Quarterly Journal of the Geological Society of London, Volume 25, 0167
Illustration in the Quarterly Journal of the Geological Society of London, volume 25
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Illustration in the Quarterly Journal of the Geological Society of London, volume 25
Quarterly Journal of the Geological Society of London, Volume 25, 0579
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Illustration in the Quarterly Journal of the Geological Society of London, volume 25
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Illustration in the Quarterly Journal of the Geological Society of London, volume 25
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Illustration in the Quarterly Journal of the Geological Society of London, volume 25
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Illustration in the Quarterly Journal of the Geological Society of London, volume 25
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Illustration in the Quarterly Journal of the Geological Society of London, volume 25
The Quarterly journal of the Geological Society of London (12961259805...
446 PROCEEDINGS OF THE GEOLOGICAI, SOCIETY. ifiill W =^- 4-4- 1 t=. ^-E I? CO CO o i^ ^ \ •aa^i JaAja ^ a ii^l 1 /'I -§^a (0 A r^- rt5 .D S -^ P-l -1-3 OS X «5 'S -^ £ 8 ^ i !S ... More
The Quarterly journal of the Geological Society of London (12961251653...
124 PROCEEDINGS OE THE GEOLOGICAL SOCIETY. .DcC. 23, are found, as a general rule, forming the summits of the hills, while 2 and 5 almost invariably occur at the bottom of the valleys. In the Suichang distr... More
The Quarterly journal of the Geological Society of London (12961530314...
98 PKOCEEDINGS OF THE GEOLOGICAL SOCIETY. the current was reduced, the finer materials might be deposited. There is no evidence of any change of level during these deposits ; and the river must have risen 5... More
The Quarterly journal of the Geological Society of London (12961008565...
^ W '^ ^-1 LU . §^ !^
The Quarterly journal of the Geological Society of London (12961051745...
TYLOE QUATEENAKY GEAVELS. 83 at the present time ; but the physical conditions under which a gravel- deposit like that at Sangatte could occur do not exist at the present time in France. It would require th... More
The Quarterly journal of the Geological Society of London (12961135173...
42 PROCEEDINGS OF THE GEOLOGICAL SOCIETr. .DcC. 9, 1. Limestone with a few celestine nodules. 2. Limestone with much nodular celestine and thin plates of fibrous gypsum ... 1 3. Sandy marls with nodules of... More
The Quarterly journal of the Geological Society of London (12961268633...
1869.. WHITAKER SOUTH-DEVON " NEW RED. 155 It would be a work of time and trouble to measure the thickness of each division ; perhaps, indeed, it would be impossible to do so at all accurately; but I must ... More
Quarterly Journal of the Geological Society of London, Volume 25, 0155
Illustration in the Quarterly Journal of the Geological Society of London, volume 25
The Quarterly journal of the Geological Society of London (12961028545...
TTLOK QTJATEENAEY GIIA"VELS. 73 % St - CRAiO OCLL/eRY S/D/UC HiP.WAlU RAILWAY ■IPtKE RO&Q FROM ABSRDA Sm BRECON & .NEflTH 5a tai fVVER CYNON
The Quarterly journal of the Geological Society of London (12961232995...
ua-rLJoupn Geoi.SocJol XKV PIXVI. MJ:N Hanliipl iinr SAURIAN HUMERUS FROM KIMMERIDGE
The Quarterly journal of the Geological Society of London (12961266163...
1869.. WfllTAKER SOUTH-DEVON '^ NEW RED." 153 masses, that little is to be seen below the " White Lias " until we pass to the west of the great landslip of 1839 at Dowlands. The cliff is then clearer, and ... More
Quarterly Journal of the Geological Society of London, Volume 25, 0172
Illustration in the Quarterly Journal of the Geological Society of London, volume 25
The Quarterly journal of the Geological Society of London (12961145753...
P J.&SX OF CRAYl ORD, KLEJVT. Copied Prxmo the Oi'djuince PoTi-sh Map Quai-t.Jouai.l.^ol. So^- Vol XSV: Pl.VI ^ .' The Jiiva^ Thames fiaws fixrm. W.S.Wto 1 ■ J:.M.K. frvm,£rHJv Wharf to Crciy/brti 'i\ f ... More
The Quarterly journal of the Geological Society of London (12961151215...
