k Limestone pavement and tree Limestone pavement and tree. Limestone is a sedimentary rock formed from calcium minerals such as calcium carbonate. This landscape shows the clints and grykes that are a characteristic feature of limestone scenery. The grykes are the deep fissures, caused by the erosion of joints in the limestone, which crisscross the pavement. The clints are the separated blocks of rock that remain. Grykes are often inhabited by shadeloving plants. Photographed in September, near Malham in the Yorkshire Dales National Park, UK. Stock Photo - Afloimages
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Limestone pavement and tree Limestone pavement and tree. Limestone is a sedimentary rock formed from calcium minerals such as calcium carbonate. This landscape shows the clints and grykes that are a characteristic feature of limestone scenery. The grykes are the deep fissures, caused by the erosion of joints in the limestone, which criss cross the pavement. The clints are the separated blocks of rock that remain. Grykes are often inhabited by shade loving plants. Photographed in September, near Malham in the Yorkshire Dales National Park, UK.
RM

Limestone pavement and tree

Limestone pavement and tree. Limestone is a sedimentary rock formed from calcium minerals such as calcium carbonate. This landscape shows the clints and grykes that are a characteristic feature of limestone scenery. The grykes are the deep fissures, caused by the erosion of joints in the limestone, which criss-cross the pavement. The clints are the separated blocks of rock that remain. Grykes are often inhabited by shade-loving plants. Photographed in September, near Malham in the Yorkshire Dales National Park, UK.

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