High Geest
The High Geest is a Geest -Landscape with landscape increases by glacial deposits in the south of Schleswig-Holstein and in Geesthang area of Hamburg (north and south of the Elbe) as well as in the northern Lower Saxony . It surrounds the Elbe glacial valley with partly steep elevations, such as the so-called Altona balcony on the Elbe with about 27 m, up to 94.4 m above sea level. NHN on the Haferberg near the Geesthacht pumped storage power station .
Geological origin and condition
The Hohe Geest consists of the old and end moraines of the glacier of the Warthe stage of the Saale Ice Age (about 160,000 to 100,000 BC) coming from the northeast from Finland and Scandinavia , which covered northern Germany. The Hohe Geest is cut through by the up to twenty kilometers wide glacial valley of the Elbe and can be roughly assigned to the south of Schleswig-Holstein and the northern part of Lower Saxony through this natural border. Hamburg is essentially located in and around the glacial valley of the Elbe and therefore has a significant share in this landscape: The height differences in Harburg and Blankenese are determined by the Geest slope. The course of the B5 between Billstedt and Geesthacht clearly shows the Geest slope, the border between the high Geest and the marshland as well as the lowland riverside landscape (also called Brook ) or alluvial forest . Agricultural significance of the High Geest by the proportion fertile glacial till , by the glaciers carried sound or Lehmschollen have formed clay or clay pits.
High Geest in Schleswig-Holstein
This geest, consisting of "Hoher Geest" and "Niederer Geest", is the middle natural landscape in Schleswig-Holstein . Part of it is the Heide-Itzehoer Geest .
Hohe Geest in the north of Lower Saxony & in the south of Hamburg
In northern Lower Saxony and in the south of Hamburg , the Hohe Geest is characterized by three mountain ranges:
- The Harburger mountain range includes the Black Mountains ( Harburger Berge ), the Haake, the Rosengarten and Stuvenwald, the Lohberge with the Brunsberg , the Töps and the high area around the Wilseder Berg .
- The Garlstorfer ridge extends from the Mascher Hallonen and the Buchwedel bei Stelle to Brackel and Egestorf .
- The Lüneburg ridge begins at Radbruch and extends over Westergellersen and Wetzen to Robbery Chamber .
Individual evidence
- ↑ Map services of the Federal Agency for Nature Conservation ( information )
- ↑ Tim Mansfeldt: Geology and Geomorphology Schleswig-Holstein ( Memento of the original from March 7, 2016 in the Internet Archive ) Info: The archive link has been inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice. , Faculty of Geosciences - Geographical Institute of the Ruhr University Bochum: Seminar: Geology, geomorphology and soils of Schleswig-Holstein
- ^ Wilhelm Marquardt: The landscape of the circle; in: Harburg district - history - landscape - economy; Gerhard Stalling AG (ed.); Wirtschaftsverlag, Oldenburg, 1963; P. 38