Geological overview map 1:300.000 — Geological overview map

Geological Map of Rhineland Palatinate 1:300,000 (Guek 300) The Guek 300 has been reassembled on the basis of public geological maps of different scales. It replaces the previous official geological overview map of Rhineland-Palatinate in scale 1: 500 000. The new map is based on the geological overview maps issued by the Federal Institute for Geosciences and Raw Materials in Hannover in cooperation with the State Geological Services of the Laender in scale 1: 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 Land Office for Geology and Mining Rhineland-Palatinate: 100 000, 1: 50 000 and 1: 25 000 as well as the geological (and vulcanological) maps of external agents. Due to the scale, stratigraphic formations were merged into larger units and boundary lines were generalised. The area-wise very complex stoning pattern has been reduced (strongly generalised and) to the representation of significant shocks. Terms of use see: http://www.lgb-rlp.de/karten-und-produkte/online-karten/nutzungsbedingungen-fuer-online-karten.html:Geologische Overview Map of Rhineland Palatinate 1:300.000 (Guek 300) The Guek 300 has been reassembled on the basis of published geological maps of different masses. It replaces the previous official geological overview map of Rhineland-Palatinate in scale 1: 500 000. The new map is based on the geological overview maps issued by the Federal Institute for Geosciences and Raw Materials in Hannover in cooperation with the State Geological Services of the Laender in scale 1: 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 Land Office for Geology and Mining Rhineland-Palatinate: 100 000, 1: 50 000 and 1: 25 000 as well as the geological (and vulcanological) maps of external agents. Due to the scale, stratigraphic formations were merged into larger units and boundary lines were generalised. The area-wise very complex stoning pattern has been reduced (strongly generalised and) to the representation of significant shocks. Terms of use see: http://www.lgb-rlp.de/karten-und-produkte/online-karten/nutzungsbedingungen-fuer-online-karten.html