1869.. COQUAND CEETACEOTJS STKATA. 245 on the Geology of Constantine, I have received from M. Brossard several unpublished species; and M. Peron, who has intelligently explored the high plateaux of the pro... More
The Quarterly journal of the Geological Society of London (12961399163...
422 PKOCEEDINGS OF THE GEOLOGICAL SOCIETY. .June 23, SO, I shall merely quote from my notes. At the east end of the sec- tion, and near to the railway- station I unexpectedly found real pinel in a deep side... More
The Quarterly journal of the Geological Society of London (12961660134...
384 PROCEEDINGS OF THE GEOLOGICAL SOCIETY. Fig. 3. — Scales of Gyrodiis coccoderma. .June 23, Mr. Etheridge having kindly directed my attention to some spe- cimens of Pycnodont teeth deposited in Jermyn St... More
The Quarterly journal of the Geological Society of London (12961674864...
408 PEOCEEDIl^GS OF THE GEOLOGICAL SOCIETY. .Juno 23, deposits had scarcely been suggested *, the author thought it best to remain ignorant of what had been said about this particular locality previously to... More
The Quarterly journal of the Geological Society of London (12961041185...
80 PROCEEDINGS OF THE GEOLOGICAL SOCIETY, the intermediate series of stratified gravels, with the lower beds called Combe rock, a mixture of chalk and flint with yellow clay, have been pitched and washed by... More
The Quarterly journal of the Geological Society of London (12961131495...
1869.. HFLL GEOLOGY OP CHESHIRE. 183 of the great formation of Warwickshire. To the north and to the south of this barrier the Permian formation exists under two distinct phases or types of character ; and... More
The Quarterly journal of the Geological Society of London (12961138253...
Qirapi J ourn. Geol . Sog .PI XX7. PI .11 ^1 ttytr-^. ,-j- ^— _. JWSal-er M&K.Ha7ihdz-L..th MENEVIAN TRILOBITES.
The Quarterly journal of the Geological Society of London (12961165723...
TYLOR QUATERNARY GRAVELS. 67 Junction ; the river under the viaduct is 325 feet above the mean level of the tide at Liverpool. The rails of the Taif-Yale line are 96 feet above the Taff at Quaker's- Yard Ju... More
The Quarterly journal of the Geological Society of London (12961318793...
1869.. KATTHAY CAPE-YOKK PENINSULA. 299 Mount Bremer (409 ft., see Map). In all, the porphyry presents nearly the same lithological characters, and consists of a matrix of felspar enclosing numerous crysta... More
The Quarterly journal of the Geological Society of London (12961033115...
74 PKOCEEDIlSrGS OP THE GEOLOGICAL SOCIETY. dation than can be obtained from natural sections in brooks, where the different gravels are moved and mixed up together by the recent action of water. The total ... More
The Quarterly journal of the Geological Society of London (12961112575...
130 PROCEEDJNGS OF THE GEOLOGICAL SOCIETY. .DeC. 23, of the village of Tungiiu, twelve miles outside the Taiping gate, to the Chung-shan, where it attains a height of about 1700 feet, and thence descends ag... More
The Quarterly journal of the Geological Society of London (12961201233...
TYLOR QrATERNART GRAVELS. 85 will give an idea of the surface -configuration of the Thames valley and of the position of the fossiliferous gravels. The top bed of the Chalk and the basement bed of the Thane... More
The Quarterly journal of the Geological Society of London (12961245023...
1868.. KINGSMILL GEOLOGY OF CHIJfA. 121 1^ Kintse-schan pass (750 ft.). Coal. Ankowan (village). Coal-mine (closed). Fossils in chert. Summit 850 ft. p— 4 c3 o 02 -^^-' 2Q &0 •r-( PhO Oi c3 ... More
The Quarterly journal of the Geological Society of London (12961316143...
278 PROCEEDINGS OF THE GEOLOGICAL SOCIETY. .May 12, decay I have not noticed on Dartmoor (unless perhaps the primary hollows of the rock basins have been caused by it), but the con- verse takes place ; the ... More
The Quarterly journal of the Geological Society of London (12961612764...
