Identifier: quarterlyjourna331877geol (find matches) Title: The Quarterly journal of the Geological Society of London Year: 1845 (1840s) Authors: Geological Society of London Subjects: Geology Publisher: L More
Illustration from The Quarterly Journal of the Geological Society of London, volume 33 (1877)
GLOUCESTER, DORSET, AND SOMERSET. O bring that about), there would not be much difference between the Ham-Hill section and several other sections near Sherborne. Fig. 2. — Comparative Sections of Beds at Ham More
Pericosmus crawfordi (syn. Megalaster compressus), abactinal surface.
A REDUCTION OF PORTION OF CHART 1 '£1 E L A W 13 Sheet XV. Wexford Bay, AND ADJOINING COAST LINE. ritr Cohere skinale beach and si/c vl'tllc Cnltoiv Iciqwrt . WICKLOW HEAD Arklow Hank L r Site rC C More
LATER TERTIARY GEOLOGY OF EAST ANGLIA. 93 Fig. 14.__ Section XIV., across the Tese Valley. (Length 4 miles. Yortical scale 17£ times the horizontal.) Brick-pit 5 furl. W.N.W. of Site of Shottesham church More
F. W. HARMER ON THE KESSINGLAND CLIFF-SECTION. 130 Mastodon, lihinoceros, and other animals whose remains occur in this stone -bed been buried in it at the time they died, or soon after, we could not fail t More
J. BTJCKMAN ON THE CEPHALOPODA-BEDS OF exceeds 28 or 30 feet in thickness, of which from 8 to 10 feet belong to the lower subdivision. The upper subdivision immediately underlies the Fuller's Earth ; and More
136 F. W. HARMER OK THE KESSIKGLAKD CLIFF- SECTION , &5 bJO • i-H CU &JD "6 -a a C3 «" ^ ".S 03 __! Qj i«S . • ,-H .2 © ^ "3 -Q o © .§ S T§ § "§. g %. rrt •■- -i- 1 on rt^ d • © c s ^ 2 §^ More
104 S. V. WOOD, JVN., AND F. W. HARMER ON THE «H CO 03 © h=3 • l-H 3 03 «H. T3 P 03 CO © r— t • r-t Pi © a Kl © . +3 5S P Si o 1C1 pQ 03 .» O t. to ^O ^ p © © ,Q 3* ^_ More
LATER TERTIARY GEOLOGY OF EAST ANGLIA. 9D Middle Glacial a thin bed of dark brown loam, which also fills a pothole excavated some 5 feet or thereabouts in that drift. After what we have observed as to t More
• s rACEous patellim; &
AND CIRQUES IN NORWAY AND GREENLAND. 107 r Jl ) o 1— ■ • N O P i— i a o P o p ax CO to 2- 4X O 00 ?! i— . -j ft "!. CfO. W ^s lM V5 A. OS M & o a- s ^ \ u Or 00 Co O: © More
uart . Journ. Geol . Soc .Vol . XXXEI . PI . Ill . 13. v, oV t o- -'0 W ,0 • - o - 10 s 9 - "oo^^o'^OU - ; J, ' : -~ C.Berieau. tilll. AUSTRALIAN CAINOZOIC ECHINODERMS.
1. 1 . Join n . Geo! . Soc .Vol . XXX - AUSTP
LATER TERTIARY GEOLOGY OF EAST ANGLIA. 105 5* k*S ^ ^i ^ l*" 5 2Q ^. ^^ c* r— 1 © a ■4-Z OS fl © o £» NJ o 'r-. 8 o ^ r& § o cs r& §e +3 .» oo © ~ .» q •i— i -*3 .^. More
LATER TERTIARY GEOLOGY OF EAST ANGLIA. 81 this crag and associated sands are capped directly by the Middle Glacial in the way shown by section III. Fig. 3. — Section III., in a Coprolite-pit by Foxhcdl Hall More
152 AHUFD HELLAND ON THE FJOKDS, LAKES, CO I 4 ..^ &Q ^ 5? OJ .& ba •rH
76 S. V. WOOD, J TIN., AND F. W. HARMER ON THE signs of any gradual disappearance of the shells by the abstracting agency being apparent, and also that the dividing line was very irregular, the shelly crag More
GRITS OF CORWEN, NORTH WALES. 209 the direction of the second pressure may coincide with that of the first ; and though perhaps the result may be more intense cleavage in the previously cleaved rocks, no cr More
Spines of Hibbertopterus stevensoni (syn. Eurypterus stevensoni), probably from the dorsal posterior margin of an abdominal somite. From Kimmerghame Quarry, near Dunse, Berwickshire.
