300px, upright=1.35, View of the South Småland peneplain at Store_Mosse_National_Park._Note_the_residual_hill_or_ Store_Mosse_National_Park._Note_the_residual_hill_or_inselberg_in_the_background.">inselberg.html"_;"title="Store_Mosse_National_Park._Note_the_residual_hill_or_inselberg">Store_Mosse_National_Park._Note_the_residual_hill_or_inselberg_in_the_background. The_South_Småland_peneplain_(_sv.html" ;"title="inselberg_in_the_background..html" ;"title="inselberg.html" ;"title="Store Mosse National Park. Note the residual hill or inselberg">Store Mosse National Park. Note the residual hill or inselberg in the background.">inselberg.html" ;"title="Store Mosse National Park. Note the residual hill or inselberg">Store Mosse National Park. Note the residual hill or inselberg in the background. The South Småland peneplain ( sv">Sydsmåländska peneplanet) is a large flattish erosion surface, a peneplain, formed during the Tertiary, covering large swathes of southern Småland and nearby areas in Southern Sweden. To the east the South Småland peneplain bounds with the Sub-Cambrian peneplain uphill across an

escarpment An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations. The terms ''scarp'' and ''scarp face'' are often used interchangeably with ''esca ...

. While is almost as flat as the Sub-Cambrian peneplain the South Småland peneplain differs in that it contains far more residual hills and that it has never been covered by

sedimentary rock Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles ...

s. To the south and west (chiefly

Halland Halland () is one of the traditional provinces of Sweden (''landskap''), on the western coast of Götaland, southern Sweden. It borders Västergötland, Småland, Scania and the sea of Kattegat. Until 1645 and the Second Treaty of Brömseb ...

and

Blekinge Blekinge (, old da, Bleking) is one of the traditional Swedish provinces (), situated in the southern coast of the geographic region of Götaland, in southern Sweden. It borders Småland, Scania and the Baltic Sea. It is the country's secon ...

) the peneplain transitions into Mesozoic-aged hilly surfaces. In a 2013 study the surface is described as extending over an altitude range of 100 to 150 meters above sea level, while in a subsequent 2017 study the main surface is said to range from 175 to 125 m a.s.l. with a lower level at 100 m a.s.l. existing in near the

- Småland border. The South Småland peneplain is the lowest surface in a piedmonttreppen or staircase of erosion surfaces that make up the South Swedish Dome. The level immediately above it is the 200 m peneplain, that is then followed by the 300 m peneplain and the crestal portion of the Sub-Cambrian peneplain. The western part of the peneplain is drained by the river Nissan while Bolmån drains the southwest.

Mörrumsån Mörrumsån is a river in Blekinge County and Kronoberg County, Sweden. It is roughly long, with its tributary in the lake Asnen, from which it flows south, into the Baltic Sea. The river is known among fishing enthusiasts around the world, becau ...

drains eastern parts of peneplain. It is possible that the Kvärkabäcken and Skäralid streams that traverses the Söderåsen horst in

Scania Scania, also known by its native name of Skåne (, ), is the southernmost of the historical provinces (''landskap'') of Sweden. Located in the south tip of the geographical region of Götaland, the province is roughly conterminous with Skåne ...

are old antecedent rivers that once flowed through the South Småland peneplain. The existence of this plain was first noted by Sten De Geer in 1913 who termed it ''Smålands urbergslätt''.

References

{{DEFAULTSORT:South Smaland peneplain Landforms of Jönköping County Landforms of Kronoberg County Planation surfaces Plains of Sweden Småland

See also

References