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CLIMATE, VEGETATION AND MAN
IN THE HUDDERSFIELD DISTRICT
BY T.W. WOODHEAD

12. PLANT ASSOCIATIONS IN 1900

The plant associations of the present day are shown on Model 10. Recent times have been marked by extensive reduction of forest coincident with great increase in population, cultivation and industrial development in the area. Three main groups of plant associations are distinguished:- Cultivation; Woodland, and Moorland associations. Aquatic associations are meagerly developed in the area, being confined to river sides, and artificial sheets of water as canals, reservoirs, and to small lakes in parklands.

1. Cultivation: - Lowland cultivation, from 150 feet to 600 feet, including the river plains and lower slopes of the spurs, with arms extending up the narrow valleys. upland Cultivation, from 600 feet to 1,200 feet, including the spurs and foothills. In both zones arable land is limited in extent (reaching to higher levels on the Coal Measures than on the grits) the farms being employed mainly in the production of milk and meat.

2. Woodland: - Alder-Willow swamps, greatly reduced by draining, are confined to the smaller valleys and the neighbourhood of disused and silting-up reservoirs. Moist-Oak woods and parklands, chiefly in the area of lowland cultivation, especially on the shales of the Lower and Middle Coal Measures. Intermediate Oak Woods, especially on the naturally drained shaley slopes of the Coal Measures. Oak-Birth-Heath Woods on the sandstones and stoney slopes of the spurs, and approaching the summit plateau.

3. Moorland: - Grass-Heath and Calluna Moor on the sites of former Oak-Birth-Heath Woods, best developed on the shallow soils over the sandstones, especially on the terraces of the Millstone Grits, though frequent on the sandstones of the Lower and Middle Coal Measures. On the steep and stoney slopes of the higher valleys the bracken is extending and forms unbroken sheets for miles. Cottongrass Moss characterises the wet and cold summit plateau where thick beds of cottongrass peat cover the ground, its principal associates being the Crowberry and Cloudberry. There are frequent "Rushbeds" but Sphagnum Bogs are scarce and of small extent. Over large areas the peat is breaking down, and on the drying retrogressive peat hags the cottongrass is giving way to bilberry, the latter, along with the cowberry forming extensive "edges" along the better drained fringe of the cottongrass moss, and merging into the grass-heath and bracken on the slopes.

A comparison of the models shows how extensively the forest has been replaced, on the one hand by moorland (cottongrass, moss, grass and Calluna Heath) and on the other hand by farmland, chiefly pasture. At the lower levels the more extensive remnants of the forest are confined largely to steep and stone escarpments of little economic value, or are enclosed as parklands. As we approach the summit plateau, the numerous areas of native grassheath pick out a tension belt between the lowland cultivation and the peat moss on the summit. This tension belt indicates the limit of profitable cultivation, notwithstanding its proximity to a large industrial population. Over considerable areas the cottongrass is degenerating and exposing rocky subsoil on which it originally developed, here re-invasion is going on, not by plants of the moss, but by wiry grasses from the grass-heath. This is well seen in the photographs of local vegetation in the entrance hall, adjoining Room 3, Botany.

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