Distribution of basalt boulders and ice rafted debris in the region of the Iceland-Faroe-Ridge (Fig. 6-12)
Psephitic particles in the region of the Iceland-Faeroe-Ridge have been transported and deposited by means of a complex interplay of glacier movements and drifting icebergs. The composition of the particle association is controlled by the sedimentation of basaltic rock particles derived from the rid...
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PANGAEA
1982
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.548073 https://doi.org/10.1594/PANGAEA.548073 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.548073 2023-05-15T16:21:44+02:00 Distribution of basalt boulders and ice rafted debris in the region of the Iceland-Faroe-Ridge (Fig. 6-12) Wohlfeil, Kay MEDIAN LATITUDE: 62.867179 * MEDIAN LONGITUDE: -9.864359 * SOUTH-BOUND LATITUDE: 60.250000 * WEST-BOUND LONGITUDE: -16.916667 * NORTH-BOUND LATITUDE: 64.916667 * EAST-BOUND LONGITUDE: -4.833333 * MINIMUM DEPTH, sediment/rock: 0 m * MAXIMUM DEPTH, sediment/rock: 0 m 1982-01-08 text/tab-separated-values, 391 data points https://doi.pangaea.de/10.1594/PANGAEA.548073 https://doi.org/10.1594/PANGAEA.548073 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.548073 https://doi.org/10.1594/PANGAEA.548073 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Wohlfeil, Kay (1982): Verbreitung, Herkunft und Bedeutung der Psephite des Seegebietes zwischen den Färöer und Island. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C36, 31-56 Basalt Carbonates Chert Claystone DEPTH sediment/rock Dredge DRG Event label Gravity corer (Kiel type) Iceland-Faeroe Ridge Ice rafted debris Latitude of event Longitude of event M20 M20_20 M20_22 M20_23 M20_24 M20_25 M20_26 M20_27 M20_28 M20_29 M20_34 M20_35 M20_36 M20_37 M20_38 M20_39 M20_43 M20_45 M20_46 M20_47 M38 M38_198 M38_208 M38_229 M38_233 M38_236 M38_243 M38_248 M38_249 M38_252 M38_254 M54 M54_329 M54_330 M54_331 M54_332 Dataset 1982 ftpangaea https://doi.org/10.1594/PANGAEA.548073 2023-01-20T08:22:19Z Psephitic particles in the region of the Iceland-Faeroe-Ridge have been transported and deposited by means of a complex interplay of glacier movements and drifting icebergs. The composition of the particle association is controlled by the sedimentation of basaltic rock particles derived from the ridge itself and, in addition to that and in southern parts of the ridge, from the Faeroe Islands, the Faeroe-Bank and the Bill Baileys-Bank. Besides, there are crystalline and sedimentary dropstones showing a very varied petrography and a wide range of particle sizes. Their percentage becomes greater as the distance from the ridge increases. The association of dropstones is relatively homogeneous in the region of the ridge and only at greater distances from the ridge it becomes more differentiated. Owing to their composition and distribution, as well as on the basis of characteristic fossils and rock types, the drop-stones are derived from Scandianvia and Great Britain. During periods of maximum glaciation, the Icland-Faeroe-Ridge, th eFaeroe-Bank and the Bill Baileys-Bank were under ice. Dataset glacier Iceland PANGAEA - Data Publisher for Earth & Environmental Science Bill Baileys Bank ENVELOPE(-10.250,-10.250,60.583,60.583) ENVELOPE(-16.916667,-4.833333,64.916667,60.250000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Basalt Carbonates Chert Claystone DEPTH sediment/rock Dredge DRG Event label Gravity corer (Kiel type) Iceland-Faeroe Ridge Ice rafted debris Latitude of event Longitude of event M20 M20_20 M20_22 M20_23 M20_24 M20_25 M20_26 M20_27 M20_28 M20_29 M20_34 M20_35 M20_36 M20_37 M20_38 M20_39 M20_43 M20_45 M20_46 M20_47 M38 M38_198 M38_208 M38_229 M38_233 M38_236 M38_243 M38_248 M38_249 M38_252 M38_254 M54 M54_329 M54_330 M54_331 M54_332 |
spellingShingle |
