https://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&feed=atom&action=historyHydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences - Revision history2024-03-29T00:58:06ZRevision history for this page on the wikiMediaWiki 1.41.0https://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&diff=25645&oldid=prevDbk: Protected "Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences" ([Edit=Allow only administrators] (indefinite) [Move=Allow only administrators] (indefinite)) [cascading]2016-02-18T08:32:19Z<p>Protected "<a href="/index.php/Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences" title="Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences">Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences</a>" ([Edit=Allow only administrators] (indefinite) [Move=Allow only administrators] (indefinite)) [cascading]</p>
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</td></tr></table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&diff=25644&oldid=prevDbk: Removed protection from "Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences"2016-02-18T08:32:12Z<p>Removed protection from "<a href="/index.php/Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences" title="Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences">Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences</a>"</p>
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</td></tr></table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&diff=25266&oldid=prevDbk: Protected "Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences" ([Edit=Allow only administrators] (indefinite) [Move=Allow only administrators] (indefinite)) [cascading]2016-02-11T14:19:16Z<p>Protected "<a href="/index.php/Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences" title="Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences">Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences</a>" ([Edit=Allow only administrators] (indefinite) [Move=Allow only administrators] (indefinite)) [cascading]</p>
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</td></tr></table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&diff=25265&oldid=prevDbk: Removed protection from "Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences"2016-02-11T14:18:57Z<p>Removed protection from "<a href="/index.php/Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences" title="Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences">Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences</a>"</p>
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</td></tr></table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&diff=9616&oldid=prevDbk: Protected "Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences" ([Edit=Allow only administrators] (indefinite) [Move=Allow only administrators] (indefinite)) [cascading]2015-05-05T15:30:33Z<p>Protected "<a href="/index.php/Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences" title="Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences">Hydrogeology of Wales: The Old Red Sandstone aquifer - groundwater occurrences</a>" ([Edit=Allow only administrators] (indefinite) [Move=Allow only administrators] (indefinite)) [cascading]</p>
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<td colspan="1" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 15:30, 5 May 2015</td>
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</td></tr></table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&diff=6732&oldid=prevDbk at 15:59, 29 January 20152015-01-29T15:59:19Z<p></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 15:59, 29 January 2015</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The Old Red Sandstone waters are moderately fresh and tend to have low conductivities compared with other British groundwaters reflecting shallow and rapid groundwater circulation in the aquifer. Most groundwaters are either at or approaching saturation with respect to both calcite and dolomite.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The Old Red Sandstone waters are moderately fresh and tend to have low conductivities compared with other British groundwaters reflecting shallow and rapid groundwater circulation in the aquifer. Most groundwaters are either at or approaching saturation with respect to both calcite and dolomite.</div></td></tr>
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<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">{{HOWpages}}</ins></div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[Category:Hydrogeology of Wales| 014]]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[[Category:Hydrogeology of Wales| 014]]</div></td></tr>
</table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&diff=3795&oldid=prevDbk at 07:52, 20 May 20142014-05-20T07:52:10Z<p></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 07:52, 20 May 2014</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Nevertheless, the Devonian-age Old Red Sandstone is arguably the most important aquifer in Wales. The main outcrop of the aquifer contains at least 2650 abstractions and over 80 per cent of these are licensed for groundwater abstractions (i.e. >20 m<sup>3</sup> d<sup>-1</sup>), either boreholes, wells or springs, the majority for domestic, agricultural and industrial supply ([[Hydrogeology of Wales: References|'''Moreau et al., 2004''']]). Of the licences granted for agricultural purposes a significant proportion are for spray irrigation. In addition, there are over 2300 private water supplies from Old Red Sandstone strata that are registered with local government, although many small sources such as supplies to single dwellings remain unregistered. At least 50 per cent of the known private supplies are for domestic use only.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Nevertheless, the Devonian-age Old Red Sandstone is arguably the most important aquifer in Wales. The main outcrop of the aquifer contains at least 2650 abstractions and over 80 per cent of these are licensed for groundwater abstractions (i.e. >20 m<sup>3</sup> d<sup>-1</sup>), either boreholes, wells or springs, the majority for domestic, agricultural and industrial supply ([[Hydrogeology of Wales: References|'''Moreau et al., 2004''']]). Of the licences granted for agricultural purposes a significant proportion are for spray irrigation. In addition, there are over 2300 private water supplies from Old Red Sandstone strata that are registered with local government, although many small sources such as supplies to single dwellings remain unregistered. At least 50 per cent of the known private supplies are for domestic use only.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[Image:P802423.jpg|thumb|300px|Holy Spring at Maen-Du, north of Brecon Cathedral. <del style="font-weight: bold; text-decoration: none;">[https://bgsintranet/asset-bank/action/viewFullSizedImage?id=390741&size=1000 </del>P802423.<del style="font-weight: bold; text-decoration: none;">]</del>]]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[Image:P802423.jpg|thumb|300px|Holy Spring at Maen-Du, north of Brecon Cathedral. P802423.]]