Styggforsen

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Styggforsen
Styggforsen 2010.jpg
The upper cascade of Styggforsen waterfall
Styggforsen
Location Dalarna, Sweden
Coordinates 61°00′00″N15°11′00″E / 61.00000°N 15.18333°E / 61.00000; 15.18333
Total height36 metres (118 ft)
WatercourseStyggforsån

Styggforsen is a waterfall and a nature reserve located in Dalarna County, Sweden. It is part of the European Union-wide Natura 2000 network. [1]

Contents

Geography

The waterfall is located in the village of Boda, 20 kilometres north of Rättvik. It lies at the eastern edge of the Siljan Ring, [2] a prehistoric impact crater formed 377 million years ago during the Devonian period. This crater was created when a bolide, estimated to be about 4 kilometres in diameter and traveling at around 100,000 kilometres per hour, struck the Earth's surface. [3] The impact caused a significant vertical realignment of the horizontal rock strata and created a bedrock depression, resulting in many of the geological features present today, such as Lake Siljan to the southwest and Styggforsen itself.

The Styggforsån river is interrupted by the 36-meter-high Styggforsen waterfall, which is composed of a column of Ordovician limestone. The waterfall's base meets a dike of brecciated quartz believed to predate the impact event. [4] This site is popular with tourists and features a circular path about one kilometre long that leads to a cave called Troll Hole. During the summer, a cafe is open, and there is an information centre nearby.

Flora and fauna

In 1979, a nature reserve of approximately 12 hectares was established around the waterfall, and in 2005, it was incorporated into the Natura 2000 network. [1] The area's moist climate supports a diverse range of lichens, mosses, and plants, including the rare orchid Epipactis atrorubens, [5] Additionally, it provides a habitat for many insect species, including Venusia cambrica , Hyloicus pinastri, and Epirrhoe alternata. [6] Within the nature reserve, picking flowers and any activities that could affect the environment are strictly prohibited.

Trivia

Ingmar Bergman's film, The Virgin Spring, used Styggforsen as one of its locations. [7]

Related Research Articles

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An impact crater is a depression in the surface of a solid astronomical body formed by the hypervelocity impact of a smaller object. In contrast to volcanic craters, which result from explosion or internal collapse, impact craters typically have raised rims and floors that are lower in elevation than the surrounding terrain. Impact craters are typically circular, though they can be elliptical in shape or even irregular due to events such as landslides. Impact craters range in size from microscopic craters seen on lunar rocks returned by the Apollo Program to simple bowl-shaped depressions and vast, complex, multi-ringed impact basins. Meteor Crater is a well-known example of a small impact crater on Earth.

<span class="mw-page-title-main">Natura 2000</span> Network of protected areas

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<span class="mw-page-title-main">Siljan (lake)</span> Lake in Sweden

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<span class="mw-page-title-main">Siljan Ring</span> Impact structure in the country of Sweden

The Siljan Ring is a prehistoric impact structure in Dalarna, central Sweden. It is one of the 15 largest known impact structures on Earth and the largest in Europe, with a diameter of about 52 kilometres (32 mi). The impact that created the Siljan Ring occurred when a meteorite collided with the Earth's surface during the Devonian period. The exact timing of the impact has been estimated at 376.8 ± 1.7 Ma or at 377 ± 2 Ma. This impact has been proposed as a cause of the first Devonian extinction, the Kellwasser Event or Late Frasnian extinction, due to it being believed by some researchers to coincide around the time of the Kellwasser event at 376.1 Ma ± 1.6 Ma, although the timing of this extinction event has since been pushed forward to 371.93–371.78 Ma. The effects of the impact can clearly be seen in the bedrock in the area. The Cambrian, Ordovician and Silurian sedimentary rocks deformed by the impact are rich in fossils.

The Folkeslunda Limestone is a thin limestone and mudstone geologic formation of Sweden. The formation crops out on the island of Öland to the east of Kalmar, where Folkeslunda is located. Other exposures of the formation are in Dalarna, Jämtland and Östergötland. The Folkeslunda Limestone was deposited in an open marine environment with an estimated water depth of 150 to 200 metres in a eustatically transgressive phase.

<span class="mw-page-title-main">Hällingsåfallet</span> Nature reserve in Jämtland, Sweden

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<span class="mw-page-title-main">Tandövala</span>

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The Hummeln structure was confirmed, in 2015, as an impact crater in Småland province, Sweden. It is a 1.2 kilometres (0.75 mi) wide depression within Lake Hummeln and is estimated to have formed between 470 and 443 Ma ago, during the Ordovician.

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References

  1. 1 2 "Styggforsen (SE0620088)". Natura 2000 . European Environment Agency . Retrieved 5 July 2015.
  2. Juhlin, Christopher; Sturkell, Erik; Ebbestad, Jan Ove R. (December 2012). "A new interpretation of the sedimentary cover in the western Siljan Ring area, central Sweden, based on seismic data". Tectonophysics. 580: 88–99. doi: 10.1016/j.tecto.2012.08.040 . hdl: 10037/4985 .
  3. Reimold, Wolf U.; Kelley, Simon P.; Sherlock, Sarah C. (April 2005). "Laser argon dating of melt breccias from the Siljan impact structure, Sweden: Implications for a possible relationship to Late Devonian extinction events". Meteoritics & Planetary Science. 40 (4): 591–607. doi: 10.1111/j.1945-5100.2005.tb00965.x .
  4. Lindström, Maurits; Schmitz, Birger (20 August 2008). "Palaeozoic impact craters" (PDF). www.iugs.org. pp. 22–23. Retrieved 4 July 2015.
  5. Bremer, Fredrika (1845). I Dalarna, Volume 7 (in Swedish). p. 149.
  6. Tutt, James William; Burr, Malcolm (1998). "List of species". The Entomologist's Record and Journal of Variation. 110: 61, 63–64.
  7. "The Virgin Spring". ingmarbergman.se. Retrieved 4 July 2015.