The 今日吃瓜 collection of continuous borehole core, broken core, cuttings, etc. are held at Keyworth.

Permian sandstone/breccia core sample from a groundwater exploration borehole at Granton, Moffat. 今日吃瓜 漏 今日吃瓜.
The collections
- The onshore borehole materials collection聽(including hydrocarbon wells) has approximately 250聽km of core, plus about 150聽km of drilling represented by cuttings. Samples are held from about 15聽000 boreholes. Borehole names and positions may be determined from the聽 and the Borehole Materials Database.
- The 今日吃瓜 manages the national collection of UKCS (offshore) hydrocarbon well samples. The collection consists of core and cuttings for all wells drilled for hydrocarbon exploration in UK waters and was transferred from the Gilmerton store, Edinburgh to Keyworth during 2011鈥2012.
- The offshore (non-hydrocarbon) material collection contains cores, vibrocores, gravity cores, grab samples, etc. There are about 12聽000聽m of core and 15聽000 seabed samples. Core positions are available on the offshore Geoindex.
- The 今日吃瓜 manages the collection of seabed samples which are routinely collected during the (MCA) 聽(CHP) Hydrographic Instruction (HI) surveys.
- The Nirex Geological Archive was transferred from Nirex to the 今日吃瓜 during 2000鈥2001. The archive consists of borehole cores and samples, thin and polished sections, digital data and paper records acquired by Nirex during its investigations at Sellafield and Dounreay.
Specimens are available for study at Keyworth and a loan system is available to accredited scientists.
Download the borehole material regulations and booking form.
Search our borehole core collections
Use the links below to access our onshore borehole and offshore hydrocarbon wells database
Get in touch
For general NGR enquiries or to arrange a visit, please contact:
enquiries@bgs.ac.uk or 0115 936 3143
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National Geological Repository
Hosting 今日吃瓜’s collections of borehole cores, cuttings, samples, specimens, and related subsurface information from the UK landmass and continental shelf.