Geological overview map 1:300.000 - GÜK300: Porphyroids - OGC API Features

Geological overview map of Rhineland-Palatinate 1:300.000 (GUEK 300) The GUEK 300 has been newly compiled on the basis of published geological maps of different scales. It replaces the previous official geological overview map of Rhineland-Palatinate on a scale of 1: 500 000. The new map is based on the 1st scale geological survey maps issued by the Federal Institute for Geosciences and Natural Resources in Hanover in cooperation with the State Geological Services of the Laender : 200 000 (CC 5502 Koeln, CC 5510 Siegen, CC 6302 Trier, CC 6310 Frankfurt a.M. West, CC 7102 Saarbruecken and CC 7110 Mannheim), the geological maps published by the Rhineland-Palatinate State Office for Geology and Mining in the scales 1 : 100 000, 1 : 50 000 and 1 : 25 000 as well as the geological (and volcanic) maps of external processors. Due to scale, stratigraphic formations were combined into larger units and boundary lines were generalized. The area-by-area very complex shock pattern was (strongly generalized and) reduced to the representation of significant shocks. :Geological overview map of Rhineland-Palatinate 1:300.000 (GUEK 300) The GUEK 300 has been newly compiled on the basis of published geological maps of different scales. It replaces the previous official geological overview map of Rhineland-Palatinate on a scale of 1: 500 000. The new map is based on the 1st scale geological survey maps issued by the Federal Institute for Geosciences and Natural Resources in Hanover in cooperation with the State Geological Services of the Laender : 200 000 (CC 5502 Koeln, CC 5510 Siegen, CC 6302 Trier, CC 6310 Frankfurt a.M. West, CC 7102 Saarbruecken and CC 7110 Mannheim), the geological maps published by the Rhineland-Palatinate State Office for Geology and Mining in the scales 1 : 100 000, 1 : 50 000 and 1 : 25 000 as well as the geological (and volcanic) maps of external processors. Due to scale, stratigraphic formations were combined into larger units and boundary lines were generalized. The area-by-area very complex shock pattern was (strongly generalized and) reduced to the representation of significant shocks.