Template:Featured article1 - Revision history

http://earthwise.bgs.ac.uk/index.php?action=history&feed=atom&title=Template%3AFeatured_article1 Template:Featured article1 - Revision history 2026-04-24T07:11:26Z Revision history for this page on the wiki MediaWiki 1.42.3 http://earthwise.bgs.ac.uk/index.php?title=Template:Featured_article1&diff=44885&oldid=prev Dbk at 08:54, 6 January 2020 2020-01-06T08:54:49Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 09:54, 6 January 2020</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</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>[[Image:P894510.jpg|frameless| right|200px| ]]</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>[[Image:P894510.jpg|frameless| right|200px| ]]</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>'''Bristol and Gloucester <del style="font-weight: bold; text-decoration: none;">regioal </del>guide'''<br></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>'''Bristol and Gloucester <ins style="font-weight: bold; text-decoration: none;">regional </ins>guide'''<br></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 area dealt with comprises the Cotswolds and the Severn Estuary region, and includes the greater part of the counties of Avon, Gloucestershire and Somerset (excluding west Somerset); also, for geological continuity, small parts of the counties of Gwent, Herefordshire, Worcestershire, Wiltshire and Dorset. Geologically speaking, it is one of the most varied districts of Britain, for, with the exception of the Ordovician and possibly the Permian, there is exposed at the surface every geological system from the Cambrian to the Cretaceous . . . [[Bristol and Gloucester region - an introduction | '''(Read the full article...)''']]</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 area dealt with comprises the Cotswolds and the Severn Estuary region, and includes the greater part of the counties of Avon, Gloucestershire and Somerset (excluding west Somerset); also, for geological continuity, small parts of the counties of Gwent, Herefordshire, Worcestershire, Wiltshire and Dorset. Geologically speaking, it is one of the most varied districts of Britain, for, with the exception of the Ordovician and possibly the Permian, there is exposed at the surface every geological system from the Cambrian to the Cretaceous . . . [[Bristol and Gloucester region - an introduction | '''(Read the full article...)''']]</div></td></tr> </table>

Dbk http://earthwise.bgs.ac.uk/index.php?title=Template:Featured_article1&diff=44739&oldid=prev Dbk at 08:41, 11 December 2019 2019-12-11T08:41:53Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 09:41, 11 December 2019</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</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>[[Image:P894510.jpg|frameless| right|200px| ]]</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>[[Image:P894510.jpg|frameless| right|200px| ]]</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>'''Bristol and Gloucester regioal guide <del style="font-weight: bold; text-decoration: none;">- </del>'''<br></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>'''Bristol and Gloucester regioal guide'''<br></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 area dealt with comprises the Cotswolds and the Severn Estuary region, and includes the greater part of the counties of Avon, Gloucestershire and Somerset (excluding west Somerset); also, for geological continuity, small parts of the counties of Gwent, Herefordshire, Worcestershire, Wiltshire and Dorset. Geologically speaking, it is one of the most varied districts of Britain, for, with the exception of the Ordovician and possibly the Permian, there is exposed at the surface every geological system from the Cambrian to the Cretaceous . . . [[Bristol and Gloucester region - an introduction | '''(Read the full article...)''']]</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 area dealt with comprises the Cotswolds and the Severn Estuary region, and includes the greater part of the counties of Avon, Gloucestershire and Somerset (excluding west Somerset); also, for geological continuity, small parts of the counties of Gwent, Herefordshire, Worcestershire, Wiltshire and Dorset. Geologically speaking, it is one of the most varied districts of Britain, for, with the exception of the Ordovician and possibly the Permian, there is exposed at the surface every geological system from the Cambrian to the Cretaceous . . . [[Bristol and Gloucester region - an introduction | '''(Read the full article...)''']]</div></td></tr> </table>

