply into the mud; and it would appear to have been mired, extricating itself with some ditliculty, and leaving deep marks of the body and legs. These footprints must have been made on a subacri Stock Photo](https://c8.alamy.com/comp/RJ48JJ/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-04-the-caudoniferous-in-the-labyrlnthudonts-of-the-carboaifeious-on-aiiotlier-slab-there-seems-to-have-been-a-soft-place-where-the-legs-of-the-anunal-have-sunk-deeply-into-the-mud-and-it-would-appear-to-have-been-mired-extricating-itself-with-some-ditliculty-and-leaving-deep-marks-of-the-body-and-legs-these-footprints-must-have-been-made-on-a-subacri-RJ48JJ.jpg ". The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 04 THE CAUDONIFEROUS. in the labyrlnthudonts of the Carboaifeious. On aiiotlier slab there seems to have been a soft place where the legs of the anunal have sunk deeply into the mud; and it would appear to have been mired, extricating itself with some ditliculty, and leaving deep marks of the body and legs. These footprints must have been made on a subacri Stock Photo")
. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 04 THE CAUDONIFEROUS. in the labyrlnthudonts of the Carboaifeious. On aiiotlier slab there seems to have been a soft place where the legs of the anunal have sunk deeply into the mud; and it would appear to have been mired, extricating itself with some ditliculty, and leaving deep marks of the body and legs. These footprints must have been made on a subacri Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-04-the-caudoniferous-in-the-labyrlnthudonts-of-the-carboaifeious-on-aiiotlier-slab-there-seems-to-have-been-a-soft-place-where-the-legs-of-the-anunal-have-sunk-deeply-into-the-mud-and-it-would-appear-to-have-been-mired-extricating-itself-with-some-ditliculty-and-leaving-deep-marks-of-the-body-and-legs-these-footprints-must-have-been-made-on-a-subacri-image234893194.htmlRMRJ48JJ–. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 04 THE CAUDONIFEROUS. in the labyrlnthudonts of the Carboaifeious. On aiiotlier slab there seems to have been a soft place where the legs of the anunal have sunk deeply into the mud; and it would appear to have been mired, extricating itself with some ditliculty, and leaving deep marks of the body and legs. These footprints must have been made on a subacri
![. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 600 THE UPPER SILURIAN.. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, an Stock Photo](https://c8.alamy.com/comp/RJ5KEB/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-600-the-upper-silurian-i-the-trenton-limestone-but-a-careful-comparison-shows-it-to-be-wider-and-more-abrupt-at-its-posterior-termination-while-the-direction-of-the-striae-of-growth-is-very-distinctive-these-marks-being-regularly-curving-toward-the-posterior-end-in-m-nasutus-while-in-this-species-they-are-abruptly-bent-at-the-postero-basal-angle-an-RJ5KEB.jpg ". The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 600 THE UPPER SILURIAN.. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, an Stock Photo")
. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 600 THE UPPER SILURIAN.. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, an Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-600-the-upper-silurian-i-the-trenton-limestone-but-a-careful-comparison-shows-it-to-be-wider-and-more-abrupt-at-its-posterior-termination-while-the-direction-of-the-striae-of-growth-is-very-distinctive-these-marks-being-regularly-curving-toward-the-posterior-end-in-m-nasutus-while-in-this-species-they-are-abruptly-bent-at-the-postero-basal-angle-an-image234923651.htmlRMRJ5KEB–. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 600 THE UPPER SILURIAN.. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, an
