Antony Glauser's Photo Gallery
Copper secondaries on surface exposure
Copper secondaries formed by weathering of the exposed mineralization, near the top of Mont Noble.
Mineralized surface exposure, Mt. Noble
Continuation of the U mineralization near the top of Mont Noble, identified by tracing the gamma ray anomaly along the strike of the exposure from the outcrop.
Mineral outcrop on Mont Noble
A mineralized schist outcrop near the top of Mont Noble, similar in appearance to the occurrence at Cleuson. A weak gamma ray anomaly (approx. 0.5-1 µSv/hr) is detectable in the vicinity of the outcrop.
XEL-GRLUraninite (Var: Pitchblende) UO2
A specimen of pitchblende, approximately 15 cm across, with a streak of characteristic yellow secondaries. Lying by the side of the road, on the way up to La Creusaz.
La Creusaz exploration gallery spoil tip
View north-east across the spoil tip below the exploration gallery entrance, La Creusaz.
Iron cemented sandstone 'pipe'
Close-up of the broken end of a box-shaped iron 'pipe' in the sandstone at the Devil's Jumps, near Farnham, Surrey, UK. Weathering has removed the loose, iron-depleted sand in the centre of the pipe, leaving just the iron-rich wall.
Iron cemented sandstone
Weathered face of the iron cemented sandstone exposure at the Devil's Jumps, near Farnham, Surrey, UK, revealing the contorted nature of this curious formation.
Iron cemented sandstone
Exposure of iron cemented sandstone at the Devil's Jumps, near Farnham, Surrey, UK. This section is relatively lightly weathered, being shielded by overhanging rock. Note cross-bedding in the sand.
Mine chimney, St. Austell Consols
View north from the public footpath towards the mine chimney, St. Austell Consols.
Beta contact dose rate for uranium and uraninite
