Gagnasafn (GDB) NI_J5v_Surtsey_jardsaga1963-2006: Surtsey Jarðfræðikort jarðsaga 1963-2006 1:5.000 [Surtsey Geological time 1963-2006 1:5.000]. Sýning Náttúrufræðistofnunar í Þjóðmenningarhúsinu – SURTSEY 1963-2130, 7. maí 2007 til mars 2009. Náttúrufræðistofnun Íslands stóð fyrir sýningunni, með stuðningi fjölda stofnana, fyrirtækja og ráðuneyta umhverfis- og menntamála. Tilefnið var að 40 ár voru liðin frá því eldgosi lauk í Surtsey og eyjan var í tilnefningarferli sem heimsminjasvæði UNESCO. Fyrir þessa sýningu var útbúin tímaröð sem sýnir breytingar í jarðfræði Surtseyjar frá upphafi til ársins 2006, eða samtals 15 jarðfræðikort sem sýna eyjuna 16. nóv. 1963, 17. feb. og 25. ág. 1964, 1965, 1966, 1967, 1972, 1977, 1983, 1988, 1992, 1998, 2002, 2004 og 2006. Gagnaserían inniheldur upplýsingar um hraun, móberg, gjósku, gjall, strandset, foksand (flákalag) og gíga (fláka- og línulag). Jarðfræðikortin sýna myndun eyjarinnar 1963-1967, myndun móbergs og sjávarrof eftir að gosi lauk.

An interpretation of bedrock geology, topography and other sources of information that shows the potential for karst formations. This is a reconnaissance level map for all of British Columbia

The Kentucky Geological Survey (KGS), as part of the United States Geoscience Information Network (USGIN), provides a compilation of geologic maps from the NGCMP-09 database (http://ngcmp.usgs.gov/) covering the United States of America including Hawaii and Alaska. This Service was published by the KGS as part of the USGIN initiative to “create and facilitate discovery and access to geoscience information provided by state and federal geological surveys of the United States”. These data were compiled by the Kentucky Geological Survey. Three (3) layers included in this service are as follows: 1. GeologicUnitView is a compilation datasets containing geologic units covering the Commonwealth of Kentucky at 1:24,000 scale. The data table includes geologic name, description, lithology, and geologic history. 2. ContactView is a compilation dataset containing geologic contacts covering the Commonwealth of Kentucky at a scale of 1:24,000. The table includes contact type, positional accuracy and generic symbolizer (FGDC). Citations are included in the data set. 3. ShearDisplacementStructureView is a compilation dataset containing shear displacement structures covering the Commonwealth of Kentucky at a scale of 1:24,000. The table includes fault type, positional accuracy, and generic symbolizer (FGDC). Citations are included in the dataset.

The bedrock map of Laos

A polygon coverage showing the location of coalfields with coalbed methane (cbm) potential in BC

Historic placer mining areas in Yukon can be grouped into ten areas: Klondike; Sixtymile; Fortymile; Clear Creek; Moosehorn Range; Stewart River; Whitehorse South; Mayo; Dawson Range and Livingstone Creek. Each area has its own geomorphic setting and depositional history which is related to its glacial history. Several Quaternary glacial advances have been described in Yukon, and these are generally divided into three episodes, commonly known as the pre-Reid, Reid and McConnell, in order of oldest to most recent. Distributed from [GeoYukon](https://yukon.ca/geoyukon) by the [Government of Yukon](https://yukon.ca/maps) . Discover more digital map data and interactive maps from Yukon's digital map data collection. For more information: [geomatics.help@yukon.ca](mailto:geomatics.help@yukon.ca)

This layer contains polygon features that represent the generalized surficial geology of New Brunswick. Unconsolidated materials occurring over bedrock, are classified according to physical attributes and genesis, and categorized into map units. This layer is intended to be used at small scales (e.g., provincial scale). It is an update of the 2002 Generalized Surficial Geology Map of New Brunswick, the updates reflect re-interpretation of the geology based on additional field investigations.

Canadian Geoscience Knowledge Network WMS provides national coverage geoscience layers

Yukon Territory has been glaciated by Cordilleran and montane glaciers at various times throughout the Pleistocene, as well as by continental ice, the Laurentine Ice Sheet in the Late Pleistocene. Throughout the Late Cenozoic, each successive glaciation appears to have been less extensive than the previous one. In west-central Yukon the earliest glaciation occurred between 2.6 and 2.9 Ma. ago (Duk-Rodkin and Barendregt, 1997). This glaciation was the most extensive and formed a continuous carapace of ice covering all the mountain ranges, except for a small area of Dawson Range and a more extensive area in northern Yukon. The Mid Pleistocene Cordilleran glaciation was less extensive than older glaciations but it formed an extensive ice sheet covering most of the northern Cordillera. The Late Pleistocene glaciation was the most restrictive and formed a continuous carapace of ice from the continental divide to the Saint Elias Mountains, but only restricted ice caps formed on the Ogilvie Mountains. During the last glaciation, the Laurentide Ice Sheet, flowing from the east, reached the northeast part of the Yukon Territory ca. 30 ka ago. Distributed from [GeoYukon](https://yukon.ca/geoyukon) by the [Government of Yukon](https://yukon.ca/maps) . Discover more digital map data and interactive maps from Yukon's digital map data collection. For more information: [geomatics.help@yukon.ca](mailto:geomatics.help@yukon.ca)

GTK Bedrock and Superficial Geology