LATER TERTIARY GEOLOGY OF EAST AN G LI A. oo 05 cc o o cr o o 3 cd M « E, 5 Or 05 cr o . CD a. SB B P B PL, ^ tr CD OQ CD o g o s Pj a. P p cs c-f- o tr CD CD « ^3 More
268 J. F. BLAKE AND W. H. H1TDLEST0N ON And about 22 ft. below this occur the great doggers previously noticed on the coast. Nearly the whole of this section shows oolitic conditions, though the beds are v More
LATER TERTIARY GEOLOGY OF EAST ANGLIA. 101 the Waveney and Yare extended, which, having been filled in with the Upper and Middle Glacial, has not been re-excavated, re- maining as a low tableland, of which More
LATER TERTIARY GEOLOGY OF EAST ANGLIA. 85 CnttingW. of the Station. "1 Cutting and Pit E. of . Hethersett Railway J Station. Pit half a mile W. of Cringleford church. I Excavations made j. near the Cot More
Centrochelys robusta, syn. Testudo robusta. Fig. 1. Caudal vertebra Figs. 2, 2a. Right coracoid of the scapula Figs. 3, 3a. Right tibia Figs. 4, 4a, 4b. Proximal third of the left femur Figs. 5, 6, 7. Phalangeal bones
F. W. HARMER ON THE KESSINGLAND CLIFF-SECTION. 137 The bed No. 4 is the Middle Glacial sand with fine shingle bands, which is generally present in the district. It rests upon the nearly horizontal surface More
Fig. 1. Left radius of Centrochelys robusta (syn. Testudo robusta, Testudo spratti) Figs. 2, 2a. Left radius of C. robusta Figs. 3, 3a, 3b. Portion of a left scapula of C. robusta Figs. 4, 4a. Left tibia of C. More
W;. sgs* -l-^-t: 81 ?z i Quart. Joarn. Geo! Soc.Vcl XXXIII PL VIII. ,-:;,; ,.£31^ 77 .'». ■ i\H 2. y ■ - 20 & c
IN THE LOWER OLD RED SANDSTONE OE SCOTLAND. 217 In the foregoing notes we have endeavoured to give a short and con- cise sketch of the literature of the Old-Red plants of Scotland. "We have not thought it n More
ON THE SILURIAN GRITS OF CORWEN, NORTH "WALES. 20' 12. On the Silurian Grits 0/ Corwen, Xorth AY ales. By Prof. T. McKenni Hughes, M.A., F.G.S. (Read December 20, 1876.) I beg to offer a few notes, made chie More
LOWER-CARBONIFEROUS CRUSTACEAN. 225 rings of E. Scouleri*. The following are the measurements of this specimen (approximately) : — in. lin. Length . . 1 7 Breadth 1 11 Length of central spine 1 2 In anot More
324 J. P. BLAKE AND W. H. HITDLESTON ON c. Cylindrites elongatus, Phil, v. c. Gervillia aviculoides, Sow. Avicula ovalis, Phil. Astarte Duboisiana, D' Orb. Trigonia (clavellate form). c. Sowerbya triangu More
244 W. J. SOLLAS OX PHAKETllOSPOXGIA STKAHAXI. Oscular Surface. — This (PL XI. fig. 2) is smooth all over and much more even than the other face ; the fibres of its network are broader than those of the inte More
W. J. SOLLAS ON PHARETROSPONGIA STRAHANI. 247 sen ted in PL XI. fig. 6, where a fibre is longitudinally striated throughout except at its rounded termination, where the striae are replaced by circles. This More
THE C0RALL1AN ROCKS OF ENGLAND. 371 This happens to to have been one of those places where the acci- dents of distribution were favourable to the accumulation of shells. Although no corals have been found, More
