Galerie d'images
Toutes les images de la base — taxons, formations et intervalles géologiques.
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2,839 image(s)
'The Kitchen Door' in Quality Square, Ludlow
"The Vaults"
Pseudocidaris mammosa Stage : Kimmeridgian 157.3 ± 1.0 Ma and 152.1 ± 0.9. (million years ago)
Etage: Kimméridgien, Sous-étage: inférieur, Zone: Rasenia cymodoce, Sous-zone: Lithacosphinctes achilles, Horizon: Lithacosphinctes achilles. -150.8 à –155.7 millions d'années.
Fig 2. Geological section of the “Mittlerer Kimmeridge”. This figure is based on Fischer and modified from Lallensack et al. Beds yielding terrestrial fossils are listed.
Steinbruch Langenberg. Steilgestellte Schichten des Jura.
Formation d'âge Kimmeridgien (jaune orangé) et Tithonien (Barre tithonique, en gris sur la photo). On peut remarquer que les strates ont été plissées. L'âge des mouvements tectoniques ayant déformé la structure est donc plus jeune que le Tithonien.
The GSSP for the Hirnantian stage in the ICS geological timescale (uppermost Ordovician stage), located in the Wangjiawan profile (an outcrop of black shale, brownishly weathered siliceous shale and chert layers of the Wufeng Formation) along the G241 road, about 40 km north of Yichang, Hubei, China. An exact golden spike is missing in the profile (2025) but a memorial plague marks the place. The GSSP occurs at the first appearance of fossils of the graptolite species Normalograptus extraordinarius. It was ratified in 2006.
Eleniceras cf. curvicostatum (Tzankov), Lower Hauterivian, Kalotina, Bulgaria Cr1 963X1 at the Sofia University 'St. Kliment Ohriski' Museum of Paleontology and Historical Geology
Eleniceras aff. stevrecensis Breskovski, Lower Hauterivian, Dragoman, Bulgaria, Cr1 959 - Cr1 960 X 1 at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
DUVALIA POLYGONALIS (BLAINVILLE) HAUTERIVIAN TEKE DERE SHUMEN SOFIA UNIVERSITY 'ST. KLIMENT OHRIDSKI' MUSEUM OF PALEONTOLOGY AND HISTORICAL GEOLOGY
Distoloceras belimelensis sp.n. Lower Hauterivian, Belimel, Montana Province, Cr1 970X1 (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
Crioceratites (C.) villiersianum bituberculatum (Sarkar) Hauterivian, Belimel, Cr1 929X1 at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
Acrioceras (Aspinoceras) dilatatum (d'Orbigny) Upper Hauterivian, Belimel, Montana Province, (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
Acanthodiscus vaceki (Neumayr & Uhlig) Lower Hauterivian, Dragoman, Bulgaria, Cr1 976X1 (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
Life reconstruction of two species of Protonympha in the Devonian Catskill delta of New York
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene) 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The rocks seen here are of marine origin and date from the late Pliocene and Pleistocene.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene) 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily. A geologist is seen at work at the red line.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene), 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily. Two geologists are seen at work at the red line.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene), 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene), 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily.
Monte San Nicola in Sicily, Italy, south of Butera in the province of Caltanissetta. The red line below the '5' on the rock marks the basis of the Gelasian (Lower Pleistocene), 2.58 million years ago. The Gelasian is a geologic age named after the nearby city of Gela in southern Sicily.
Kalksandskalk fra København kalk Fm med omlejrede bryozoer (netmønster) og skalstumper
Koralkalk fra Faxe kalkbrud
Main floristic types from the earliest Danian: Cheirolepidiaceae, shrubs and other low–diversity flora. doi:10.1371/journal.pone.0052455.g007
Glacialt forstyrret koralkalk, Faxe
Eekaulostomus cuevasae gen. and sp. nov. from the Danian marine deposits of the Belisario Domínguez quarry, near Palenque, Chiapas, southeastern Mexico. 1, General view of IGM 4716, holotype and single specimen known. 2, Idealized line drawing of the same specimen.
Bryozobanker i Stevns klint, set fra stranden ved Boesdal kalkbrud (i let diset vejr)
Grå flint med fossiler af søpindsvin, Krauseparken i København
“Sternberger Kuchen” (“Sternberg cake”), a large late Pleistocene glaciofluvial pebble of a highly fossiliferous, shallow marine sandstone of the North German Paleogene (Sülstorf beds, formerly known as “Sternberg rock”, Chattian, Oligocene, about 25 million years old). The fossil content is mainly made up of mollusks (pelecypods, gastropods, scaphopods). Provenance: Sternberg, Mecklenburg-Vorpommern, Northeast Germany.
4 Tonnen schwerer Findling mit Muscheln einer Art der Gattung Pectunculus, der wohl ungefähr 25 Millionen Jahre alt ist
Stein aus Sandstein aus dem Cenoman im Alpengarten in Pfronten-Steinach, Obere Kreide, Herkunft Pfronten-Röfleuten
Quarry called “Ratssteinbruch” at Plauenscher Grund (gorge-like valley of the river Weißeritz nearby/in the city of Dresden, Saxony, Germany), Upper Carboniferous Monzonite (historically identified as Syenite) of the Meißen Massif (Paleozoic basement) unconformably overlain by Upper Cenomanian beds of the Dölzschen Formation, yellowish basal conglomerate and overlying bluish silty clay-marlstone (“plenus-Pläner”) of the Saxo-Bohemian Cretaceous Basin (Mesozoic platform).[1]
A light coloured sample of Miorcani flint from the Cenomanian chalky marl layer of the Moldavian Plateau. This sample came from the flint mine near Rădăuţi-Prut. (ca. 7.5 cm wide)
Pilares de Los Gigantes, provincia de Río Negro, correspondientes la la Formación Candeleros.
Typical landscape of the hills around Montmoreau. Saint-Amant, Charente, France.
Typical landscape of the hills around Montmoreau. Saint-Amant, Charente, France.
Chalky hillside with its characteristic vegetation (dry lawn, juniper, orchids, pines on the top). Juignac, Charente, France.
Holotype skull of the centrosaurine ceratopsian dinosaur Diabloceratops eatoni from the Late Cretaceous (Campanian) of the Wahweap Formation, Grand Staircase-Escalante National Monument, Utah. Photograph by Nick Longrich, 2023.