Quajt. Journ.Geol. Soc.Vol.IXy. PHI c--. E FIELCniGr LITE PHOLIDERPETO.^ M & N HAirHAJB.T IMP
The Quarterly journal of the Geological Society of London (12961662964...
1869.. EGEKTON GTRODTJS. 385 but from this it differs in having the median teeth circular, instead of transversely oval. Another specimen belonging to Mr. Mansel is one of great in- terest. There has long... More
The Quarterly journal of the Geological Society of London (12961678104...
1869.. MACKINTOSH LANCASHIEE AND CUMBERLAND DRIFTS. 409 a. Upper Boulder-clay. — The existence of an Upper Boulder-clay along the coast is clearly defined. It stretches into the interior to an unknown dist... More
Quarterly Journal of the Geological Society of London, Volume 25, 0162...
Illustration in the Quarterly Journal of the Geological Society of London, volume 25
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Illustration in the Quarterly Journal of the Geological Society of London, volume 25
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The Quarterly journal of the Geological Society of London (12961001075...
Quart. Jonm. Geol. Soc Yol .XK7. PI TIT. P.JjajJjPeL'llcid liLh
The Quarterly journal of the Geological Society of London (12961168593...
68 PROCEEDINGS OF THE GEOLOGICAL SOCIETY. through a deep railway- cutting, the rails being 80 feet below the surface of the ground, and 112 feet below the adjoining peak of rock at D. The escarpment of roc... More
The Quarterly journal of the Geological Society of London (12961214363...
90 PEOCEEDINaS OP THE GEOLOGICAL SOCIETY. of what is there called boulder-clay, just as the stratified fossiliferous gravels at Erith are close to and interstratified with the non-remanie but moved Tertiari... More
The Quarterly journal of the Geological Society of London (12961238355...
Quart, Jourri.Geol Soc Vol.XW PI XVIII Ft(^:i .\ Fi^.2 Ft^f. 3. (i-.) FieldrnjS lith. MT .k N Hanhart imp STEFEOSAURUS EROM KIMMERIDGE.
The Quarterly journal of the Geological Society of London (12961265145...
450 PKOCEEDIKGS OF THE GEOLOGICAL SOCIETY. deposit is met with, the position of which, however, is essentially different from that found at Broomhill. From a careful survey which Plan of Gravel Hill, Brando... More
The Quarterly journal of the Geological Society of London (12961274503...
1869.. HTTLL GEOLOGY OF CHESHIRE. 181 c 2 q3 .D 0.3 o o C3 CD C3 CD a o 1— H fi o o o c3 Q •J a S Is ^ O) CO c3 S 'o Oi O O (D Jw p CO .D JiJ -^ .a -l -—1 te Si Q -S ,^ .2 45 c!... More
The Quarterly journal of the Geological Society of London (12961609914...
308 PKOCEEDINGS OF THE GEOLOGICAL SOCIETY. .May 26, was unknown to M. Pictet at the time he published his work, I here append the drawings I made in 1848 from specimens formerly in the possession of the lat... More
The Quarterly journal of the Geological Society of London (12961668804...
Qusrl.Jinirn.&ecl.SoeTol.irV.Pl.XVII. ru,'2..-ir) ^'"■■idini h;,h STENEOSAURUS FROM KIMMERIDGE M8(i; na'-naj'l lift
The Quarterly journal of the Geological Society of London (12961080975...
94 PROCEEDINGS OF IHE GEOLOGICAL SOCIETY. Fig. 28 is a careful sketch of part of the Cyrena-bed, by Mr. S. Skertchly. The section is as follows, in ascending order : — sands 4 feet, wavy laminated brick-ear... More
The Quarterly journal of the Geological Society of London (12961158265...
1869.. MOEaAKS — SPATHOSE-IEON-OKE TEINS. 255 mentions a tunnel, 430 feet above the sea-level, bored through the whole thickness of one of the seams for a distance of between 150 and 250 feet. A cross tunn... More
The Quarterly journal of the Geological Society of London (12961283933...
218 PROCEEDINGS OF THE GEOLOGICAL SOCIETY. POSTPONED PAPEE. On DAKOSATJErs from the Ximmeeidge Clat of Shototee Hill. By J. Wood Masoi^, Esq., E.G.S. (Eead Not. 25, 1868*.) Eaely in the spring of 1866 I... More
The Quarterly journal of the Geological Society of London (12961328673...
