The Hornblende Schist continues south of the South Pier for where there is a fault boundary with the serpentine.
2.
On the South-east tip of the Lizard the hornblende schist is " inter-bedded " with pale yellow / green veins and pods of epidosite.
3.
About two miles ( 3 km ) from the Irasburg line, and parallel with it, there is a narrow vein of hornblende schist the whole length of the town.
4.
The hornblende schist, found in contact with the serpentine mass directly to the North ( at Ogo Dour ) and to the South ( at Pentreath and Church Cove ) is the metamorphic remnant of basaltic intrusives into the Folding of the schist at Housel Bay indicates that the formation was also subject to more than one subsequent stage of shear stress.
मोबाइल