WMSLower Saxony's geology is visualised in the 1 : 50 000 geological map of Lower Saxony - base map (GK50) in a homogeneous, scientifically uniform format using up-to-date nomenclature. The map provides information on the distribution, consistence and sequence of rocks to a depth of two metres below ground. Additionally, information on the continuation of these consolidated rock sequences at greater depth can generally be derived. The thematic foundation for map construction is primarily provided by the 1:25 000 map sheets of the geological map of Lower Saxony (GK25) and the derived electronic datasets. Information taken from soil scientific maps and current data from the fields of pedology/soil appraisal, and moor and peat studies are also incorporated. The stratigraphy (age) and the genesis (method of formation) are represented and described in the map and in the corresponding legend. In addition, the legend includes information on the primary and secondary petrographic constituents (rock consistence), and on the lime and humus content of the individual layers. All units identified and numbered in the map are described using the abbreviations of the Symbolschlüssel Geologie (PREUSS et al. 1991). Representation of the geological conditions in the base map is subject to certain rules. Rock strata at least two metres thick and exposed at the surface are designated by a colour fill, and by hatched shading where several layers are superimposed. Horizontal hatching marks stratigraphic sequences comprising only unconsolidated rock, oblique hatching signifies unconsolidated strata overlying consolidated rock. Widely spaced hatching indicates rock exposed at the surface; underlying strata are marked by narrower hatching. Both fill and hatching colours indicate the respective rock type. The original distribution of the rocks is shown in order to emphasise the natural geological conditions in densely built-up areas, even though they may be modified as a result of anthropogenic activity (e.g. made ground).inspireidentifiziertopendatasgd_GeologieNIBIS-MetadatenopendataGeologygeoscientificInformationinfoMapAccessServiceLandesamt für Bergbau, Energie und Geologie (LBEG)postal

Stilleweg 2

HannoverNiedersachsen30655Deutschland+49 511 643-0metadaten@lbeg.niedersachsen.denonenone18001800text/xmlapplication/vnd.ogc.wms_xmlimage/pngimage/png32image/png24image/png;mode=32bitimage/png;mode=24bitimage/jpegtext/htmltext/plaintext/html;fragmenttext/html;cardoapplication/geo+jsonapplication/geojsonapplication/vnd.ogc.se_xmlXML<_ExtendedCapabilities xsi:type="idu:WmsExtendedCapabilities_Type">3.9.7.78266.3.2.52truetruetruehttps://nibis.lbeg.de/cardomap3/public/ogc.ashx?Service=IKX&RenderHint=TargetISOWMS&nodeId=146gergerL105Lower Saxony's geology is visualised in the 1 : 50 000 geological map of Lower Saxony - base map (GK50) in a homogeneous, scientifically uniform format using up-to-date nomenclature. The map provides information on the distribution, consistence and sequence of rocks to a depth of two metres below ground. Additionally, information on the continuation of these consolidated rock sequences at greater depth can generally be derived. The thematic foundation for map construction is primarily provided by the 1:25 000 map sheets of the geological map of Lower Saxony (GK25) and the derived electronic datasets. Information taken from soil scientific maps and current data from the fields of pedology/soil appraisal, and moor and peat studies are also incorporated. The stratigraphy (age) and the genesis (method of formation) are represented and described in the map and in the corresponding legend. In addition, the legend includes information on the primary and secondary petrographic constituents (rock consistence), and on the lime and humus content of the individual layers. All units identified and numbered in the map are described using the abbreviations of the Symbolschlüssel Geologie (PREUSS et al. 1991). Representation of the geological conditions in the base map is subject to certain rules. Rock strata at least two metres thick and exposed at the surface are designated by a colour fill, and by hatched shading where several layers are superimposed. Horizontal hatching marks stratigraphic sequences comprising only unconsolidated rock, oblique hatching signifies unconsolidated strata overlying consolidated rock. Widely spaced hatching indicates rock exposed at the surface; underlying strata are marked by narrower hatching. Both fill and hatching colours indicate the respective rock type. The original distribution of the rocks is shown in order to emphasise the natural geological conditions in densely built-up areas, even though they may be modified as a result of anthropogenic activity (e.g. made ground).sgd_GeologieErdbeobachtung und UmweltopendatainspireidentifiziertGeologieopendataNIBIS-MetadatenCRS:84EPSG:3038EPSG:3039EPSG:3040EPSG:3041EPSG:3042EPSG:3043EPSG:3044EPSG:3045EPSG:3046EPSG:3047EPSG:3857EPSG:4258EPSG:4314EPSG:4326EPSG:4647EPSG:5649EPSG:5650EPSG:25832EPSG:31466EPSG:31467EPSG:31468EPSG:31469EPSG:32631EPSG:32632EPSG:326336.5474718411.7416108651.224963353.93431815https://registry.gdi-de.org/id/de.ni.land.lbeg/1dcc3786-fb81-4c4d-9e7e-f9e831ddb62btext/xml167410.714285714