HCOV_0600, thickness of the Ledo-Paniselian-Brusselian Aquifer system
Description
Flanders is made up of an alternation of aquifers (sand, gravel, chalk, solid rock, ...) and regionally occurring non-aquifers (e.g. clay). The sequence of these aquifers and aquitards has its own coding in Flanders: the Hydrogeological Coding of the Subsurface of Flanders (HCOV-coding). The HCOV coding is made up of hydrogeological main, sub and base units. The main unit groups a sequence of geological layers that have broadly the same hydrogeological properties and thus form a single whole. HCOV_0600 (Ledo-Paniselian-Brusselian Aquifer System), formed by the various sand layers of the Formations of Maldegem (Member of Wemmel), Lede, Brussels, Aalter and Ghent, is an important water-carrying system in Flanders. The dataset ‘HCOV_0600, thickness of the Ledo-Paniselian-Brusselian Aquifer system’ shows the thickness of this hydrogeological layer in a grid per grid cell.
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/b7a21874-0a8a-463e-951c-796716e83551 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/b7a21874-0a8a-463e-951c-796716e83551 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/b7a21874-0a8a-463e-951c-796716e83551 |
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https://metadata.vlaanderen.be/srv/dut/catalog.search#/metadata/b7a21874-0a8a-463e-951c-796716e83551 |
Tags
- ledo-paniseliaan-brusseliaan-aquifersysteem
- geologie
- vmm
- vlaanderen
- hcov
- 0600
- ondergrond
- dov
- databank-ondergrond-vlaanderen