Quart JouraGcul .WolXXyRin ^ ' .sSr ■^-pp-^-fi JAAA'^OF MEC-ALOSAUKUS.
The Quarterly journal of the Geological Society of London (12961482284...
82 PKOCEEDINGS OF THE GEOLOGHCAL SOCIETY. In the middle of the Sangatte series a line of chalk boulders, de- posited at an angle of 12°, is shown in some places. At about half a -pig. 14. — Section of Cliff... More
The Quarterly journal of the Geological Society of London (12961519584...
TYLOR QUATEENAEY GRAVELS. 95 The Cyrena-bed varies from 4 feet to 6 feet (D, fig. 29) in thick- ness, and consists of false-bedded sand containing a great number of small and delicate shells in a perfect st... More
The Quarterly journal of the Geological Society of London (12961526324...
TYLOR QUATERNAEY GRATELS. 97 tell from the appearance of the surface that such a cavity had existed. There must have been a wash of gravel all over the sand to have furnished the material to fill up such ca... More
The Quarterly journal of the Geological Society of London (12961499574...
88 PROCEEDINGS OF THE GEOLOGICAL SOCIETY. tificial excavation, if other sections, such as fig. 19, did not exist close by. The gravel (c) fills up the inequalities in the sand. Fig. 20. — Section in Erith P... More
The Quarterly journal of the Geological Society of London (12961550584...
1869.. HTJXLET HTPERODAPEDON. 145 is, it measures 1*5 in. in length ; and the palatine surface has a width of 0-25 in. in front and 0-55 in. behind. The section of the bone is trihedral, the outer face of ... More
The Quarterly journal of the Geological Society of London (12961696064...
Quart, Joum.Geca.Soc. Vol. XXV PI. XX, "'"' Mjirlt/ttv- Creek ^M ^ ^C3. SJn-ub Bm BiooniMl "WMteffiU Gravel HUL IlvFMTvom X akenlieaih. FI)imsifTfidit,Wi: 2%£ml-furd S' Cavait Garden . o« DTCAc Mrtn^^.... More
The Quarterly journal of the Geological Society of London (12961691314...
MarL Jouni Geol ooc Vol.Xv/ PL XIX. Fv^.l j:r^.2 . Fw. .V Is V/i^je 11 !h 'vr 't- W Ha.rtii^ ri •iri^.
Geological Society of London, vol. 25 - Fig 19
Fig. 19.—Section in Erith Pit. (Natural scale.)
The Quarterly journal of the Geological Society of London (12961014775...
62 PEOCEEDINGS OF THE GEOLOGICAL SOCIETY. boniferous Limestone, one branch coming from a cave near Gbrdale Scar, then flows over the very thick formation of Millstone-grit, reaches the Coal-measures between... More
The Quarterly journal of the Geological Society of London (12961087745...
96 PROCEEDINGS OF THE aEOLOGICAL SOCIETY. at a height of 140 feet, it is only covered by 6 feet of gravel, while in fig. 30 it is covered by about 50 feet of the Quaternary series. Pig. 31 is a drawing t... More
The Quarterly journal of the Geological Society of London (12961101575...
122 PBOCEEDINGS OF THE GEOLOGICAL SOCIETY. .DoC. 23, River, a tributary of the former flowing past Kweilin-fu, the capital of Kwangsi province. In the valley of Modo, near Soochow, in Kiangsu, a fine sectio... More
The Quarterly journal of the Geological Society of London (12961164485...
276 PEOCEEDINGS OF THE GEOLOGICAL SOCIETY. .May 12, A sKght inspection of a tor will in most cases show that the form in which it now appears is caused by lines of joint. In those where the granite is crysta... More
The Quarterly journal of the Geological Society of London (12961185095...
Quart: Jo\o:n. Geol. Soc. VnlXSV, TlSKttl
The Quarterly journal of the Geological Society of London (12961280663...
1869.. WILTSHIRE HUNSTANTON EED CHALK. 185 2. On the Ued Chalk of Hunstanton. By the Rev. T. Wiltshire, M.A., FX.S., F.G.S. Not far from the apex of the angle which the Wash, opening out into the German O... More
The Quarterly journal of the Geological Society of London (12961352723...
1869.. ULRICH — ^' NUGGETTT REEF." 331 tioned, suceessM in striking the former vein above the granite. Figs. 5, 5a, 5b represent these relations of the " horse," reef, and intrusive vein. The third vein o... More
The Quarterly journal of the Geological Society of London (12961368223...
Qiudil, JourrL_Geol. Soc.VolXXY. Pl.XV. WH.Bai^ Jcr^rer&C^lmp.Dui;! AMTPJM FOSSIL PLAKTS.
The Quarterly journal of the Geological Society of London (12961346043...
1869.. ULEICH '* NTJGGETTT REEF." 329 of 20 feet, where it cuts into the western wall (fig. 3). It extends with a slight northerly dip to a depth of 120 feet, terminating there quite abruptly in the reef; ... More
Quarterly Journal of the Geological Society of London, Volume 25, 0168
Illustration in the Quarterly Journal of the Geological Society of London, volume 25
Quarterly Journal of the Geological Society of London, Volume 25, 0176...
Illustration in the Quarterly Journal of the Geological Society of London, volume 25
The Quarterly journal of the Geological Society of London (12961025285...
70 PROCEEDINGS OF THE GEOLOaiCAL SOCIETY. top surface of tlie bed of stones on which it lies, just as the last bed is almost parallel with the mean angle of the surface of the rock on which it is spread by ... More
The Quarterly journal of the Geological Society of London (12961074675...
92 PKOCEEDINGS OP THE GEOLOGICAL SOCIETY. for a long time. The chalk is excavated at the tramway to 20 feet above the Ordnance datum-line, and, is 55 feet high at E, where the Thanet sands (B) are nearly in... More
The Quarterly journal of the Geological Society of London (12961141423...
OiJ^-L.JouTTi.GeoL Soc YolJJVV^ W J.W.Salter fecib M(fcN JIaxLharb.imp. PARAD OXIDE S HICKSU , SaZter.
The Quarterly journal of the Geological Society of London (12961154825...
Quart,. Jo-Qm .Geol . So c Vol JIXV.PIa . V7. Ct S-mith F .L, . &.Jitii , W.West TDiD STKUCTUKE OF SIGILLARIA.
The Quarterly journal of the Geological Society of London (12961188135...
1869.. JOASS SUTHERLAND GOLD-FIELD. 319 gneissose strata (fig. 2). In a paper "On the Metamorphic Rocks of the Banffshire coast, the Scarabins, and a portion of rig. 1. — Section showing Granite in Mica-sc... More
The Quarterly journal of the Geological Society of London (12961218173...
TYLOR QUATERNARY GRAVELS. 91 gradient of 1 in 25 in that part. Only 48 feet in height is shown in fig. 23. The sketch is to natural scale ; so that the angles of the escarpment of chalk are not exaggerated.... More
The Quarterly journal of the Geological Society of London (12961337563...
320 PKOCEEDINGS OY TELE GEOLOGICAL SOCIETY. .June 9, while at the opposite point of contact on the S.E. the existing dip might remain comparatively unaffected. The upheaval along this line of fault, vrith w... More
The Quarterly journal of the Geological Society of London (12961492394...
S6 PROCEEDINGS OF THE GEOLOGICAL SOCIETY. west of A; but I have no doubt that the fossiliferous gravels, A B, will be found to lie in a similar concavity to those at Grays and Crayford, where the Thanet san... More
Geological Society of London, vol. 25 - Pl. VIII
Pl. VIII. Part of Erith, Kent.
The Quarterly journal of the Geological Society of London (12960981545...
14 PKOCEE DINGS OF THE GEOLOGICAL SOCIETY. .NoV. 25, m a p^ -^i 5* e« ■Si Of^ eg ^ w& m ill nil J I i •Fault. 0^ 02 § .1^ fl ni g fl .D -5 OS a ^ o -u 1 ^ c3 o to l—H 0) ... More
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240 TBOCEEDINGS OF THE GEOLOGICAL SOCIETY. .Maich 24, f5q . I, si) t£) o
The Quarterly journal of the Geological Society of London (12961147895...
