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Direct groundwater discharge to the Baltic Sea in Gdańsk region
| Content Provider | Semantic Scholar |
|---|---|
| Author | Lidzbarski, Miros Aw |
| Copyright Year | 2005 |
| Abstract | InGdansk region groundwater discharge into the Baltic Sea varies largely along the coast. This is due to variability in lithology, permeability and morphology of different formation (sediments of Quaternary, Tertiary and Cretaceous). About 95% of groundwater is drained by hydrographic system (rivers, polders). Only a small part of this water, participating in circulation system, flows directly to the Baltic Sea in Gdansk Region. Largest flow is observed in the area of Coastal Terrace, western part of Vistula Delta Plain and Kaszuby ice-marginal valley. |
| Starting Page | 49 |
| Ending Page | 51 |
| Page Count | 3 |
| File Format | PDF HTM / HTML |
| Volume Number | 18 |
| Alternate Webpage(s) | https://www.pgi.gov.pl/en/docman-tree-all/publikacje-2/special-papers/83-lidzbarski/file.html |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |