Physical properties of sediment cores from the Iberian Continental Slope, supplement to: Heilemann, Kristina (2000): Hydrodynamische Änderungen des Mittelmeerausstromwassers und deren Abbildung in den Sedimenten des Iberischen Kontinentalhangs. PhD Thesis, Mathematisch-Naturwissenschaftliche Fakultät der Christian-Albrechts-Universität zu Kiel, Germany, 88 pp


Climatic changes cause alterations in circulation patterns of the world oceans. The highly saline Mediterranean Outflow Water (MOW), built within the Mediterranean Sea crosses the Strait of Gibraltar in westerly directions, turning north-westward to stick to the Iberian Slope within 600-1500m water depths. Circulation pattern and current speed of the MOW are strongly influenced by climatically induced variations and thus control sedimentation processes along the South- and West - Iberian Continental Slope.

Metadata Access
Creator Heilemann, Kristina
Publisher PANGAEA - Data Publisher for Earth & Environmental Science
Publication Year 2000
Rights Creative Commons Attribution 3.0 Unported (CC-BY)
Language English
Resource Type Supplementary Collection of Datasets
Format application/zip
Discipline Earth System Research
Spatial Coverage (36N-39N,11W-7 W)
Temporal Point 1997-04-21T11:59:59Z