Illustrations of the Geology of Yorkshire, Or, A Description of the Strata and Organic Remains of the Yorkshire Coast: Accompanied by a Geological Map, Sections, and Plates of the Fossil Plants and AnimalsAuthor, 1829 - 192 páginas |
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Página 4
... the chalk - hills of Oxfordshire and Berkshire ; then crosses vales of clay and sandstone , ascends a range of oolitic limestone ; traverses wide plains of blue and red marl ; arrives in districts where coal , iron 4 PRINCIPLES OF GEOLOGY .
... the chalk - hills of Oxfordshire and Berkshire ; then crosses vales of clay and sandstone , ascends a range of oolitic limestone ; traverses wide plains of blue and red marl ; arrives in districts where coal , iron 4 PRINCIPLES OF GEOLOGY .
Página 21
... seek more satisfactory evidence than in each case each valley furnishes , it deserves to be mentioned . Some vallies cross and cut through vertical strata , which must necessarily have been at first deposited PRINCIPLES OF GEOLOGY . 21.
... seek more satisfactory evidence than in each case each valley furnishes , it deserves to be mentioned . Some vallies cross and cut through vertical strata , which must necessarily have been at first deposited PRINCIPLES OF GEOLOGY . 21.
Página 34
... Cross , one thousand feet , Egton moors , and Loose Hoe , fourteen hundred and four feet , to Burton Head , fourteen hundred and eighty - five feet . This is supposed to be the highest point of land in the eastern part of the county ...
... Cross , one thousand feet , Egton moors , and Loose Hoe , fourteen hundred and four feet , to Burton Head , fourteen hundred and eighty - five feet . This is supposed to be the highest point of land in the eastern part of the county ...
Página 36
... crosses the Derwent at Howsham , and proceeds by Leppington and Bugthorpe , till it comes to be almost concealed under the chalk - hills at Garraby and Bishop Wilton . Its course , however , is still continued in a narrow tract ...
... crosses the Derwent at Howsham , and proceeds by Leppington and Bugthorpe , till it comes to be almost concealed under the chalk - hills at Garraby and Bishop Wilton . Its course , however , is still continued in a narrow tract ...
Página 43
... crosses the Derwent , and , after rising into the high ground of Langton wolds , turns again to the south , and passes under the chalk - hills at Acklam . Some of the strata which belong to this group of rocks , re - appear from below ...
... crosses the Derwent , and , after rising into the high ground of Langton wolds , turns again to the south , and passes under the chalk - hills at Acklam . Some of the strata which belong to this group of rocks , re - appear from below ...
Otras ediciones - Ver todas
Illustrations of the Geology of Yorkshire; Or, a Description of the Strata ... John Phillips Sin vista previa disponible - 2018 |
Illustrations of the Geology of Yorkshire, Or a Description of the Strata ... John Phillips Sin vista previa disponible - 2017 |
Términos y frases comunes
Aldstone moor ammonites appears argillaceous Bath oolite beds Blue wick Bolland Brandsby calcareous grit chalk chert cliffs Cloughton coal Conch coralline oolite cornbrash Craven fault dale deposits depressed Derbyshire diluvial dislocation district Ditto dyke east elevation fell Flagstone formation fossils geological grauwacke Greenhow Greenhow hill Gristhorpe gritstone hill hundred feet inferior oolite Ingleborough ironstone Kelloways rock Kirby Lonsdale laminated layers lias shale lime limestone limestone series lower limestone lower scar limestone main limestone Malton marlstone mass mesial millstone grit mountain limestone Nidderdale Northumberland organic remains Oxford clay pebbles Penyghent Plate red sandstone remarkable Ribblesdale ridge Robin Hood's Bay sandstone Scarborough septa Sheffield shells side slate species specimens Speeton clay stone strata striæ striated summit surface Swaledale Teesdale thickness underset undulated upper vale valley veins Wensleydale Wharfedale Whernside Whin sill Whitby whorls Yoredale series Yorkshire
Pasajes populares
Página 19 - The excavation of vallies can be ascribed to no other cause than a great flood of water which overtopped the hills, from whose summits those vallies descend.
Página xvi - Enough, if something from our hands have power To live, and act, and serve the future hour; And if, as toward the silent tomb we go, Through love, through hope, and faith's transcendent dower, We feel that we are greater than we know.
Página 50 - The alterations in the form of land, occasioned by diluvial agency, must have been considerable, but are not yet well understood; the operation of natural causes since that period deserves to be maturely considered, for these have materially changed the face of the globe. The lakes which were left, on the retiring of the diluvial currents, appear to have been continually diminished in depth, and contracted in extent, by deposits of vegetable matter, decayed shells, and sediment brought into them...
Página 117 - the interesting remains of Spongiae are nowhere so well developed as in England, and perhaps nowhere in England, so well as in Yorkshire. On the shore near Bridlington, they lie exposed in the cliffs and scars, and being seldom enclosed in flint, allow their organization to be studied with the greatest advantage.
Página 46 - Yorkshire, is composed of a base of clay, containing fragments of pre-existing rocks, varying in roundness and size. The rocks from which the fragments appear to have been transported are found, some in Norway...
Página 154 - in the midland counties, the Fuller's earth rock of Mr. Smith does by no means furnish a constant or wellmarked line of distinction between the middle (great or Bath) oolite and the inferior oolite ; and I am decidedly of opinion, that in the northern part of Northamptonshire, and throughout Rutland and Lincolnshire, there is but one thick oolitic rock beneath the cornbrash, resting upon brown sandstone, which immediately covers the upper lias shale.
Página xi - Explorations of three of the fine mountains which are visible from Florence Court gave us a complete section of the limestone series in Ireland, and while the forms of Ben Jochlin, Kulkeagh, and Belmore, seemed copied from Penyghent, Wildboar Fell, Water Crag, their constituent rocks were found closely analogous.
Página 18 - No one can doubt that great alterations were occasioned in the features of the earth's surface, at the period of the deluge, who considers the extensive tracts formed of the diluvial detritus. All the solid land of Holderness is an accumulation of this kind, from the ruins of others parts of England and Scotland and perhaps Norway.
Página 95 - ... feet above the vale of the Eden and the plain of Carlisle, and the level beds of the red sandstone deposited in later times at the foot of the ancient escarpment, upon the relatively depressed portion of the same mountain limestone series.
Página 151 - Sternberg. and mountain limestone" — in other words, is associated with the more ancient carboniferous deposits. " A cursory observer," adds Mr. Phillips, " may, perhaps, be led to confound together the ferns and calamites of the coal district with the ferns and equiseta of the oolitic rocks : though to a botanical eye their difference is very apparent : but who can mistake the lepidodendra of the former, the cycadiform fronds of the middle period, and the dicotyledonous leaves and fruits which...