Thickness (geology)

Thickness in geology and mining refers to the distance across a packet of rock, whether it be a facies, stratum, bed, seam, lode etc.

Actual (1) and apparent (2) bed thickness. (3) Dip angle.

Thickness is measured at right angles to the surface of the seam or bed and thus independently of its spatial orientation. The concept of thickness came originally from mining language, where it was used mainly to indicate the workability of seams. It has since become an established term in earth science, for example in geology, for the depth of sedimentary rocks, in hydrogeology for the vertical extent of groundwater – i.e. the distance from the base of the groundwater layer to its surface – or in soil science for the vertical extent of soil horizons.

Literature

  • Walter Bischoff, Heinz Bramann, Westfälische Berggewerkschaftskasse Bochum: Das kleine Bergbaulexikon. 7th edn., Verlag Glückauf GmbH, Essen, 1988, ISBN 3-7739-0501-7.
  • Heinz Kundel: Kohlengewinnung. 6. Auflage, Verlag Glückauf GmbH, Essen, 1983, ISBN 3-7739-0389-8.
gollark: Perhaps. I don't see why my computer would be much worse than average for that, though.
gollark: Humanbenchmark has a bunch of other things. I have this vaguely weird set of results.
gollark: Perhaps you could try and get a more comfortable keyboard.
gollark: If you blame xorg, try wayland?
gollark: No. As far as I know, at least, load is added more by being in channels than by having lots of people. And if lots of people are in the same channels, this doesn't create much additional load.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.