Proceedings of the Geological and Polytechnic Society of the West Riding of Yorkshire, Volume 12Includes list of members in each vol. |
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Pagina 12
... run short , we should still have beds of immense thickness which , though not so valuable as pure coals , might in case of need be made to render good service ( See Table No. 20 , 50 , etc. ) The sharp line of demarcation between the ...
... run short , we should still have beds of immense thickness which , though not so valuable as pure coals , might in case of need be made to render good service ( See Table No. 20 , 50 , etc. ) The sharp line of demarcation between the ...
Pagina 23
... run off in floods , and a third absorbed . If numerous stream lines traverse the square inch in all directions , two - thirds of the rainfall will be run off in floods , and be only available in catchment reservoirs of large extent ...
... run off in floods , and a third absorbed . If numerous stream lines traverse the square inch in all directions , two - thirds of the rainfall will be run off in floods , and be only available in catchment reservoirs of large extent ...
Pagina 72
... runs the Markington Beck , a great part of which shortly disappears in swallow - holes and crevices of the Limestone . After passing underneath the hill , which is between Markington and Bishop Monkton , the stream bursts out in the ...
... runs the Markington Beck , a great part of which shortly disappears in swallow - holes and crevices of the Limestone . After passing underneath the hill , which is between Markington and Bishop Monkton , the stream bursts out in the ...
Pagina 135
... runs from Bycliffe along Groove Gill , crosses Gateup Gill , where the fracture is seen , and thence crossing north of Wig- stones it runs down Stony Groove to Merryfield ; and thence into the Craven Fault near Pateley Brig . This vein ...
... runs from Bycliffe along Groove Gill , crosses Gateup Gill , where the fracture is seen , and thence crossing north of Wig- stones it runs down Stony Groove to Merryfield ; and thence into the Craven Fault near Pateley Brig . This vein ...
Pagina 143
... about 50 yards from the elbow , just above the 1,500 contour line ; it runs to the spring on the east side of the road . Shales sandy micaceous ; concretionary and jointed , bluish in DAKYNS : GEOLOGY OF GRASSINGTON AND WENSLEYDALE . 143.
... about 50 yards from the elbow , just above the 1,500 contour line ; it runs to the spring on the east side of the road . Shales sandy micaceous ; concretionary and jointed , bluish in DAKYNS : GEOLOGY OF GRASSINGTON AND WENSLEYDALE . 143.
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Overige edities - Alles bekijken
Veelvoorkomende woorden en zinsdelen
Ascodictyon Askern bands Barnsley barrow base beds Blea Wyke bones boulder clay Bridlington Brit British Bryozoa Calamostachys Carboniferous Carter cells Chalk cliff Coal Measures coast Cornbrash Cretaceous d'Orb Dadoxylon Davis deposits described district doggers drift east Embleton Estuarine faults feet Filey flint fossils fragments genus Geol glacial glacier Grassington gravel Grey Gristhorpe Halifax Hall hard Harrogate Hill Horizon Huddersfield inches ironstone Journ Keuper layer Leeds Lias Limestone Lower Marl Middle miles Millstone Grit moraine mound nodules occur Oolite Permian Plate Polyzoa portion present probably Proboscina Proc Prof quarry Quart Red Sandstone Robin Hood's Bay rock sand Sandstone sandy Scarborough seen Shale shells side Silurian Skipton Society Soft species specimens Speeton Stomatopora stone strata sulphuretted surface thickness thin tissue Upper Vine Yorksh Yorkshire Zoarium Zoccia zone
Populaire passages
Pagina 451 - President, in the Chair. The Minutes of the last General Meeting were read and confirmed. The following Annual Report of the Council was then read : — ANNUAL REPORT OF THE COUNCIL.
Pagina 442 - Bay is well-known to tourists and to most geologists, lu point of scenery it is one of the most beautiful, if not the most beautiful, bay on the Yorkshire Coast.
Pagina 56 - ... first-rate dentists, that it is almost impossible to distinguish the one from the other — the real from the false. There is another method of fixing called the continuous gum ; it consists of an artificial gum, in which the teeth are embedded, and which is made of a somewhat similar composition to that of the teeth, but more flexible ; this fits over the real gum, and is...
Pagina 323 - Unconformability of the Permian Limestone to the Red Rocks west of its Escarpment in Central Yorkshire [1877J.
Pagina 213 - ... to which I am indebted for much of the information in this paper : — J.
Pagina 332 - On the Fossil Fishes of the Carboniferous Limestone Series of Great Britain.
Pagina 90 - ... pyriform calcareous vesicles, varying in length from one fifth to one third of a line, and usually disposed in stellate clusters, each containing from three to six cells, or sometimes more. The walls of the vesicles are perforated by microscopic foramina, usually showing a distinctly linear arrangement. The clusters are connected together by creeping filamentous tubes, the free surfaces of which are perforated by a single row of minute foramina, and which generally anastomose so as to form a...
Pagina 78 - I regard as having been deciduous and developed by budding from the creeping stolons at the parts now represented by small pores.
Pagina 321 - On the Fossil Fishes of the Mountain Limestone of Great Britain " (1883) ; " On the Fossil Fishes of the Chalk of Mount Lebanon and Syria" (1887); and "On the Fossil Fishes of the Tertiary and Cretaceo-Tertiary Formations of New Zealand'
Pagina 230 - Topinard found that the index is somewhat higher than in short persons (averaging 81 '1 in males with statures between 1 m. 70 and 2 m. 06, ;md 797 in those with statures varying from 1 m. 43 to 1 m. 60) the index is so high in D as to lead us to suspect that some error has occurred in recording the length of the tibia in that skeleton. The index of Platycnemism, or the relation between the transverse breadth of the tibia to its antero-posterior diameter...