298 J. F. BLA.KE AND W. H. HUDLESTON ON by him as absent, an interpretation which, though in our opinion erroneous, proves that he saw the difference between these beds and the Lower Calcareous Grit. Yig. More
THE CORALLIAN ROCKS OP ENGLAND. 369 kinds, and also immense quantities of shells and shell-fragments, the whole forming a sparkling white limestone with a splintery fracture almost wholly devoid of oolite. More
350 J. F. BLAKE AND W, H. BTTDLESTON ON •r ^ 5 & l« 03 © en O -s 0) © o © s to © 00 ■+3 o -s -^. © k5 CD rH 60 W Whitestone cliff. 1050 feet. . •srf ■AY » &tv P do - M — More
276 J. F. BLAKE AND W. H. HTTDLESTON ON Section in Sturminster Railway -cutting. u a ^. O .N O .jo a 4-3 fee c .x. (-1 5Q ^ S5 I H .a oo o ft. wis .$35 go =a 33 "x .a Hu sj § t^ More
AND SALEXI A FROM SOUTH AUSTRALIA. 257 Belemxites SBNB8CBNS, spec. uov. Fig. 1. Guard elongated, slender, gradually tapering to an acute apex, cylindrical, but inclined to subquadrangular in section, especi More
A. CORRELATION OF UPPER CARBONIFEROUS OR PERMIAN STRATA Quart. Journ GeolSocVolXXXOWt I B. SECTION OF STRATA FROM CHI RK, DE N BICHSHIRE TO IFTON HEATH, SHROPSHIRE. .rn -COLLIERIES %t - 5 -£-— _.£_, 4 fF More
356 J. F. BLAKE AND W. H. H1JDLEST0N ON (fig. 16), attention to the following points will be necessary. The two are approximately parallel ; the distance between them about 1 J mile. Their eastern terminati More
Quart Journ.Geol3oc T ;': .I.P1.XIII MSuft del.etlith. ■ it* i : .
AND CAHORE SHINGLE BEACH, CO. WEXFORD. 35 back wash (A, fig. 1) of each wave will carry a quantity of sand and the like with it, which at the junction (B) with the incoming wave Fig. 1. — Diagram of a Wind- More
Quart Journ Geol.SocVol XXXIII Pl.XV. - It MSuft del.et Tith M&KHanhart imp. CORALLIAN FOSSILS
THE CORALLIAN ROCKS OF ENGLAND. 305 beds in the neighbourhood, we have no doubt that the red soil here is the representative of the Upper Calcareous Grit ; but the sands and clays below, being overlain by o More
Character of the whin sill of Northumberland. 413 © 85 g ^ «$ ©* a "*" § ta.© 1 ^ A ^ - 'p i' o Os & «*• tl ^ B I" &•§ Q .* "5 o ©- © © o 1
Quart Journ . Geol . Soc .Vol . XXXIII PI . XVIII From W.FORSTERS Section^ of -the Strata" 1822 j\ £ ■ Co "n r- Pi 01 o h 111 11 c» rn to o a: a: w en o a) . m 30 CO O z O z o More
THE BORROWDALE SERIES AND THE CONISTON FLAGS. 465 hard grey or bluish grey, cleaved, and often highly calcareous shales, containing numerous nodules or thin but distinct bands of limestone. In some places t More
316 J. F. BLAKE AND W. H. HTJDLESTON ON S. r^ ^ £ r. 8 I o CO ■Si § 6 ■M &5
Hypothetical restoration of the skull of Portheus gaultinus. bs. Upper portion of basisphenoid. as. Alisphenoid. pa. Parietal region. ps. Presphenoid. fr. Frontal. sp.ot. Sphenotic (postfrontal). pr.ot. Prootic More
LATER TERTIARY GEOLOGY OF EAST ANGLIA. 87 Figs. 7-9. — Sections VII.-IX., across the Wensum Valley. (Length of each section about 2 miles. (Vertical scale about 17 j times the horizontal.) Fig. 7.— Section More