Dbk http://earthwise.bgs.ac.uk/index.php?title=Template:Featured_article1&diff=44738&oldid=prev Dbk at 08:41, 11 December 2019 2019-12-11T08:41:43Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 09:41, 11 December 2019</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</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:<del style="font-weight: bold; text-decoration: none;">P947780</del>.jpg|frameless| right|200px| ]]</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:<ins style="font-weight: bold; text-decoration: none;">P894510</ins>.jpg|frameless| right|200px| ]]</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;">The geology of Northern Ireland</del>'''<br></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;">Bristol and Gloucester regioal guide - </ins>'''<br></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;">On a global scale Northern Ireland</del>, <del style="font-weight: bold; text-decoration: none;">despite being a mere 0.00001% </del>of the <del style="font-weight: bold; text-decoration: none;">land area </del>of <del style="font-weight: bold; text-decoration: none;">planet Earth</del>, <del style="font-weight: bold; text-decoration: none;">presents an opportunity to study an almost unparalleled variety of geology in such a </del>small <del style="font-weight: bold; text-decoration: none;">area. The diverse ages </del>of the <del style="font-weight: bold; text-decoration: none;">rocks present in Northern Ireland </del>is <del style="font-weight: bold; text-decoration: none;">illustrated in these articles by </del>the <del style="font-weight: bold; text-decoration: none;">[[Geology_of_Northern_Ireland:_our_natural_foundation|contents menu]]. Their stratigraphical record commences in </del>the <del style="font-weight: bold; text-decoration: none;">Mesoproterozoic and includes representatives in all </del>of the <del style="font-weight: bold; text-decoration: none;">systems up to </del>and <del style="font-weight: bold; text-decoration: none;">including </del>the <del style="font-weight: bold; text-decoration: none;">Palaeogene. If </del>the Cambrian <del style="font-weight: bold; text-decoration: none;">age attributed </del>to <del style="font-weight: bold; text-decoration: none;">upper parts of </del>the <del style="font-weight: bold; text-decoration: none;">Dalradian Supergroup in Scotland is substantiated then it is likely that their correlatives in Northern Ireland will fall within that system </del>. . . [[<del style="font-weight: bold; text-decoration: none;">Introduction_to_the_geology_of_Northern_Ireland </del>| '''(Read the full article...)''']]</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;">The area dealt with comprises the Cotswolds and the Severn Estuary region</ins>, <ins style="font-weight: bold; text-decoration: none;">and includes the greater part </ins>of the <ins style="font-weight: bold; text-decoration: none;">counties </ins>of <ins style="font-weight: bold; text-decoration: none;">Avon, Gloucestershire and Somerset (excluding west Somerset); also, for geological continuity</ins>, small <ins style="font-weight: bold; text-decoration: none;">parts </ins>of the <ins style="font-weight: bold; text-decoration: none;">counties of Gwent, Herefordshire, Worcestershire, Wiltshire and Dorset. Geologically speaking, it </ins>is <ins style="font-weight: bold; text-decoration: none;">one of </ins>the <ins style="font-weight: bold; text-decoration: none;">most varied districts of Britain, for, with </ins>the <ins style="font-weight: bold; text-decoration: none;">exception </ins>of the <ins style="font-weight: bold; text-decoration: none;">Ordovician </ins>and <ins style="font-weight: bold; text-decoration: none;">possibly the Permian, there is exposed at </ins>the <ins style="font-weight: bold; text-decoration: none;">surface every geological system from </ins>the Cambrian to the <ins style="font-weight: bold; text-decoration: none;">Cretaceous </ins>. . . [[<ins style="font-weight: bold; text-decoration: none;">Bristol and Gloucester region - an introduction </ins>| '''(Read the full article...)''']]</div></td></tr> </table>

Dbk http://earthwise.bgs.ac.uk/index.php?title=Template:Featured_article1&diff=32709&oldid=prev Dbk at 15:01, 26 September 2017 2017-09-26T15:01:39Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 16:01, 26 September 2017</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</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:P947780.jpg|frameless| right|<del style="font-weight: bold; text-decoration: none;">300px</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:P947780.jpg|frameless| right|<ins style="font-weight: bold; text-decoration: none;">200px</ins>| ]]</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;"><div>'''The geology of Northern Ireland'''<br></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 geology of Northern Ireland'''<br></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>On a global scale Northern Ireland, despite being a mere 0.00001% of the land area of planet Earth, presents an opportunity to study an almost unparalleled variety of geology in such a small area. The diverse ages of the rocks present in Northern Ireland is illustrated in these articles by the [[Geology_of_Northern_Ireland:_our_natural_foundation|contents menu]]. Their stratigraphical record commences in the Mesoproterozoic and includes representatives in all of the systems up to and including the Palaeogene. If the Cambrian age attributed to upper parts of the Dalradian Supergroup in Scotland is substantiated then it is likely that their correlatives in Northern Ireland will fall within that system . . . [[Introduction_to_the_geology_of_Northern_Ireland | '''(Read the full article...)''']]</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>On a global scale Northern Ireland, despite being a mere 0.00001% of the land area of planet Earth, presents an opportunity to study an almost unparalleled variety of geology in such a small area. The diverse ages of the rocks present in Northern Ireland is illustrated in these articles by the [[Geology_of_Northern_Ireland:_our_natural_foundation|contents menu]]. Their stratigraphical record commences in the Mesoproterozoic and includes representatives in all of the systems up to and including the Palaeogene. If the Cambrian age attributed to upper parts of the Dalradian Supergroup in Scotland is substantiated then it is likely that their correlatives in Northern Ireland will fall within that system . . . [[Introduction_to_the_geology_of_Northern_Ireland | '''(Read the full article...)''']]</div></td></tr> </table>

