Web Map Service (WMS) displaying the GEO_1M_1GE_RO dataset that has been created for the OneGeology-Europe project.

Superficial deposits in Norway in various mapscales - best of. The Superficial Deposits of Norway (best of) is a database giving full coverage of the superficial deposits throughout Norway. High resolution data at scales of 1:20 000 to 1:50 000 exists for only about 30% of the country, mostly in areas where superficial deposits are of significant economic importance. The deposits are classified according to their genesis and thickness.

The Geological Map of Finland depicts the main features of bedrock geology in Finland. In this dataset bedrock areas are classified according to rock types and ages. The dataset is an improved version of the Geological map of the Fennoscandian Shield. The legend has been revised in cooperation with the geological surveys of Sweden and Norway.

The GEOBG100 dataset was created during the period 1995-1997 by digitizing the paper version of the Geological map of Bulgaria at a scale of 1:100 000. This consists of 86 coloured flat sheets, covering the whole onshore territory of the country. The map is available in a Bulgarian or in an English edition. The dataset is digitally integrated and available in MapInfo and ArcGIS formats.

The first version of the contiguous digital map was compiled by Š. Káčer et al.(2005) under the terms of the geological project Digital Geological Map of the Slovak Republic at a scale of 1: 50 000. In addition to areal, line and point information, the following separate layers are available: a list of the background documents, classification of the data in terms of quality, a review of the scheme used for classification of geological units and structures. The areal information provided on the digital map includes: the unified legend and the original legend showing the characteristics and occurrence of individual lithotypes across the whole territory of Slovakia.

GEORH1M is a simplifield version of the geological map of the Republic of Croatia 1 :300 000, which is based on 61 map sheets of the Basic Geological Map 1:100 000 produced in the time period between 1962. and 1989. Map shows lithotostratigraphic units and tectonics of the Republic of Croatia. GEORH1M was edited specifically for the purpose of the OneGeology-Europe project. Map is completely made with GIS technology (ArcGIS 9.3.).

The GEOBG500 dataset was created in 1995 by digitizing the paper version of the Geological map of Bulgaria at a scale of 1:500 000, that was published in 1989. This consists of 2 flat coloured sheets covered the whole territory of Bulgaria. The map has been produced in a combined Bulgarian-English edition and was compiled using the Geological Map of Bulgaria at a scale of 1:100 000 as a base, combined with data from the National Geofund. The dataset is digitally integrated and available in MapInfo format.

Geological map of the Quaternary of Slovakia at a scale of 1 : 500 000 compiled by J. Maglay et al. showing different types of Quaternary deposits according to their origin. The map plainly shows the spatial distribution and surface extent of all primary, as well as some selected "transitional" genetic types of Quaternary sedimentary and volcanic rocks in Slovakia. It presents a basic picture of the sequence of their evolution and their patterns of distribution and deposition. A component of the map is a lithostratigraphic classification of the Quaternary of Slovakia.

The digital geological map of Greece at 1:1million scale is composed of layers of polygonal objects depicting stratigraphic units and lines depicting faults. It has been created - in the frame of the One Geology Europe Plus project - from the 1:50 000 scale map sheets, using the One Geology Europe vocabulary terms to describe lithology & age of formations.

The dataset for the Geological Map of Estonia has been created by vectorizing the paper version of the Bedrock Geological Map of Estonia at a scale of 1:200 000 and has been published in 1997. The map shows areas of bedrock classified into geological units according to the types of rock and their ages. In addition, fault zones in the bedrock are also depicted.