. The earth in past ages. Geology, Stratigraphic; Earth sciences. THE MATERIALS OF STRATA. 47 served at Shell Ness which makes the eastern end of the Isle of Sheppey. Parts of the forest mar- ble in Oxfordshire, consist of accumulated growths of shells; and in Gloucestershire portions of the same deposit show ripple marks which indicate shallow conditions of deposition. Coral reefs are also to be classed as shallow- water limestones since the coral grows most vigor- sly where the water is aerated by the movement of the wav^ near to the surface of the sea. The. Fig. 7.—Carboniferous limestone, Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-earth-in-past-ages-geology-stratigraphic-earth-sciences-the-materials-of-strata-47-served-at-shell-ness-which-makes-the-eastern-end-of-the-isle-of-sheppey-parts-of-the-forest-mar-ble-in-oxfordshire-consist-of-accumulated-growths-of-shells-and-in-gloucestershire-portions-of-the-same-deposit-show-ripple-marks-which-indicate-shallow-conditions-of-deposition-coral-reefs-are-also-to-be-classed-as-shallow-water-limestones-since-the-coral-grows-most-vigor-sly-where-the-water-is-aerated-by-the-movement-of-the-wav-near-to-the-surface-of-the-sea-the-fig-7carboniferous-limestone-image232526924.htmlRMRE8ED0–. The earth in past ages. Geology, Stratigraphic; Earth sciences. THE MATERIALS OF STRATA. 47 served at Shell Ness which makes the eastern end of the Isle of Sheppey. Parts of the forest mar- ble in Oxfordshire, consist of accumulated growths of shells; and in Gloucestershire portions of the same deposit show ripple marks which indicate shallow conditions of deposition. Coral reefs are also to be classed as shallow- water limestones since the coral grows most vigor- sly where the water is aerated by the movement of the wav^ near to the surface of the sea. The. Fig. 7.—Carboniferous limestone,
![. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, and again on the cardinal s Stock Photo](https://c8.alamy.com/comp/RJ5KE4/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-i-the-trenton-limestone-but-a-careful-comparison-shows-it-to-be-wider-and-more-abrupt-at-its-posterior-termination-while-the-direction-of-the-striae-of-growth-is-very-distinctive-these-marks-being-regularly-curving-toward-the-posterior-end-in-m-nasutus-while-in-this-species-they-are-abruptly-bent-at-the-postero-basal-angle-and-again-on-the-cardinal-s-RJ5KE4.jpg ". The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, and again on the cardinal s Stock Photo")
. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, and again on the cardinal s Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-i-the-trenton-limestone-but-a-careful-comparison-shows-it-to-be-wider-and-more-abrupt-at-its-posterior-termination-while-the-direction-of-the-striae-of-growth-is-very-distinctive-these-marks-being-regularly-curving-toward-the-posterior-end-in-m-nasutus-while-in-this-species-they-are-abruptly-bent-at-the-postero-basal-angle-and-again-on-the-cardinal-s-image234923644.htmlRMRJ5KE4–. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. I the Trenton limestone, but a careful comparison shows it to be wider and more abrupt at its posterior termination, while the direction of the striae of growth is very distinctive, these marks being regularly curving toward the posterior end in M. nasutus, while in this species they are abruptly bent at the postero-basal angle, and again on the cardinal s
![. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 356 THE CAnnoNIFKKOUS SYSTEM. a plantigmdu nppcnranco to tho trackri. liaiii-marks had boon im- pressed on tlio Btirfaco after tho animal had passed over it, and those had probably aided in obliterating tho finer parts of tho impressions. These observations were ])ublished in the Journal of the Geological Society of London, vols. 1 and 2. Shortly afterward Stock Photo](https://c8.alamy.com/comp/RJ4M9G/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-356-the-cannonifkkous-system-a-plantigmdu-nppcnranco-to-tho-trackri-liaiii-marks-had-boon-im-pressed-on-tlio-btirfaco-after-tho-animal-had-passed-over-it-and-those-had-probably-aided-in-obliterating-tho-finer-parts-of-tho-impressions-these-observations-were-ublished-in-the-journal-of-the-geological-society-of-london-vols-1-and-2-shortly-afterward-RJ4M9G.jpg ". The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 356 THE CAnnoNIFKKOUS SYSTEM. a plantigmdu nppcnranco to tho trackri. liaiii-marks had boon im- pressed on tlio Btirfaco after tho animal had passed over it, and those had probably aided in obliterating tho finer parts of tho impressions. These observations were ])ublished in the Journal of the Geological Society of London, vols. 1 and 2. Shortly afterward Stock Photo")
. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 356 THE CAnnoNIFKKOUS SYSTEM. a plantigmdu nppcnranco to tho trackri. liaiii-marks had boon im- pressed on tlio Btirfaco after tho animal had passed over it, and those had probably aided in obliterating tho finer parts of tho impressions. These observations were ])ublished in the Journal of the Geological Society of London, vols. 1 and 2. Shortly afterward Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-356-the-cannonifkkous-system-a-plantigmdu-nppcnranco-to-tho-trackri-liaiii-marks-had-boon-im-pressed-on-tlio-btirfaco-after-tho-animal-had-passed-over-it-and-those-had-probably-aided-in-obliterating-tho-finer-parts-of-tho-impressions-these-observations-were-ublished-in-the-journal-of-the-geological-society-of-london-vols-1-and-2-shortly-afterward-image234902348.htmlRMRJ4M9G–. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. 356 THE CAnnoNIFKKOUS SYSTEM. a plantigmdu nppcnranco to tho trackri. liaiii-marks had boon im- pressed on tlio Btirfaco after tho animal had passed over it, and those had probably aided in obliterating tho finer parts of tho impressions. These observations were ])ublished in the Journal of the Geological Society of London, vols. 1 and 2. Shortly afterward
. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. THE CRETACEOUS STRATIGRAPHY OF SOUTH-CENTRAL AFRICA 103 West Coast. Maastrichtian Campanian Santonian Coniacian Turonian Cenomanian Aptian Neocomian Fig. 10. A comparison of the known Cretaceous stratigraphic sequences along the east and west coasts of south-central Africa. T marks the start of a marine trans- gression while R marks regressive phases.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annals-of-the-south-african-museum-=-annale-van-die-suid-afrikaanse-museum-natural-history-the-cretaceous-stratigraphy-of-south-central-africa-103-west-coast-maastrichtian-campanian-santonian-coniacian-turonian-cenomanian-aptian-neocomian-fig-10-a-comparison-of-the-known-cretaceous-stratigraphic-sequences-along-the-east-and-west-coasts-of-south-central-africa-t-marks-the-start-of-a-marine-trans-gression-while-r-marks-regressive-phases-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-image236479587.htmlRMRMMG3F–. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. THE CRETACEOUS STRATIGRAPHY OF SOUTH-CENTRAL AFRICA 103 West Coast. Maastrichtian Campanian Santonian Coniacian Turonian Cenomanian Aptian Neocomian Fig. 10. A comparison of the known Cretaceous stratigraphic sequences along the east and west coasts of south-central Africa. T marks the start of a marine trans- gression while R marks regressive phases.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance
![. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. RAIN-MARKS IN MARINE ALLUVIUM. 27 Fig. 1. Fig. 2. Fig. 3.. Fig. 4. r. 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.. Dawson, J. W. (John William), Sir, 1820-1899. London : Macmillan; M Stock Photo](https://c8.alamy.com/comp/RJ52P6/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-rain-marks-in-marine-alluvium-27-fig-1-fig-2-fig-3-fig-4-r-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-dawson-j-w-john-william-sir-1820-1899-london-macmillan-m-RJ52P6.jpg ". The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. RAIN-MARKS IN MARINE ALLUVIUM. 27 Fig. 1. Fig. 2. Fig. 3.. Fig. 4. r. 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.. Dawson, J. W. (John William), Sir, 1820-1899. London : Macmillan; M Stock Photo")
. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. RAIN-MARKS IN MARINE ALLUVIUM. 27 Fig. 1. Fig. 2. Fig. 3.. Fig. 4. r. 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.. Dawson, J. W. (John William), Sir, 1820-1899. London : Macmillan; M Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-rain-marks-in-marine-alluvium-27-fig-1-fig-2-fig-3-fig-4-r-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-dawson-j-w-john-william-sir-1820-1899-london-macmillan-m-image234910542.htmlRMRJ52P6–. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. RAIN-MARKS IN MARINE ALLUVIUM. 27 Fig. 1. Fig. 2. Fig. 3.. Fig. 4. r. 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.. Dawson, J. W. (John William), Sir, 1820-1899. London : Macmillan; M
