File:Aufschluss Halterner Sande am Hünsberg.jpg
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| Camera location |  | View this and other nearby images on: OpenStreetMap |  |
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| Description |
Deutsch: Das Münsterland war während der gesamten Oberkreide Teil eines urzeitlichen Meeres. Zwischen de:Recklinghausen, Dorsten, Borken und Coesfeld wurden während des Santoniums (ca. 86,3 – 83,6 mya) sogenannte Halterner Sande in Schichten bis zu 250 Meter Mächtigkeit abgelagert. Das Bild zeigt einen Aufschluss dieser Sande am Hünsberg bei Coesfeld. Die Sandsteilwand hat eine Höhe von etwa 12 Metern. |
| Date | |
| Source | Own work |
| Author | Günter Seggebäing |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 11:16, 29 December 2013 | | 5,453 × 1,929 (8.3 MB) | Watzmann (talk | contribs) | {{Location dec|51.91097|7.086388}} {{Information |description={{de|1=Das Münsterland war während der gesamten Oberkreide Teil eines urzeitlichen Meeres. Zwischen de:Recklinghausen, [[:de:Dorsten|Dor... |
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