. . . . . . . . . . . . . . . . . . . . . "The South Sm\u00E5land peneplain (Swedish: Sydsm\u00E5l\u00E4ndska peneplanet) is a large flattish erosion surface, a peneplain, formed during the Tertiary, covering large swathes of southern Sm\u00E5land and nearby areas in Southern Sweden. To the east the South Sm\u00E5land peneplain bounds with the Sub-Cambrian peneplain uphill across an escarpment. While is almost as flat as the Sub-Cambrian peneplain the South Sm\u00E5land peneplain differs in that it contains far more residual hills and that it has never been covered by sedimentary rocks. To the south and west (chiefly Halland and Blekinge) 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 Blekinge-Sm\u00E5land border. The South Sm\u00E5land 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 Bolm\u00E5n drains the southwest. M\u00F6rrums\u00E5n drains eastern parts of peneplain. It is possible that the Kv\u00E4rkab\u00E4cken and Sk\u00E4ralid streams that traverses the S\u00F6der\u00E5sen horst in Scania are old antecedent rivers that once flowed through the South Sm\u00E5land peneplain. The existence of this plain was first noted by Sten De Geer in 1913 who termed it Sm\u00E5lands urbergsl\u00E4tt."@en . . . . . . "4160"^^ . . "The South Sm\u00E5land peneplain (Swedish: Sydsm\u00E5l\u00E4ndska peneplanet) is a large flattish erosion surface, a peneplain, formed during the Tertiary, covering large swathes of southern Sm\u00E5land and nearby areas in Southern Sweden. To the east the South Sm\u00E5land peneplain bounds with the Sub-Cambrian peneplain uphill across an escarpment. While is almost as flat as the Sub-Cambrian peneplain the South Sm\u00E5land peneplain differs in that it contains far more residual hills and that it has never been covered by sedimentary rocks. To the south and west (chiefly Halland and Blekinge) the peneplain transitions into Mesozoic-aged hilly surfaces."@en . . "47287735"^^ . "South Sm\u00E5land peneplain"@en . . . . . . "1094829739"^^ . . . . . . . . . . . .