Page:Transactions of the Geological Society, 1st series, vol. 3.djvu/183

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 * style="text-align:center;border-style:none none solid solid;border-bottom-width:.4pt;border-left-width:2pt;" | . || style="text-align:center;border-style:none none solid solid;border-bottom-width:.4pt;border-left-width:.4pt;" | . || style="text-align:center;border-style:none none solid solid;border-bottom-width:.4pt;border-left-width:.4pt;" | . || style="text-align:center;border-style:none none solid solid;border-bottom-width:.4pt;border-left-width:.4pt;" | . || style="text-align:center;border-style:none none solid solid;border-bottom-width:.4pt;border-left-width:.4pt;" | . || style="text-align:center;border-style:none solid solid solid;border-bottom-width:.4pt;border-left-width:.4pt;border-right-width:2pt;" |.
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Murloch bay, on the east of Fairheader || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 560 || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 652 the summit of the cliff || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" |
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Benvaan, on the south of Murloch || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 885 || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" | This form a platform of chalk, covered with grass
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Ballypatrick, 3 miles south from Fairhead || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 622 || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" |
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Knocklead, an insulated mountain, 2 miles south from Ballycastle || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | S.W || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | very small || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 895 || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" | The intersection of the conical section surface of Knocklead with the plane of the chalk stratum, forms a zone completely encircling its middle region. In the exact direction of that plane the stratum of chalk (here interrupted by a deep valley) is resumed on the slope of the opposite mountain to the south. Towards the west it catches the plain near Ardmoy, where pits are opened. At Corky, 6 miles south from Ardmoy, and higher up the same valley, there are also chalk pits. See Dr. Richardson's papers.
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Ballycastle, west of the pier || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | S.W. 17 || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | from 15 to 18 || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | emerging from the sea || rowspan="2" valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" | The upper limit of the chalk stratum through the line of coast between these points, about 30 miles distant, keeps nearly the level of the sea, vacillating slightly on either side of that level, but seldom rising very high, and probably seldom submerged very deeply beneath it: the same description applies to the opposite island of Rathlin. It is unnecessary here to insert detailed particulars, which will be found represented in the sections of the coast.
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Down hill, on the west of the river Bann, in the county of Derry || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | N.E || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | emerging from the sea
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Benyavenagh || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | on the north side but little elevated above the sea, on the south about 200 feet || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" |
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Kedy || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | N.E || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 10 || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 550? || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 600 || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" | The deposit here hardly exceeds forty feet
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Donald hill || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 800 || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 900 || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" | The deposit here increase in thickness to 100 feet: the upper beds are soft enough to soil the fingers, the lower quite compact.
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Ballyness || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" |
 * valign="top" style="border-style:none none solid solid;border-left-width:2pt;" | Benbradagah || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none solid solid solid;border-left-width:.4pt;border-right-width:2pt;" | The thickness of the deposit here is greatly increased, amounting to no less than 363 feet: it is less regular stratified than usual. Towards its upper extremity it wears the character of considerable detached masses; in Kedy Donald and Ballyness mulattoe is interspersed between the chalk and sandstone, but in Bendradah the appear to be in contact.
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 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Down hill, on the west of the river Bann, in the county of Derry || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | N.E || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | emerging from the sea
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Benyavenagh || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | on the north side but little elevated above the sea, on the south about 200 feet || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" |
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Kedy || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | N.E || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 10 || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 550? || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 600 || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" | The deposit here hardly exceeds forty feet
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Donald hill || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 800 || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 900 || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" | The deposit here increase in thickness to 100 feet: the upper beds are soft enough to soil the fingers, the lower quite compact.
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Ballyness || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" |
 * valign="top" style="border-style:none none solid solid;border-left-width:2pt;" | Benbradagah || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none solid solid solid;border-left-width:.4pt;border-right-width:2pt;" | The thickness of the deposit here is greatly increased, amounting to no less than 363 feet: it is less regular stratified than usual. Towards its upper extremity it wears the character of considerable detached masses; in Kedy Donald and Ballyness mulattoe is interspersed between the chalk and sandstone, but in Bendradah the appear to be in contact.
 * }
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Ballyness || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" |
 * valign="top" style="border-style:none none solid solid;border-left-width:2pt;" | Benbradagah || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none solid solid solid;border-left-width:.4pt;border-right-width:2pt;" | The thickness of the deposit here is greatly increased, amounting to no less than 363 feet: it is less regular stratified than usual. Towards its upper extremity it wears the character of considerable detached masses; in Kedy Donald and Ballyness mulattoe is interspersed between the chalk and sandstone, but in Bendradah the appear to be in contact.
 * }
 * valign="top" style="border-style:none none solid solid;border-left-width:2pt;" | Benbradagah || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none none solid solid;border-left-width:.4pt;" | || valign="top" style="border-style:none solid solid solid;border-left-width:.4pt;border-right-width:2pt;" | The thickness of the deposit here is greatly increased, amounting to no less than 363 feet: it is less regular stratified than usual. Towards its upper extremity it wears the character of considerable detached masses; in Kedy Donald and Ballyness mulattoe is interspersed between the chalk and sandstone, but in Bendradah the appear to be in contact.
 * }