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GEOLOGY The rocks consist
of alternating bands of shale and sandstone, with shales generally dominating.
A small tributary of the Meers Brook runs just within the western boundary of the wood. The north-eastern limb of the woodland occupies a small, narrow, dry valley. SOILS 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, with the thinnest and most acid soils being found on steeply sloping sites. Deeper and less acidic soils occur on flatter ground, even over sandstone. 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. |