Geology of Gotland
Gotland is made up of a sequence of sedimentary rocks of a Silurian age, dipping to the south-east. The main Silurian succession of
The lime rocks have been weathered into characteristic
The rocks of Gotland display signals of global extinction events, which take their name from parishes on the island: the Ireviken, Mulde and Lau events.
Stratigraphy
The earlier Paleozoic of the island comprises the following formations, listed from youngest to oldest (i.e. from south to north).[7][8]
- Sundre Formation
- Hamra Formation
- Burgsvik Formation– terrestrial input; deposited during regression
- Eke Formation
- Hemse Formation
- Klinteberg Formation
- Halla-Mulde Formation
- Fröjel Formation – terrestrial input; deposited during regression and topped with erosional sequence boundary.
- Slite Group
- Hangvar Formation
- Tofta Formation
- Högklint Formation
- Upper Visby Formation
Quaternary geology
Gotland has mostly a subdued relief composed of flat erosion surfaces. Higher areas usually correspond to those of more-less pure limestone while lower areas have commonly a geology of marl.[2] The reason for this is that limestone is more resistant to erosion than marl.[9] Another general relief feature is that northwestern margin of the island is higher than the southeastern parts.[2] This higher northwestern coast is in part result of the southeast tilt of the sedimentary strata.[10] The northwest coast is straight and contain active cliffs.[2][10] On the other side the eastern coastline is irregular and sinuous.[10]
During large
At the end of the last glaciation Gotland was fully summerged in the waters of the proto-Baltic Sea. The
There are few traces of river and stream erosion in Gotland. Some drainage in the island occurs through karstic systems, including caves.[2] The soils of Gotland are thin with calcareous till clay being the main parent material.[10]
Economic geology
The particular geology of Gotland has conditioned many aspects of human life and economic activity. The economic activities influenced by geology include forestry, farming, cement production and quarrying building stones.[11]
During the industrial age demand for Gotland limestone came from
Exploratory wells have revealed the existence of petroleum oil of Lower Paleozoic age beneath Gotland.[15]
References
- ^ a b Laufeld, S. (1974). Silurian Chitinozoa from Gotland (PDF). Fossils and Strata. Universitetsforlaget.
- ^ JSTOR 520895.
- ^ Creer, K. M (1973). Tarling, D. H.; Runcorn, S. K. (eds.). "A discussion of the arrangement of palaeomagnetic poles on the map of Pangea for Epochs in the Phanerozoic". Implications of Continental Drift to the Earth Sciences L. London, New York: Academic Press: 47–76.
- S2CID 22967281.
- ISSN 0016-786X.
- ^ Laufeld, Sven; Martinsson, Anders (22–28 August 1981). "Reefs and ultrashallow environments. Guidebook to the field excursions in the Silurian of Gotland". Project Ecostratigraphy Plenary Meeting.
- .
- ISBN 978-91-44-05847-4
- ^ Eliason et al. 2010, p. 11
- ^ a b c d Behrens, Sven. "Gotland: Terrängformer". Nationalencyklopedin (in Swedish). Cydonia Development. Retrieved November 30, 2017.
- ^ Eliason et al. 2010, p. 5
- ^ Eliason et al. 2010, p. 41
- ^ Liljebäck, Lars-Erik. "Kalkbrottet som delar Gotland". Naturvetarna (in Swedish). Naturvetarna. Retrieved July 13, 2015.
- ^ "Mål om kalkbrytning på Gotland skjuts upp". Dagens Nyheter (in Swedish). April 10, 2015.
- ^ Zdanaviciute, O.; Lazauskiene, J.; Khoubldikov, A.I.; Dakhnova, M.V.; Zheglova, T.P. (2013). The Hydrocarbon Potential of the Baltic Basin: Geochemistry of Source Rocks and Oils of the Lower Paleozoic Succession. Beijing, China: AAPG Hedberg Conference.
Bibliography
- Eliason, Sara; Bassett, Michael G.; Willman, Sebastian (2010). Geotourism highlights of Gotland. Tallinn. pp. 5, 41. ISBN 978-9985-9973-4-5.)
{{cite book}}
: CS1 maint: location missing publisher (link
Further reading
For a reconstruction of the facies of Gotland, presented as an east–west section, see page 25 of:
- Samtleben, C.; Munnecke, A.; Bickert, T. (2000). "Development of facies and C/O-isotopes in transects through the Ludlow of Gotland: Evidence for global and local influences on a shallow-marine environment". Facies. 43 (1): 1–38. S2CID 130640332.