</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The Brownstones Formation and the Senni Beds are the best yielding formations in the Old Red Sandstone because the more transmissive sandstone of the Upper Old Red Sandstone are locally poorly represented. There are some large springs at the base of the St Maughans Sandstone. Among the sacred springs located north of Brecon is that at Maen-Du [SO 0390 2963] that formerly supplied Brecon Castle ('''Plate P802423'''). Most of the waters from the Old Red Sandstone are hard ([[Hydrogeology of Wales: References|'''Jones et al., 2000''']]). The hard water favours tufa formation and fractures are commonly lined with travertine in cuttings or excavations.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The Brownstones Formation and the Senni Beds are the best yielding formations in the Old Red Sandstone because the more transmissive sandstone of the Upper Old Red Sandstone are locally poorly represented. There are some large springs at the base of the St Maughans Sandstone. Among the sacred springs located north of Brecon is that at Maen-Du [SO 0390 2963] that formerly supplied Brecon Castle ('''Plate P802423'''). Most of the waters from the Old Red Sandstone are hard ([[Hydrogeology of Wales: References|'''Jones et al., 2000''']]). The hard water favours tufa formation and fractures are commonly lined with travertine in cuttings or excavations.</div></td></tr>
</table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&diff=3658&oldid=prevDbk at 14:41, 19 May 20142014-05-19T14:41:12Z<p></p>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Nevertheless, the Devonian-age Old Red Sandstone is arguably the most important aquifer in Wales. The main outcrop of the aquifer contains at least 2650 abstractions and over 80 per cent of these are licensed for groundwater abstractions (i.e. >20 m<sup>3</sup> d<sup>-1</sup>), either boreholes, wells or springs, the majority for domestic, agricultural and industrial supply ([[Hydrogeology of Wales: References|'''Moreau et al., 2004''']]). Of the licences granted for agricultural purposes a significant proportion are for spray irrigation. In addition, there are over 2300 private water supplies from Old Red Sandstone strata that are registered with local government, although many small sources such as supplies to single dwellings remain unregistered. At least 50 per cent of the known private supplies are for domestic use only.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Nevertheless, the Devonian-age Old Red Sandstone is arguably the most important aquifer in Wales. The main outcrop of the aquifer contains at least 2650 abstractions and over 80 per cent of these are licensed for groundwater abstractions (i.e. >20 m<sup>3</sup> d<sup>-1</sup>), either boreholes, wells or springs, the majority for domestic, agricultural and industrial supply ([[Hydrogeology of Wales: References|'''Moreau et al., 2004''']]). Of the licences granted for agricultural purposes a significant proportion are for spray irrigation. In addition, there are over 2300 private water supplies from Old Red Sandstone strata that are registered with local government, although many small sources such as supplies to single dwellings remain unregistered. At least 50 per cent of the known private supplies are for domestic use only.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">{| class="wikitable" width="100pt" style="margin-left</del>:<del style="font-weight: bold; text-decoration: none;">40px; margin-right:0px; margin-bottom:10px; float:right; text-align:left;"</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">[[Image</ins>:<ins style="font-weight: bold; text-decoration: none;">P802423.jpg</ins>|<ins style="font-weight: bold; text-decoration: none;">thumb</ins>|<ins style="font-weight: bold; text-decoration: none;">300px</ins>|Holy Spring at Maen-Du, north of Brecon Cathedral. [https://bgsintranet/asset-bank/action/viewFullSizedImage?id=390741&size=1000 P802423.]<ins style="font-weight: bold; text-decoration: none;">]]</ins></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| <del style="font-weight: bold; text-decoration: none;"><img src="https://bgsintranet/asset-bank/action/directLinkImage?assetId=390741&width=300&height=150"></del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>|<del style="font-weight: bold; text-decoration: none;">-</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>| Holy Spring at Maen-Du, north of Brecon Cathedral. [https://bgsintranet/asset-bank/action/viewFullSizedImage?id=390741&size=1000 P802423.]</div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">|}</del></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The Brownstones Formation and the Senni Beds are the best yielding formations in the Old Red Sandstone because the more transmissive sandstone of the Upper Old Red Sandstone are locally poorly represented. There are some large springs at the base of the St Maughans Sandstone. Among the sacred springs located north of Brecon is that at Maen-Du [SO 0390 2963] that formerly supplied Brecon Castle ('''Plate P802423'''). Most of the waters from the Old Red Sandstone are hard ([[Hydrogeology of Wales: References|'''Jones et al., 2000''']]). The hard water favours tufa formation and fractures are commonly lined with travertine in cuttings or excavations.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The Brownstones Formation and the Senni Beds are the best yielding formations in the Old Red Sandstone because the more transmissive sandstone of the Upper Old Red Sandstone are locally poorly represented. There are some large springs at the base of the St Maughans Sandstone. Among the sacred springs located north of Brecon is that at Maen-Du [SO 0390 2963] that formerly supplied Brecon Castle ('''Plate P802423'''). Most of the waters from the Old Red Sandstone are hard ([[Hydrogeology of Wales: References|'''Jones et al., 2000''']]). The hard water favours tufa formation and fractures are commonly lined with travertine in cuttings or excavations.</div></td></tr>
</table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&diff=1195&oldid=prevDbk at 09:21, 23 September 20132013-09-23T09:21:35Z<p></p>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>| Holy Spring at Maen-Du, north of Brecon Cathedral. [https://bgsintranet/asset-bank/action/viewFullSizedImage?id=390741&size=1000 P802423.]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>| Holy Spring at Maen-Du, north of Brecon Cathedral. [https://bgsintranet/asset-bank/action/viewFullSizedImage?id=390741&size=1000 P802423.]</div></td></tr>
</table>Dbkhttps://earthwise.bgs.ac.uk/index.php?title=Hydrogeology_of_Wales:_The_Old_Red_Sandstone_aquifer_-_groundwater_occurrences&diff=1194&oldid=prevDbk at 09:21, 23 September 20132013-09-23T09:21:19Z<p></p>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>| Holy Spring at Maen-Du, north of Brecon Cathedral. [https://bgsintranet/asset-bank/action/viewFullSizedImage?id=390741&size=1000 P802423.]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>| Holy Spring at Maen-Du, north of Brecon Cathedral. [https://bgsintranet/asset-bank/action/viewFullSizedImage?id=390741&size=1000 P802423.]</div></td></tr>
</table>Dbk