242 1.R0CEEDINGS OF THE GEOLOGICAL SOCIETY. .Maicll 24, 2iid. Santonian stage: the lower part with Ostrea acutirostris, 0. santonensis, Spondylus truncatus, Janira quadricostata, SjphceruUtes Coquandi, and R... More
The Quarterly journal of the Geological Society of London (12961214835...
1869.. TATE GUYANA, m VENEZUELA. 347 I o CO I O o ^ CO o o ►31 « c3 o •to ^ "BTOnap •ij-Biuni "S. •iij'Bdis'Bnf) - ^ a* •ooouuo "a 5 § i »d 4j c. S .f^ (ft ti pq M .2 'fljOO o... More
The Quarterly journal of the Geological Society of London (12961223775...
382 PEOCEEDINGS OF THE GEOLOGICAL SOCIETY. .June 23, in making it the type of a new genus, Mesodoti, to which must be added Gyrodus gibhosus, Miinster, and Pycnodus liassicus, described by myself in the 8th ... More
The Quarterly journal of the Geological Society of London (12961194685...
324 PROCEEDINGS OF THE GEOLOGICAL SOCIETY. .JunO 9, eS SP^ 1—1 o 5Si ^ ^ eS CO o 5-1 .H 03 o the very general belief that it was richly auriferous. Two large parties of miners did indeed forcibl... More
The Quarterly journal of the Geological Society of London (12961356023...
332 PROCEEDINGS OP THE GEOLOGICAL SOCIETY. .June 9, whatever ; but it was found to be quite poor, nearly barren, under- neath the granite, though pretty rich above it, and the " horse " dividing the reef g... More
The Quarterly journal of the Geological Society of London (12961472864...
TTLOK QTJATEENARY GRATELS. '9 part it is 60°, S., curving gradually towards high-water mark. At b the raised beach of flint- shingle, with masses of slightly rolled chalk, is seen reposing on it, dipping to... More
The Quarterly journal of the Geological Society of London (12961444804...
TTLOE — QTJATEBN-AEY aElVELS. 61 it to lower levels into the valleys. At page 124, Quart, Jonrn. Geol. Soc. vol. xxiv., I described snch a flood, in Sind in the year 1866, when a rainfall of 24 inches occur... More
The Quarterly journal of the Geological Society of London (12961560064...
178 PROCEEDIITGS OF THE GEOLOGICAL SOCIEXr. .Feb. 10, -to Si O .H *' 3. Dividing ridge of Lower Carhoniferous Rocks (see fig. 2). 1 now come to the explanation which seems to me the most probable, and on... More
Quarterly Journal of the Geological Society of London, Volume 25, 0175
Illustration in the Quarterly Journal of the Geological Society of London, volume 25
The Quarterly journal of the Geological Society of London (12961004035...
The Quarterly journal of the Geological Society of London.
The Quarterly journal of the Geological Society of London (12961035625...
78 PKOCEEDINGS OF THE GEOLOGICAL SOCIETY. which, according to Dr. Blackmore, are associated with, flint instru- ments of the Amiens type. Land and freshwater shells are very- abundant. The great shell-bed ... More
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TTLOR QUATERNARY GRAVELS. 81 There is a bed of marl on the 6 feet of solid chalk, shown in fig. 13, Fig. 13. — Section of the Cliff East of the Ga^, Rottingdean, Sussex, W. E. and also continuous bands of f... More
The Quarterly journal of the Geological Society of London (12961108815...
1868.. KINGSMILL GEOLOGY OF CHINJl . 125 but in general, throughout the east and north-east of Kwangtung and the greater portion of Puhkien, igneous and metamorphic rocks form the most conspicuous geologic... More
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256 PROCEEDIlfGS OF THE GEOLOGICAL SOCIETY. .April 14 ting. The greater part of each vein is " dead " or unproductive ; the productive portions or " pockets " vary from a few yards to 100 fathoms in length ... More
The Quarterly journal of the Geological Society of London (12961211695...
340 PEOCEEDINGS OF THE GEOLOGICAL SOCIETY. .JuDO 9, formation obtained from Dr. Plassard, who was at Caratal while this stuff was being worked. Fig. 3. — /Section of Alluvial Digging near Nueva Providencia.... More