Dbk http://earthwise.bgs.ac.uk/index.php?title=Template:Featured_article1&diff=32708&oldid=prev Dbk at 15:01, 26 September 2017 2017-09-26T15:01:27Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 16:01, 26 September 2017</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</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:<del style="font-weight: bold; text-decoration: none;">P929859</del>.jpg|frameless| right|300px| ]]</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:<ins style="font-weight: bold; text-decoration: none;">P947780</ins>.jpg|frameless| right|300px| ]]</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;"><div>'''The geology of Northern Ireland'''<br></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 geology of Northern Ireland'''<br></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>On a global scale Northern Ireland, despite being a mere 0.00001% of the land area of planet Earth, presents an opportunity to study an almost unparalleled variety of geology in such a small area. The diverse ages of the rocks present in Northern Ireland is illustrated in these articles by the [[Geology_of_Northern_Ireland:_our_natural_foundation|contents menu]]. Their stratigraphical record commences in the Mesoproterozoic and includes representatives in all of the systems up to and including the Palaeogene. If the Cambrian age attributed to upper parts of the Dalradian Supergroup in Scotland is substantiated then it is likely that their correlatives in Northern Ireland will fall within that system . . . [[Introduction_to_the_geology_of_Northern_Ireland | '''(Read the full article...)''']]</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>On a global scale Northern Ireland, despite being a mere 0.00001% of the land area of planet Earth, presents an opportunity to study an almost unparalleled variety of geology in such a small area. The diverse ages of the rocks present in Northern Ireland is illustrated in these articles by the [[Geology_of_Northern_Ireland:_our_natural_foundation|contents menu]]. Their stratigraphical record commences in the Mesoproterozoic and includes representatives in all of the systems up to and including the Palaeogene. If the Cambrian age attributed to upper parts of the Dalradian Supergroup in Scotland is substantiated then it is likely that their correlatives in Northern Ireland will fall within that system . . . [[Introduction_to_the_geology_of_Northern_Ireland | '''(Read the full article...)''']]</div></td></tr> </table>

