Cross-Bedded Sandstone - Dawlish Railway (S38)
Cross-Bedded Sandstone - Dawlish Railway (S38)

Cross-Bedded Sandstone with thin beds of Breccia in the cliffs behind the
Rail Line to the east of Dawlish Railway station.
The red colour is the result of the change ,over time, of Iron minerals in the Desert Dune sand from
Limonite to Hematite( Ferric Oxide ).

Ref: 6824

Date: 03/02/2019

Location: SX 9710 7740

Cross-Bedded Sandstone - Dawlish Railway (S38)

Cross-Bedded Sandstone with thin beds of Breccia in the cliffs behind the
Rail Line to the east of Dawlish Railway station.
The red colour is the result of the change ,over time, of Iron minerals in the Desert Dune sand from
Limonite to Hematite( Ferric Oxide ).

Ref: 6824

Date: 03/02/2019

Location: SX 9710 7740