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EUR 62 - 139

Parkhotel Marl

Eduard Weitsch Weg 2, 45768 MarlGBP 49 - 111

guest review score: N/A
This hotel lies directly by the town hall and lake in the town of Marl, which is situated between the green Münsterland region and Germany’s indust… More
EUR 63 - 110

Hotel Loemuhle

Loemühlenweg 221, 45770 MarlGBP 50 - 88

guest review score: N/A
Set amid idyllic lakes and parks, this 4-star hotel in the town of Marl offers a generous spa area and quick motorway access to destinations throughou… More
EUR 63 - 123

Feierabendhaus

Lipper Weg 201, 45772 MarlGBP 50 - 98

guest review score: N/A
This hotel in the west of Germany, between the Ruhrgebiet and Münsterland regions is situated in beautiful green surroundings. … More
 

Marl: Guide


Marls are calcium carbonate or lime-rich muds or mudstones which contain variable amounts of clays and calcite or aragonite. The term is most often used to describe lacustrine (lake) sediments but may also be used for marine deposits. The term 'marl' is widely used in North American geology, while the term seekreide is used in European references.

The lower stratigraphy|stratigraphic units of the chalk White cliffs of Dover|cliffs of Dover consist of a sequence of glauconite|glauconitic marl followed by rhythmically-banded limestone and marl layers. Similar upper Cretaceous cyclic sequences in Germany have been correlated with Milankovitch cycle|Milankovitch orbital forcing.

Marl is common in post-glacial lake bed sediments, often found underlying peat bogs. It has been utilized as a soil conditioner and acid soil neutralizing agent.

References


Schurrenberger, D., Russell, J. and Kerry Kelts. 2003. Classification of lacustrine sediments based on sedimentary components. Journal of Paleolimnology 29: 141-154.
Accessed 11/06/2005
Accessed 11/06/2005
Accessed 11/06/2005

See also

Agricultural lime

This "Travel Guide" section is drawn from the Wikipedia article "Marl". We hope you will edit and improve it. It is available under the terms of the GNU Free Documentation License.