Dbk http://earthwise.bgs.ac.uk/index.php?title=Template:Featured_article1&diff=32707&oldid=prev Dbk at 15:00, 26 September 2017 2017-09-26T15:00:18Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 16:00, 26 September 2017</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</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>[[Image:P929859.jpg|frameless| right|300px| ]]</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>[[Image:P929859.jpg|frameless| right|300px| ]]</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;">London Region Atlas </del>of <del style="font-weight: bold; text-decoration: none;">Topsoil Geochemistry</del>'''<br></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;">The geology </ins>of <ins style="font-weight: bold; text-decoration: none;">Northern Ireland</ins>'''<br></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;">The simplified geological map used in this atlas</del>, <del style="font-weight: bold; text-decoration: none;">and in particular for creating </del>the <del style="font-weight: bold; text-decoration: none;">soil parent material (PM) classes</del>, <del style="font-weight: bold; text-decoration: none;">is based on the classification used for radon mapping </del>in <del style="font-weight: bold; text-decoration: none;">England and Wales (Miles and Appleton, 2005)</del>. The <del style="font-weight: bold; text-decoration: none;">area </del>is <del style="font-weight: bold; text-decoration: none;">underlain </del>by <del style="font-weight: bold; text-decoration: none;">Cretaceous </del>and Palaeogene <del style="font-weight: bold; text-decoration: none;">bedrock, which is covered in some areas by Quaternary superficial deposits</del>. <del style="font-weight: bold; text-decoration: none;">Artificial ground is not used as a soil PM class, because spatial information on </del>the <del style="font-weight: bold; text-decoration: none;">distribution </del>of <del style="font-weight: bold; text-decoration: none;">artificial ground </del>in <del style="font-weight: bold; text-decoration: none;">urban areas </del>in <del style="font-weight: bold; text-decoration: none;">the UK is incomplete</del>. <del style="font-weight: bold; text-decoration: none;">Parent material classes are summarised in Table 2 with an indication of the number of topsoil results associated with each class</del>. . <del style="font-weight: bold; text-decoration: none;"> </del>[[<del style="font-weight: bold; text-decoration: none;">London Atlas: Geology </del>| '''(Read the full article...)''']]</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;">On a global scale Northern Ireland</ins>, <ins style="font-weight: bold; text-decoration: none;">despite being a mere 0.00001% of </ins>the <ins style="font-weight: bold; text-decoration: none;">land area of planet Earth</ins>, <ins style="font-weight: bold; text-decoration: none;">presents an opportunity to study an almost unparalleled variety of geology </ins>in <ins style="font-weight: bold; text-decoration: none;">such a small area</ins>. The <ins style="font-weight: bold; text-decoration: none;">diverse ages of the rocks present in Northern Ireland </ins>is <ins style="font-weight: bold; text-decoration: none;">illustrated in these articles </ins>by <ins style="font-weight: bold; text-decoration: none;">the [[Geology_of_Northern_Ireland:_our_natural_foundation|contents menu]]. Their stratigraphical record commences in the Mesoproterozoic and includes representatives in all of the systems up to </ins>and <ins style="font-weight: bold; text-decoration: none;">including the </ins>Palaeogene. <ins style="font-weight: bold; text-decoration: none;">If </ins>the <ins style="font-weight: bold; text-decoration: none;">Cambrian age attributed to upper parts </ins>of <ins style="font-weight: bold; text-decoration: none;">the Dalradian Supergroup </ins>in <ins style="font-weight: bold; text-decoration: none;">Scotland is substantiated then it is likely that their correlatives </ins>in <ins style="font-weight: bold; text-decoration: none;">Northern Ireland will fall within that system </ins>. . . [[<ins style="font-weight: bold; text-decoration: none;">Introduction_to_the_geology_of_Northern_Ireland </ins>| '''(Read the full article...)''']]</div></td></tr> </table>

Dbk http://earthwise.bgs.ac.uk/index.php?title=Template:Featured_article1&diff=31112&oldid=prev Dbk at 11:38, 30 March 2017 2017-03-30T11:38:49Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 12:38, 30 March 2017</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</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:<del style="font-weight: bold; text-decoration: none;">Africa Hgcl Envs</del>.<del style="font-weight: bold; text-decoration: none;">png</del>|frameless| right|300px| ]]</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:<ins style="font-weight: bold; text-decoration: none;">P929859</ins>.<ins style="font-weight: bold; text-decoration: none;">jpg</ins>|frameless| right|300px| ]]</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;">Hydrogeological environments in Africa</del>'''<br></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;">London Region Atlas of Topsoil Geochemistry</ins>'''<br></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;">How </del>and <del style="font-weight: bold; text-decoration: none;">where groundwater occurs depends primarily </del>on <del style="font-weight: bold; text-decoration: none;">geology; geomorphology/weathering; </del>and <del style="font-weight: bold; text-decoration: none;">rainfall </del>(<del style="font-weight: bold; text-decoration: none;">both current </del>and <del style="font-weight: bold; text-decoration: none;">historic</del>). The <del style="font-weight: bold; text-decoration: none;">interaction between these three factors gives rise to complex hydrogeological environments with countless variations </del>in <del style="font-weight: bold; text-decoration: none;">the quantity</del>, <del style="font-weight: bold; text-decoration: none;">quality, ease of access to and renewability of groundwater resources. Developing groundwater resources therefore depends </del>on <del style="font-weight: bold; text-decoration: none;">a good understanding </del>of <del style="font-weight: bold; text-decoration: none;">hydrogeology</del>. <del style="font-weight: bold; text-decoration: none;">Africa has huge diversity </del>in <del style="font-weight: bold; text-decoration: none;">geology, climate and hydrology, and as a result, </del>the <del style="font-weight: bold; text-decoration: none;">hydrogeology </del>of <del style="font-weight: bold; text-decoration: none;">Africa is hugely variable</del>. [[<del style="font-weight: bold; text-decoration: none;">Overview_of_Groundwater_in_Africa </del>| '''(Read the full article...)''']]</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;">The simplified geological map used in this atlas, </ins>and <ins style="font-weight: bold; text-decoration: none;">in particular for creating the soil parent material (PM) classes, is based </ins>on <ins style="font-weight: bold; text-decoration: none;">the classification used for radon mapping in England </ins>and <ins style="font-weight: bold; text-decoration: none;">Wales </ins>(<ins style="font-weight: bold; text-decoration: none;">Miles </ins>and <ins style="font-weight: bold; text-decoration: none;">Appleton, 2005</ins>). The <ins style="font-weight: bold; text-decoration: none;">area is underlain by Cretaceous and Palaeogene bedrock, which is covered </ins>in <ins style="font-weight: bold; text-decoration: none;">some areas by Quaternary superficial deposits. Artificial ground is not used as a soil PM class</ins>, <ins style="font-weight: bold; text-decoration: none;">because spatial information </ins>on <ins style="font-weight: bold; text-decoration: none;">the distribution </ins>of <ins style="font-weight: bold; text-decoration: none;">artificial ground in urban areas in the UK is incomplete</ins>. <ins style="font-weight: bold; text-decoration: none;">Parent material classes are summarised </ins>in <ins style="font-weight: bold; text-decoration: none;">Table 2 with an indication of </ins>the <ins style="font-weight: bold; text-decoration: none;">number </ins>of <ins style="font-weight: bold; text-decoration: none;">topsoil results associated with each class. </ins>. [[<ins style="font-weight: bold; text-decoration: none;">London Atlas: Geology </ins>| '''(Read the full article...)''']]</div></td></tr> </table>

