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environmental statement - Rotherham's Online Application for ...

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Flooding via overland flow from adjacent land; and<br />

Flooding from surface water drainage.<br />

FLOODING FROM GROUNDWATER<br />

13.29 The proposed development site is underlain by Coal Measures strata of<br />

Carboniferous age consisting of inter-bedded sandstone, siltstones and<br />

mudstones with associated coal horizons. It is understood that overlying<br />

drift deposits are relatively thin and laterally inconsistent. The<br />

Mexborough Rock, one of the more significant sandstone units in the Coal<br />

Measures, outcrops in the Ulley area. Coal Measures sandstone typically<br />

<strong>for</strong>m poor aquifers with limited potential <strong>for</strong> groundwater storage or<br />

conveyance.<br />

13.30 Numerous springs and issues are present in the vicinity of the proposed<br />

development site suggesting the presence of shallow groundwater. Issues<br />

present within the site itself which are situated at a significantly higher<br />

elevation and <strong>for</strong>m part of the headwaters of Ulley Brook, appear to<br />

represent the outfall from field drainage systems that extend eastwards.<br />

There is no direct evidence to suggest the presence of shallow<br />

groundwater beneath the site. The occurrence of springs close to the<br />

route of the Ulley Brook e.g. directly due north of Ulley Village, is likely to<br />

be a consequence of near surface variation in drift deposits rather than<br />

emergence of deeper groundwater.<br />

13.31 Other springs in the area are located at a range of surface elevations with<br />

no clear trend. This is typical of Coal Measures derived groundwater<br />

systems where surface emergence of groundwater is generally related to<br />

the random distribution of geological discontinuities or man-made<br />

structures. It is considered likely that limited groundwater resources are<br />

present in Coal Measures sandstones beneath the site.<br />

13.32 The proposed development site incorporates higher ground than the<br />

surrounding area. The site is not a natural discharge point <strong>for</strong><br />

groundwater. Due to the topography of the site, any groundwater<br />

emerging at surface, either as a consequence of intensive recharge or<br />

groundwater flow from surrounding areas would drain rapidly to the<br />

surface water drainage channels and away from the site. On this basis it<br />

is considered that the site is not at risk of groundwater flooding.<br />

FLOODING VIA OVERLAND FLOW FROM ADJACENT LAND<br />

13.33 The surrounding land is all agricultural land with well established drainage<br />

pathways to the field drainage channels connected to Ulley Brook.<br />

Surface runoff from higher ground to the south of the southern part of the<br />

site currently drains into the site towards the southern branch of the brook.<br />

There is currently no evidence to suggest that such overland flow results in<br />

flooding of land within the site and hence no basis <strong>for</strong> assuming that there<br />

is any risk of flooding associated with overland flow.<br />

285<br />

Penny Hill Wind Farm<br />

Environmental Statement

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