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GEOLOGY The rocks consist of alternating bands of shale and sandstone, with shales generally dominating. A thin band of coal
runs through the upper part of Buck Wood.
LANDSCAPE A small stream runs
down the eastern edge of the wood. This is a tributary of the Meers Brook,
the main watercourse through the Gleadless Valley. Thin dry 'acidic soils' occur over sandstone, particularly on higher ground, as well as over shales on steep slopes. The depth and acidity of the soils is strongly affected by slope, the thinnest and most acid soils being found on the most steeply sloping sites. Neutral soils are mainly found on flat to moderately sloping ground over shales. They vary in depth and clay content and also from dry to seasonally wet, the wettest areas being on stream banks, in valley bottoms and by springs and wet nutrient rich areas known as flushes. Waterlogged soils
are found in association with streams, springs and flushes. They occur
mainly over shale, particularly where this meets sandstone strata. These
conditions occur on the valley slopes as well as in the valley bottoms
and by streams. Some of the springs are wet all year round but the flushes
are more seasonal. |