Dbk http://earthwise.bgs.ac.uk/index.php?title=Template:Featured_article1&diff=29444&oldid=prev Dbk at 13:41, 2 August 2016 2016-08-02T13:41:06Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 14:41, 2 August 2016</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</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<del style="font-weight: bold; text-decoration: none;">:File</del>:Africa Hgcl Envs.png|frameless| right|300px| ]]</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:Africa Hgcl Envs.png|frameless| right|300px| ]]</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;"><div>'''Hydrogeological environments in Africa'''<br></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>'''Hydrogeological environments in Africa'''<br></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>How and where groundwater occurs depends primarily on geology; geomorphology/weathering; and rainfall (both current and historic). The interaction between these three factors gives rise to complex hydrogeological environments with countless variations in the quantity, quality, ease of access to and renewability of groundwater resources. Developing groundwater resources therefore depends on a good understanding of hydrogeology. Africa has huge diversity in geology, climate and hydrology, and as a result, the hydrogeology of Africa is hugely variable. [[Overview_of_Groundwater_in_Africa | '''(Read the full article...)''']]</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>How and where groundwater occurs depends primarily on geology; geomorphology/weathering; and rainfall (both current and historic). The interaction between these three factors gives rise to complex hydrogeological environments with countless variations in the quantity, quality, ease of access to and renewability of groundwater resources. Developing groundwater resources therefore depends on a good understanding of hydrogeology. Africa has huge diversity in geology, climate and hydrology, and as a result, the hydrogeology of Africa is hugely variable. [[Overview_of_Groundwater_in_Africa | '''(Read the full article...)''']]</div></td></tr> </table>

