
Cliffe Hill Quarry, Markfield
Signed, dated and titled watercolour with pen and ink.
From the artist's personal collection, hung on the walls of his house.
Exhibited at Wymondham Art Gallery, 1984 and Artifact Fine Art in 1986.
Located on the western outskirts of Markfield, Leicestershire this quarry exposes volcanic and sedimentary Charnian rocks dating to the Precambrian eon. It was probably then a volcanic island. An unusually homogeneous form of the rock diorite is sometimes called markfieldite because it is found in the village.
From the artist's personal collection, hung on the walls of his house.
Exhibited at Wymondham Art Gallery, 1984 and Artifact Fine Art in 1986.
Located on the western outskirts of Markfield, Leicestershire this quarry exposes volcanic and sedimentary Charnian rocks dating to the Precambrian eon. It was probably then a volcanic island. An unusually homogeneous form of the rock diorite is sometimes called markfieldite because it is found in the village.
$477.93
Original: $1,365.52
-65%Cliffe Hill Quarry, Markfield—
$1,365.52
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Description
Signed, dated and titled watercolour with pen and ink.
From the artist's personal collection, hung on the walls of his house.
Exhibited at Wymondham Art Gallery, 1984 and Artifact Fine Art in 1986.
Located on the western outskirts of Markfield, Leicestershire this quarry exposes volcanic and sedimentary Charnian rocks dating to the Precambrian eon. It was probably then a volcanic island. An unusually homogeneous form of the rock diorite is sometimes called markfieldite because it is found in the village.
From the artist's personal collection, hung on the walls of his house.
Exhibited at Wymondham Art Gallery, 1984 and Artifact Fine Art in 1986.
Located on the western outskirts of Markfield, Leicestershire this quarry exposes volcanic and sedimentary Charnian rocks dating to the Precambrian eon. It was probably then a volcanic island. An unusually homogeneous form of the rock diorite is sometimes called markfieldite because it is found in the village.











