You are here:  >   >   >   >   >   > 


Crystal System: Amorphous
Status of Occurrence: Confirmed Occurrence
Distribution: Uncommon
Chemical Composition: Hydrous aluminium silicate
Chemical Formula: Al2O3.1.3-2.0(SiO2).2.5-3.0(H2O)
Method(s) of Verification: Welsh Foxdale - unspecified analysis (by Prior, 1906), presumably wet chemistry; Cwm Dwyfnant - wet chemical analysis (G.T. Prior), X-ray diffraction analysis (Natural History Museum, no. x1663).

Chemical Group:

Geological Context:

Microcrystalline mass of allophane from Cyffty Mine, Llanrwst. National Museum of Wales specimen (NMW 87.43G.M.14), ex A. Dean. Photo by D.I. Green, © National Museum of Wales.
Introduction: allophane is a found as a low temperature secondary mineral, forming by the alteration of volcanic ash: by hydrothermal alteration of feldspar in igneous rocks or in hydrothermal veins where is can be associated with metallic ore, particularly copper.
Occurrence in Wales: four occurrences of allophane have been recorded from Wales. Although little detail is available regarding allophane from the iron mines at Betws Garmon, Snowdonia cited by Jenkins & Johnson (1993), the three remaining localities described below have formed by hydrothermal activity associated with vein mineralization.

Key Localities:


  1. Jenkins, D.A. & Johnson, D.B., 1993. Abandoned metal mines: a unique mineralogical and microbiological resource. Journal of the Russell Society, 5, 40-44.
  2. Prior, G.T., 1906. Dundasite from North Wales. Mineralogical Magazine, 14, 167-169
  3. Russell, A., 1944. Notes on some minerals either new or rare in Britain. Mineralogical Magazine, 27, 1-10.