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

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13.21 A Coal Authority Mining Report <strong>for</strong> the site identifies that the study area is<br />

within the likely zone of influence on the surface from workings in seven<br />

seams of coal at depths of between 230m and 820m. The last date of<br />

working is given as 1987 and there<strong>for</strong>e any ground movement from the<br />

workings should have ceased. There are no mine entries shown within the<br />

site boundary.<br />

13.22 The Coal Authority has not received a damage notice or claim <strong>for</strong> the<br />

property since 1 January 1984.<br />

TOPOGRAPHY<br />

13.23 The study area occupies an area of hilly topography with elevations<br />

ranging from 65m to 110m above Ordnance Datum (OD).<br />

ASSESSMENT OF EFFECTS<br />

GROUND CONDITIONS<br />

13.24 The possible presence of sandy or gravelly alluvium along the floors of the<br />

two stream courses described above, in combination with the<br />

characteristic steep valley sides of the site, could cause local instability in<br />

the <strong>for</strong>m of minor land slippage or soil creep. However features <strong>for</strong>med by<br />

such processes were not observed during previous surveys.<br />

13.25 Head deposits are commonly present on slopes or on the floors of valleys<br />

although they have not been indicated on the geological plan. They are<br />

variable in composition and are typically poorly stratified and poorly sorted.<br />

They may contain shear planes, which can be reactivated when undercut<br />

by excavations.<br />

13.26 A characteristic of the Upper Pennine Middle Coal measures mudstone is<br />

that they commonly weather to a sticky, yellow brown clay, which may<br />

exhibit shrink swell properties due to changes in soil moisture contents<br />

which can potentially cause structural damage.<br />

13.27 Faults have been mapped across the site as described above. The<br />

geological faults within this area are of ancient origin and are today mainly<br />

inactive. However they must still be regarded as planes of weakness<br />

whereby mining induced subsidence and severe subsidence effects may<br />

commonly be concentrated along them. The depths of previous old mine<br />

workings and the absence of damage notices or claims since 1984 within<br />

the scoping boundary indicate future ground movements are very unlikely.<br />

FLOOD RISK ASSESSMENT<br />

13.28 PPS25 suggests that consideration should be given to site vulnerability to<br />

other potential sources of flooding including:<br />

Flooding from groundwater;<br />

284<br />

Penny Hill Wind Farm<br />

Environmental Statement

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