Quart.Journ.Geol.Soc.Yol. XXXIII. PI XXI CAMBRIDGE GREENSAND FOSSILS. A S Foord dd . et lith
Quart Journ Geol Soc Vol XXXUl PL XXII CLGriesWJ. lith. PORTHEt'S m iS BTM ■
OF THE CAVES OF CRESWELL CRAGS. Fig. 2. — Ironstone implement, Robin Hood Cave, \, 593 entirely discarded the implements of stone and bone, relics of such materials are not uncommonly found in graves which More
Weymouth Distent I Sandsfoot Xo8v II Osmington III Milwtstiuly Corallian Rocks of Encland. TabU of Comparative Sections by the Bev. J.F.Blake, MAE G.S, and W. H. Hudleston Esq.MAJF.GS. North Wilts . Berks More
LATER TERTIARY GEOLOGY OF EAST ANGELA. Ill responds with the level at which the clay was reached in the well at the railway-station, it seems to us that this bed of chalky clay and overlying brick-earth may More
Quart. Jonrn Geo! for Vol XMI V i; '. v * * E S I: i 5 '- 1 70 i. .► . -7 BRITISH CRETACEOUS PATELLIDiE & c
594 W. BOYD DAWKINS ON THE MAMMAL-FAFNA at the present day *. The obtusely pointed quartzite choppers would be admirably adapted for that purpose. Fragments of charcoal and calcined bone show also that the More
526 T. SPRATT ON THE COAL-BEARING DEPOSITS NEAR EREKLI. already been worked as far as practicable, and few extended a greater distance before a fault was met with ; and as the seams corresponded on both sid More
Quart. Jo urn Geol. Soc. Vol. XXXIII . PL XIX x/7 77 x 77 ERUPTIVE ROCKS OF NORTH "WALES MmterrLBro? imji.
Fig. 1. Ulna outride Can
THE CORALLIAN ROCKS OF ENGLAND. 375 Ox £»■ CO to O hi . P a 7* a oa p o re §B 00 p Cp o CD co £ 4 p ro ! £-» £ ru 3 cd CD 0.? cr- ~ - P i-i •**-. o O O ^ Q n,p Qp- O fi u % » s p 2- B More
678 R. L. JACK AND J. HORNE ON GLACIAL DRIFT about 5 miles above Szigeth, the main road ascends to the level of the upper terrace, which sweeps south to the base of the hills. At this point the valley is on More
Quart. Journ GeoLSoc .Vol .XXXIII Pl.XYI MS-uft del etlitli /."■'•■i'C-v- \ m Hanhart u CORALLIAN FOSSILS
654 C. CALLAWAY ON A NEW AREA OF UPPER
236 H. HICKS ON THE PRE-CAMBRIAN ROCKS OF ST. DAVID S. sections. Most of the harder compact conglomerates have been dropped in the hill north of the Cathedral by a fault running in a N.E. direction almost a More
464 R. HARKNESS AND H. A. NICHOLSON ON THE STRATA BETWEEN Ci/bele verrucosa, fflomus Bowmanni, and Lichas laxatus, can leave no doubt as to the correctness of the inference that these rocks belong to the Bal More
Quart. Journ Geol Snc Vol HDD P. '
472 R. HARKNESS AND H. A. NICHOLSON ON THE STRATA BETWEEN Fig. 3. — Diagram showing the vertical Succession of the Silurian Strata in Slelgill BecJc, near Ambleside. Base of the Coniston Flags (Broughton- M More
W. J. S0LLAS ON PHARETROSPOtfGIA STRAHANT . 243 increase, the edge will undulate on each side of an imaginary median plane, and thus the gentle folds a b c, of PI. XI. fig. 1, shown in the diagram, Fig. 2, More
