Page:Transactions of the Geological Society, 1st series, vol. 3.djvu/182

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 * style="text-align:center;border-style:solid none solid solid;border-bottom-width:.4pt;border-left-width:2pt;" | . || style="text-align:center;border-style:solid none solid solid;border-bottom-width:.4pt;border-left-width:.4pt;" | . || style="text-align:center;border-style:solid none solid solid;border-bottom-width:.4pt;border-left-width:.4pt;" | . || style="text-align:center;border-style:solid none solid solid;border-bottom-width:.4pt;border-left-width:.4pt;" | . || style="text-align:center;border-style:solid none solid solid;border-bottom-width:.4pt;border-left-width:.4pt;" | . || style="text-align:center;border-style:solid 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;" | Magheralin, near Moira, county of Devon || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | North west 8° || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | from 30 to 32 || 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;" | The chalk proceeds from hence towards the White mountains near Lisburn, by Soldierstown and Brookhill; it forms a low table lands. At Magheralin the bluish-grey variety occurs.
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | White mountain, near Lisburn Antrim|| valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | North-west 28 || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | from 38 to 40 || 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 none solid;border-bottom-width:2pt;border-left-width:2pt;" | Colin Glen, south-west of Divis, near Belfast || 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;" | about 450 feet above the level of sea. || rowspan="3" valign="center" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" | The line of junction, with the basalt, is not strictly horizontal but very irregular.
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | East slope of Divis || 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;" | about 450 feet
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Cave 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;" | || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | 768 feet
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Carmoney moutains & Carrickfergus hills || 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;" | considerably lower than in Cave hill || 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;" | Port Muck, northeast of the isle of Magee || 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-left-width:.4pt;" | || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" | The east coast of Magee is faced with a bold range of precipices, called tje Gollins, which are entirely basaltic, the chalk being sunk below the level of the sea
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Shor of Lough Larue, about 1 mile south from the town || 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;" | but little elevated above the sea || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | about 300 || 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;" | From hence the line of the chalk is distinctly traced in the section of the coast
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Gerron point || 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 none solid;border-bottom-width:2pt;border-left-width:2pt;" | Lurgethan mountain, near Newton Glens || 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;" | Hence the mountain mass of red sand chalk and basalt, sweeps inland in a curved line towards Tesbulliagh and the head of Glendun
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Mountain of Teabuliagh, 3 miles north-west of Newton Glens, forming a ridge between the rivers Glenaan and Ballyeemin || 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;" | 735 || 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;" | Eastern slope of Slieve Norry, towards the head of Gledun || 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;" |
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Holster hill, middle Cushleak || 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;" | 695 || 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;" | Here the mica slate of Cushleak, receives a cap of red sandstone, chalk and basalt
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Port Muck, northeast of the isle of Magee || 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-left-width:.4pt;" | || valign="top" style="border-style:none solid none solid;border-left-width:.4pt;border-right-width:2pt;" | The east coast of Magee is faced with a bold range of precipices, called tje Gollins, which are entirely basaltic, the chalk being sunk below the level of the sea
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Shor of Lough Larue, about 1 mile south from the town || 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;" | but little elevated above the sea || valign="top" style="border-style:none none none solid;border-left-width:.4pt;" | about 300 || 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;" | From hence the line of the chalk is distinctly traced in the section of the coast
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Gerron point || 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 none solid;border-bottom-width:2pt;border-left-width:2pt;" | Lurgethan mountain, near Newton Glens || 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;" | Hence the mountain mass of red sand chalk and basalt, sweeps inland in a curved line towards Tesbulliagh and the head of Glendun
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Mountain of Teabuliagh, 3 miles north-west of Newton Glens, forming a ridge between the rivers Glenaan and Ballyeemin || 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;" | 735 || 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;" | Eastern slope of Slieve Norry, towards the head of Gledun || 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;" |
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Holster hill, middle Cushleak || 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;" | 695 || 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;" | Here the mica slate of Cushleak, receives a cap of red sandstone, chalk and basalt
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Lurgethan mountain, near Newton Glens || 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;" | Hence the mountain mass of red sand chalk and basalt, sweeps inland in a curved line towards Tesbulliagh and the head of Glendun
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Mountain of Teabuliagh, 3 miles north-west of Newton Glens, forming a ridge between the rivers Glenaan and Ballyeemin || 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;" | 735 || 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;" | Eastern slope of Slieve Norry, towards the head of Gledun || 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;" |
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Holster hill, middle Cushleak || 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;" | 695 || 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;" | Here the mica slate of Cushleak, receives a cap of red sandstone, chalk and basalt
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Eastern slope of Slieve Norry, towards the head of Gledun || 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;" |
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Holster hill, middle Cushleak || 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;" | 695 || 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;" | Here the mica slate of Cushleak, receives a cap of red sandstone, chalk and basalt
 * valign="top" style="border-style:none none none solid;border-bottom-width:2pt;border-left-width:2pt;" | Holster hill, middle Cushleak || 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;" | 695 || 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;" | Here the mica slate of Cushleak, receives a cap of red sandstone, chalk and basalt