Papers And Notes On the Glacial Geology of Great Britain And Ireland
Papers And Notes On the Glacial Geology of Great Britain And Ireland
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Above here are rock surfaces that are unglaciated. Immediately south of Accrington is a deep cutting through drift, in which I see numerous large projecting boulders of sandstone. This looks like a section through a moraine. More sandstone boulders appear east of Accrington, but here they are seen to bo in a drift resting upon shale. Non-glaciated rocks also occur to the eastward, and I see rock under the drift at Rose Grove which does not seem to be a moraine.
In fact I do not think the glacie...r came as far south as Burnley. There is deep drift at Burnley Barracks. Just below Brierfield Station is a mass of drift containing limestone pebbles, but north of the station rock is seen under the drift.
Digitized by LjOOQIC MANCHESTER AND VICINITY 281 From Colne I drive north-east to Laneshaw Bridge and to the moors, on the boundary line between Yorkshire and Lancashire. At the Yorkshire tongue into Lancashire is a sandstone quarry exposing 25 feet of drift on top of the rock. The drift consists of horizontally stratified sand overlaid by till.
What to read after Papers And Notes On the Glacial Geology of Great Britain And Ireland?
You can find similar books in the "Read Also" column, or choose other free books by Henry Carvill Lewis to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Above here are rock surfaces that are unglaciated. Immediately south of Accrington is a deep cutting through drift, in which I see numerous large projecting boulders of sandstone. This looks like a section through a moraine. More sandstone boulders appear east of Accrington, but here they are seen to bo in a drift resting upon shale. Non-glaciated rocks also occur to the eastward, and I see rock under the drift at Rose Grove which does not seem to be a moraine.
In fact I do not think the glacie...r came as far south as Burnley. There is deep drift at Burnley Barracks. Just below Brierfield Station is a mass of drift containing limestone pebbles, but north of the station rock is seen under the drift.
Digitized by LjOOQIC MANCHESTER AND VICINITY 281 From Colne I drive north-east to Laneshaw Bridge and to the moors, on the boundary line between Yorkshire and Lancashire. At the Yorkshire tongue into Lancashire is a sandstone quarry exposing 25 feet of drift on top of the rock. The drift consists of horizontally stratified sand overlaid by till.
What to read after Papers And Notes On the Glacial Geology of Great Britain And Ireland?
You can find similar books in the "Read Also" column, or choose other free books by Henry Carvill Lewis to read onlineMoreLess
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