Dbk http://earthwise.bgs.ac.uk/index.php?title=Template:Featured_article1&diff=29443&oldid=prev Dbk at 13:40, 2 August 2016 2016-08-02T13:40:48Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 14:40, 2 August 2016</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</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:<del style="font-weight: bold; text-decoration: none;">15028 fig1</del>.<del style="font-weight: bold; text-decoration: none;">jpg</del>|frameless| right|300px| ]]</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:<ins style="font-weight: bold; text-decoration: none;">File:Africa Hgcl Envs</ins>.<ins style="font-weight: bold; text-decoration: none;">png</ins>|frameless| right|300px| ]]</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;">Scotland’s aquifers and groundwater bodies</del>'''<br></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;">Hydrogeological environments in Africa</ins>'''<br></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;">Almost all </del>groundwater <del style="font-weight: bold; text-decoration: none;">starts life as </del>rainfall. <del style="font-weight: bold; text-decoration: none;">Some rain is taken up by plants, some runs over the land surface or through soils </del>to <del style="font-weight: bold; text-decoration: none;">rivers, and some soaks down through the soil into aquifers. Below the water table, all the spaces </del>in the <del style="font-weight: bold; text-decoration: none;">soil or rock are completely filled with water — groundwater (Figure 1). In Scotland</del>, <del style="font-weight: bold; text-decoration: none;">groundwater occurs almost everywhere beneath our feet</del>, and <del style="font-weight: bold; text-decoration: none;">the water table is usually within 10&nbsp;m </del>of <del style="font-weight: bold; text-decoration: none;">the ground surface</del>. <del style="font-weight: bold; text-decoration: none;">As </del>a <del style="font-weight: bold; text-decoration: none;">store </del>of <del style="font-weight: bold; text-decoration: none;">water that can provide a reliable source of water for drinking </del>and <del style="font-weight: bold; text-decoration: none;">other purposes, groundwater is often accessible close to where it is required</del>, and <del style="font-weight: bold; text-decoration: none;">is cheaper to treat than surface water in lochs and/or reservoirs. In rural areas in particular</del>, <del style="font-weight: bold; text-decoration: none;">groundwater </del>is <del style="font-weight: bold; text-decoration: none;">a vital water source, and it plays an important role in Scotland’s economy</del>. [[<del style="font-weight: bold; text-decoration: none;">OR/15/028 Introduction </del>| '''(Read the full article...)''']]</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;">How and where </ins>groundwater <ins style="font-weight: bold; text-decoration: none;">occurs depends primarily on geology; geomorphology/weathering; and </ins>rainfall <ins style="font-weight: bold; text-decoration: none;">(both current and historic)</ins>. <ins style="font-weight: bold; text-decoration: none;">The interaction between these three factors gives rise </ins>to <ins style="font-weight: bold; text-decoration: none;">complex hydrogeological environments with countless variations </ins>in the <ins style="font-weight: bold; text-decoration: none;">quantity</ins>, <ins style="font-weight: bold; text-decoration: none;">quality</ins>, <ins style="font-weight: bold; text-decoration: none;">ease of access to </ins>and <ins style="font-weight: bold; text-decoration: none;">renewability </ins>of <ins style="font-weight: bold; text-decoration: none;">groundwater resources</ins>. <ins style="font-weight: bold; text-decoration: none;">Developing groundwater resources therefore depends on </ins>a <ins style="font-weight: bold; text-decoration: none;">good understanding </ins>of <ins style="font-weight: bold; text-decoration: none;">hydrogeology. Africa has huge diversity in geology, climate </ins>and <ins style="font-weight: bold; text-decoration: none;">hydrology</ins>, and <ins style="font-weight: bold; text-decoration: none;">as a result</ins>, <ins style="font-weight: bold; text-decoration: none;">the hydrogeology of Africa </ins>is <ins style="font-weight: bold; text-decoration: none;">hugely variable</ins>. [[<ins style="font-weight: bold; text-decoration: none;">Overview_of_Groundwater_in_Africa </ins>| '''(Read the full article...)''']]</div></td></tr> </table>

Dbk http://earthwise.bgs.ac.uk/index.php?title=Template:Featured_article1&diff=26684&oldid=prev Dbk at 08:06, 5 April 2016 2016-04-05T08:06:50Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 09:06, 5 April 2016</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</td></tr> <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;">[[Image:15028 fig1.jpg|frameless| right|300px| ]]</ins></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;"><div>'''Scotland’s aquifers and groundwater bodies'''<br></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>'''Scotland’s aquifers and groundwater bodies'''<br></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;"></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;">[[Image:15028 fig1.jpg|frameless| right|300px| ]]</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>Almost all groundwater starts life as rainfall. Some rain is taken up by plants, some runs over the land surface or through soils to rivers, and some soaks down through the soil into aquifers. Below the water table, all the spaces in the soil or rock are completely filled with water — groundwater (Figure 1). In Scotland, groundwater occurs almost everywhere beneath our feet, and the water table is usually within 10&nbsp;m of the ground surface. As a store of water that can provide a reliable source of water for drinking and other purposes, groundwater is often accessible close to where it is required, and is cheaper to treat than surface water in lochs and/or reservoirs. In rural areas in particular, groundwater is a vital water source, and it plays an important role in Scotland’s economy. [[OR/15/028 Introduction | '''(Read the full article...)''']]</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>Almost all groundwater starts life as rainfall. Some rain is taken up by plants, some runs over the land surface or through soils to rivers, and some soaks down through the soil into aquifers. Below the water table, all the spaces in the soil or rock are completely filled with water — groundwater (Figure 1). In Scotland, groundwater occurs almost everywhere beneath our feet, and the water table is usually within 10&nbsp;m of the ground surface. As a store of water that can provide a reliable source of water for drinking and other purposes, groundwater is often accessible close to where it is required, and is cheaper to treat than surface water in lochs and/or reservoirs. In rural areas in particular, groundwater is a vital water source, and it plays an important role in Scotland’s economy. [[OR/15/028 Introduction | '''(Read the full article...)''']]</div></td></tr> </table>

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