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Statements

Subject Item
dbr:Hobbs_Quarry_SSSI,_Shepton_Mallet
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rdfs:label
Hobbs Quarry SSSI, Shepton Mallet Hobbs Quarry SSSI (Shepton Mallet)
rdfs:comment
Hobbs Quarry (grid reference ST622446) is a 0.5 hectare geological Site of Special Scientific Interest near Shepton Mallet on the Mendip Hills in Somerset, notified in 1984. This disused quarry, which now forms the back of a builders merchants yard, is a Geological Conservation Review Site which demonstrates early Jurassic transgression, with steeply-dipping Carboniferous Limestone being overlain by flatter-lying massive limestones (of early Jurassic age) known as the Downside Stone. Hobbs Quarry ist ein früherer Steinbruch eine 0,5 Hektar große geologisch bedeutsame Site of Special Scientific Interest bei Shepton Mallet in den Mendip Hills in Somerset, bekanntgemacht 1984. Der aufgelassene Steinbruch, der sich im hinteren Teil des Betriebshofes eines Bauunternehmens befindet, ist eine Stätte, an der die Transgression in der frühen Jura deutlich wird. Steil abfallender Carbon-Kalkstein ist überlagert von flachliegenden massivem Kalkstein, der als Downside Stone bekannt ist.
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Hobbs Quarry
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Hobbs Quarry
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51.19936 -2.54238
dbo:abstract
Hobbs Quarry (grid reference ST622446) is a 0.5 hectare geological Site of Special Scientific Interest near Shepton Mallet on the Mendip Hills in Somerset, notified in 1984. This disused quarry, which now forms the back of a builders merchants yard, is a Geological Conservation Review Site which demonstrates early Jurassic transgression, with steeply-dipping Carboniferous Limestone being overlain by flatter-lying massive limestones (of early Jurassic age) known as the Downside Stone. Hobbs Quarry ist ein früherer Steinbruch eine 0,5 Hektar große geologisch bedeutsame Site of Special Scientific Interest bei Shepton Mallet in den Mendip Hills in Somerset, bekanntgemacht 1984. Der aufgelassene Steinbruch, der sich im hinteren Teil des Betriebshofes eines Bauunternehmens befindet, ist eine Stätte, an der die Transgression in der frühen Jura deutlich wird. Steil abfallender Carbon-Kalkstein ist überlagert von flachliegenden massivem Kalkstein, der als Downside Stone bekannt ist.
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Somerset
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Somerset
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Geological
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