Basalt Carbonates Chert Claystone DEPTH sediment/rock Dredge DRG Event label Gravity corer (Kiel type) Iceland-Faeroe Ridge Ice rafted debris Latitude of event Longitude of event M20 M20_20 M20_22 M20_23 M20_24 M20_25 M20_26 M20_27 M20_28 M20_29 M20_34 M20_35 M20_36 M20_37 M20_38 M20_39 M20_43 M20_45 M20_46 M20_47 M38 M38_198 M38_208 M38_229 M38_233 M38_236 M38_243 M38_248 M38_249 M38_252 M38_254 M54 M54_329 M54_330 M54_331 M54_332 Wohlfeil, Kay Distribution of basalt boulders and ice rafted debris in the region of the Iceland-Faroe-Ridge (Fig. 6-12) |
topic_facet |
Basalt Carbonates Chert Claystone DEPTH sediment/rock Dredge DRG Event label Gravity corer (Kiel type) Iceland-Faeroe Ridge Ice rafted debris Latitude of event Longitude of event M20 M20_20 M20_22 M20_23 M20_24 M20_25 M20_26 M20_27 M20_28 M20_29 M20_34 M20_35 M20_36 M20_37 M20_38 M20_39 M20_43 M20_45 M20_46 M20_47 M38 M38_198 M38_208 M38_229 M38_233 M38_236 M38_243 M38_248 M38_249 M38_252 M38_254 M54 M54_329 M54_330 M54_331 M54_332 |
description |
Psephitic particles in the region of the Iceland-Faeroe-Ridge have been transported and deposited by means of a complex interplay of glacier movements and drifting icebergs. The composition of the particle association is controlled by the sedimentation of basaltic rock particles derived from the ridge itself and, in addition to that and in southern parts of the ridge, from the Faeroe Islands, the Faeroe-Bank and the Bill Baileys-Bank. Besides, there are crystalline and sedimentary dropstones showing a very varied petrography and a wide range of particle sizes. Their percentage becomes greater as the distance from the ridge increases. The association of dropstones is relatively homogeneous in the region of the ridge and only at greater distances from the ridge it becomes more differentiated. Owing to their composition and distribution, as well as on the basis of characteristic fossils and rock types, the drop-stones are derived from Scandianvia and Great Britain. During periods of maximum glaciation, the Icland-Faeroe-Ridge, th eFaeroe-Bank and the Bill Baileys-Bank were under ice. |
format |
Dataset |
author |
Wohlfeil, Kay |
author_facet |
Wohlfeil, Kay |
author_sort |
Wohlfeil, Kay |
title |
Distribution of basalt boulders and ice rafted debris in the region of the Iceland-Faroe-Ridge (Fig. 6-12) |
title_short |
Distribution of basalt boulders and ice rafted debris in the region of the Iceland-Faroe-Ridge (Fig. 6-12) |
title_full |
Distribution of basalt boulders and ice rafted debris in the region of the Iceland-Faroe-Ridge (Fig. 6-12) |
title_fullStr |
Distribution of basalt boulders and ice rafted debris in the region of the Iceland-Faroe-Ridge (Fig. 6-12) |
title_full_unstemmed |
Distribution of basalt boulders and ice rafted debris in the region of the Iceland-Faroe-Ridge (Fig. 6-12) |
title_sort |
distribution of basalt boulders and ice rafted debris in the region of the iceland-faroe-ridge (fig. 6-12) |
publisher |
PANGAEA |
publishDate |
1982 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.548073 https://doi.org/10.1594/PANGAEA.548073 |
op_coverage |
MEDIAN LATITUDE: 62.867179 * MEDIAN LONGITUDE: -9.864359 * SOUTH-BOUND LATITUDE: 60.250000 * WEST-BOUND LONGITUDE: -16.916667 * NORTH-BOUND LATITUDE: 64.916667 * EAST-BOUND LONGITUDE: -4.833333 * MINIMUM DEPTH, sediment/rock: 0 m * MAXIMUM DEPTH, sediment/rock: 0 m |
long_lat |
ENVELOPE(-10.250,-10.250,60.583,60.583) ENVELOPE(-16.916667,-4.833333,64.916667,60.250000) |
geographic |
Bill Baileys Bank |
geographic_facet |
Bill Baileys Bank |
genre |
glacier Iceland |
genre_facet |
glacier Iceland |
op_source |
Supplement to: Wohlfeil, Kay (1982): Verbreitung, Herkunft und Bedeutung der Psephite des Seegebietes zwischen den Färöer und Island. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C36, 31-56 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.548073 https://doi.org/10.1594/PANGAEA.548073 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.548073 |
_version_ |
1766009726509776896 |