686 PROF. OWEN ON THE RANK AND AFFINITIES IN mosal, 27, for the suspension of the tympanic, 28 ; the pair of hypa- pophyses, i', from the basioccipital, i ; the greater proportion of the occipital surface c More
688 PROF. OWEN ON THE RANK AND AFFINITIES IN by Cuvier (p. 319), are " sans explication osteologique " — that is, have no symbols of reference to the constituent bones. § 3. Upper Surface of the Cranium. — More
THE KEPTILIAN CLASS OF THE MOSASAURID^. 689 near the coronal suture ; but in Amblyrhynchus and other Igua- nians this foramen is in that suture. Tig. 7. Fig. 8. Monitor niloticus. Upper surface of crani More
Quart. Journ Geol. Soc Vol XXXlll . PI. XI. ?f 7. 60 ■ ' . 1' \ --,-;• fc£p & - a^ - " M-t % * I 1 ml -.,■■' fi 13 ^ o 1 i l : -J &S? .'..: PH&RETROSPMJGTA. STRAHANI. ) ' , 10. ,
H. GOVIEK SEELEY ON MATJISAUEUS GAKDNEEI. 545 rather smaller. The nutritive foramina become small circular pits rather further apart. In all about 40 vertebrae have been collected, of which about 14 are dor More
280 J. F. BLAKE AND W. H. HTTDLESTON ON Section of Oolites and Limestones at Todbere. ft. in. 1. Loose, soft yellow oolite marl, and rubbly thin-bedded oolite limestone, with numerous fossils. Natica, sp., More
292 J. P. BLAKE AND W. H. HUDLESTOtf ON" Yig. 4. — Section of Coral-beds, Hillmarton. a. Coral and altered Limestone. b. Clay. most probable that they are all organic growths on the spot, rather than tran More
r 02 PBOF. OWEN ON TFIE RANK AND AFFIMI'li Fig. 10. 33 Amblyrhynchus. Fig. 20. Fig. 21. Python.
AND PELVIC BONES OF PLTOSAURUS EVANSI. 717 bone is deeply concave from side to side, nearly flat from within outward, with the articular surface directed outward and downward so as to meet the inferior exte More
THE REPTILIAN CLASS OP THE MOSASAURIDJE. 709 coalesced neural arch represents at last the entire vertebra. All these modifications, shown in the plates of Cuvier and Goldfuss, are repeated in the figures of More
AT WINDY KNOLL, CASTLETON, DERBYSHIRE. 725 Fig. 1. — East-and- West Section through Windy-Knoll Fissure. (Scale 20 feet to 1 inch.) ' Surface denuded away. Present surface. — y ? Cavern 7 The whole skel More
'68 E. inr.r and t. g. bonnet on ttie 2 o W w — • Patch of breccia. -« Indurated slates. »=» Grit in spinney. .** Great breccia bed. Dnstratifled breccia of Tin-meadow. Porphyritic breccia. mmmm Kou More
718 H. G. SEELKY ON THE VERTEBRAL COLUMN The axis is not so well preserved as the atlas, being a little weathered on the neural surface and a little crushed on the posterior part of the basal surface ; it i More
334 J. F. BLAKE AlfD W. H. HUDLESTON ON wood, where they are cut through by the road. Here the oolites are rather crystalline limestones towards the base, but become creamy, close-grained, and thin-splittin More
'80 E. HILL AND T. G. BONNE Y ON Til K agglomerate of the centre of High Towers resemble these in some respects ; but there the weathering renders the fragments exceedingly conspicuous. 18. The section (fi More