Allenby Formation
http://dbpedia.org/resource/Allenby_Formation an entity of type: SpatialThing
La formation d'Allenby est une formation géologique de roches sédimentaires d'âge Éocène supérieur et moyen située en Colombie Britannique (Canada). Elle est constituée de conglomérats, de grès entrelacés de shale et de charbon. Les gisements de charbon contiennent une abondance de fossiles d'insectes, de poissons et de plantes, issus des shales depuis 1877, les plus connus sont ceux de Princeton Chert.
rdf:langString
The Allenby formation is a sedimentary rock formation in British Columbia which was deposited during the Ypresian stage of the Early Eocene. It consists of conglomerates, sandstones with interbedded shales and coal. The shales contain an abundance of insect, fish and plant fossils known from 1877 and onward, while the Princeton Chert was first indented in the 1950's and is known from anatomically preserved plants.
rdf:langString
rdf:langString
Allenby Formation
rdf:langString
Formation d'Allenby
rdf:langString
Allenby Formation
xsd:float
49.37666702270508
xsd:float
-120.5466690063477
xsd:integer
38615935
xsd:integer
1119334419
rdf:langString
Princeton Chert, Vermillion Bluffs Shale
xsd:integer
1952
rdf:langString
Alternating Princeton Chert and coal sequences
rdf:langString
Ypresian
xsd:string
49.376666666666665 -120.54666666666667
rdf:langString
The Allenby formation is a sedimentary rock formation in British Columbia which was deposited during the Ypresian stage of the Early Eocene. It consists of conglomerates, sandstones with interbedded shales and coal. The shales contain an abundance of insect, fish and plant fossils known from 1877 and onward, while the Princeton Chert was first indented in the 1950's and is known from anatomically preserved plants. There are several notable fossil producing localities in the Princeton & Tulameen basins. Historical collection sites included Nine Mile Creek, Vermilian Bluffs, and Whipsaw Creek, while modern sites include One Mile Creek, Pleasant Valley, Thomas Ranch, and the Princeton Chert.
rdf:langString
La formation d'Allenby est une formation géologique de roches sédimentaires d'âge Éocène supérieur et moyen située en Colombie Britannique (Canada). Elle est constituée de conglomérats, de grès entrelacés de shale et de charbon. Les gisements de charbon contiennent une abondance de fossiles d'insectes, de poissons et de plantes, issus des shales depuis 1877, les plus connus sont ceux de Princeton Chert.
rdf:langString
Shaw
rdf:langString
Coal–breccia, coal–chert
xsd:nonNegativeInteger
84621
<Geometry>
POINT(-120.54666900635 49.376667022705)
<http://commons.wikimedia.org/wiki/Special:FilePath/Amia_hesperia_scale_SRIC_SR_07-43-13_A_img1.jpg>
<http://commons.wikimedia.org/wiki/Special:FilePath/Plecia_curtula_hypotype_Rice_1959_pl1_fig10.png>
<http://commons.wikimedia.org/wiki/Special:FilePath/Plecia_dilatata_holotype_Rice_1959_pl3_fig9.png>
<http://commons.wikimedia.org/wiki/Special:FilePath/Xorides_lambei_Handlirsch_1910_Fig2_cropped.png>
<http://commons.wikimedia.org/wiki/Special:FilePath/Cercopites_torpescens_Scudder_1895_pl1_Fig1.png>
<http://commons.wikimedia.org/wiki/Special:FilePath/Equisetum_similkamense_Dawson_1890_Fig1_a-c.png>
<http://commons.wikimedia.org/wiki/Special:FilePath/Ptysmaphora_fletcheri_Scudder_1895_pl1_Fig6.png>