. The Australian zoologist. Zoology; Zoology; Zoology. VERTEBRATES OF VICTORIA FOSSIL CAVE Q bench mark 3 6 9 metres. Fig. 2. Floor plan of the fossil chamber. X marks the position of the access shaft. • peg positions for 3 m grid. A, marks position of initial excavation; B, position of stratigraphic pit; C, the third excavation. Aust. Zool. 21(4), 1984 307. 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.. Royal Zoological S Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-australian-zoologist-zoology-zoology-zoology-vertebrates-of-victoria-fossil-cave-q-bench-mark-3-6-9-metres-fig-2-floor-plan-of-the-fossil-chamber-x-marks-the-position-of-the-access-shaft-peg-positions-for-3-m-grid-a-marks-position-of-initial-excavation-b-position-of-stratigraphic-pit-c-the-third-excavation-aust-zool-214-1984-307-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-royal-zoological-s-image235289321.htmlRMRJP9X1–. The Australian zoologist. Zoology; Zoology; Zoology. VERTEBRATES OF VICTORIA FOSSIL CAVE Q bench mark 3 6 9 metres. Fig. 2. Floor plan of the fossil chamber. X marks the position of the access shaft. • peg positions for 3 m grid. A, marks position of initial excavation; B, position of stratigraphic pit; C, the third excavation. Aust. Zool. 21(4), 1984 307. 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.. Royal Zoological S
![. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. i ) . m I l"ig. 1.—Imiires«lons of Knlii-Drops.—Modern.—Itay of I'unily. „ 2.—ImpresRlons of Uiilii Drops.—Carboniferous.—Tiitiimgouclio. „ 3.—Impressions of Confiniietl Itiiin.—t'arlxmiferous. „ 4.—Shrinkage Cracks ami Unin Marks.—Carboniferous.—Reduced In nice. „ 6—Cast uf Kill Marks.—Carboiiiforous.—Reduced iu size. i|» "SI ' 11.,. Please not Stock Photo](https://c8.alamy.com/comp/RJ52M8/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-i-m-i-lquotig-1imiireslons-of-knlii-dropsmodernitay-of-iunily-2impresrlons-of-uiilii-dropscarboniferoustiitiimgouclio-3impressions-of-confiniietl-itiiintarlxmiferous-4shrinkage-cracks-ami-unin-markscarboniferousreduced-in-nice-6cast-uf-kill-markscarboiiiforousreduced-iu-size-i-quotsi-11-please-not-RJ52M8.jpg ". The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. i ) . m I l"ig. 1.—Imiires«lons of Knlii-Drops.—Modern.—Itay of I'unily. „ 2.—ImpresRlons of Uiilii Drops.—Carboniferous.—Tiitiimgouclio. „ 3.—Impressions of Confiniietl Itiiin.—t'arlxmiferous. „ 4.—Shrinkage Cracks ami Unin Marks.—Carboniferous.—Reduced In nice. „ 6—Cast uf Kill Marks.—Carboiiiforous.—Reduced iu size. i|» "SI ' 11.,. Please not Stock Photo")
. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. i ) . m I l"ig. 1.—Imiires«lons of Knlii-Drops.—Modern.—Itay of I'unily. „ 2.—ImpresRlons of Uiilii Drops.—Carboniferous.—Tiitiimgouclio. „ 3.—Impressions of Confiniietl Itiiin.—t'arlxmiferous. „ 4.—Shrinkage Cracks ami Unin Marks.—Carboniferous.—Reduced In nice. „ 6—Cast uf Kill Marks.—Carboiiiforous.—Reduced iu size. i|» "SI ' 11.,. Please not Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-geology-of-nova-scotia-new-brunswick-and-prince-edward-island-or-acadian-geology-microform-geology-geology-stratigraphic-paleontology-geology-economic-gologie-gologie-stratigraphique-palontologie-gologie-conomique-i-m-i-lquotig-1imiireslons-of-knlii-dropsmodernitay-of-iunily-2impresrlons-of-uiilii-dropscarboniferoustiitiimgouclio-3impressions-of-confiniietl-itiiintarlxmiferous-4shrinkage-cracks-ami-unin-markscarboniferousreduced-in-nice-6cast-uf-kill-markscarboiiiforousreduced-iu-size-i-quotsi-11-please-not-image234910488.htmlRMRJ52M8–. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. i ) . m I l"ig. 1.—Imiires«lons of Knlii-Drops.—Modern.—Itay of I'unily. „ 2.—ImpresRlons of Uiilii Drops.—Carboniferous.—Tiitiimgouclio. „ 3.—Impressions of Confiniietl Itiiin.—t'arlxmiferous. „ 4.—Shrinkage Cracks ami Unin Marks.—Carboniferous.—Reduced In nice. „ 6—Cast uf Kill Marks.—Carboiiiforous.—Reduced iu size. i|» "SI ' 11.,. Please not
