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Rock 365 : Day 310 : Precambrian-Cambrian Unconformity

Day 310 : Running a field course in Ercall Quarries, Shropshire, England for the third time in two weeks. This is the unconformity (nonconformity) between the Late Precambrian (~560Ma) Ercall Granophyre showing weathering at its upper surface and the breccia facies of the (~535Ma) Lower Cambrian Wrekin Quartzite.

Rock 365 : Day 304 : Fluvioglacial Sediments

Day 304 : Still on Anglesey on a glacial landform fieldtrip. Much discussion relating to the relationship between the fluvioglacial channel and the near vertical faulting. It was suggested that an ice block buried within the sediments melts out causes subsidence and localises the channel. From Gored Tre-castell, near Beaumaris, …

Rock 365 : Day 303 : Phyllite

Day 303 : A weekend away in Anglesey, Wales on a glacial landforms fieldtrip. This is the bed rock at Trwyn Cemlyn, near Wylfa Head. The Late Proterozoic phyllites of the New Harbour Group have had their colour altered by fluid passing along small faults.