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CUL-DAR30.36-69    Note:    1832.04.00--1832.06.00   Zoological diary: Rio de Janeiro   Text   Image
affected) June 8th.— From this fact of Cumili. with edge clearly defined against the blue sky, floating on a calm hot day. under 2000 feet of elevation. a landscape introducing it faithfully had to my eye, an unnatural appearance, although well aware of the truth of the fact.— On May 5th 17th there was a good instance of an appearance, which I had frequently witnessed with surprise on the Rio Macaè.— In both all cases for some hours the country had been drenched with rain; as soon [as] it ceased a
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CUL-DAR30.77-99    Note:    1832.08.00--1832.09.00   Zoological diary: Patagonian coast   Text   Image
transverse bands.— fins leaden colour.— beneath obscure: pupil dark blue.— When caught vomited up small fish a Pilumnus.— Mr Earl states these fish are plentiful at Tristan d Acunha, where it is called the Devil fish, from the bands being supposed the marks of the Devils fingers.— Was tough for eating, but good.— This sort was taken in very great numbers.— Fish (c) copied 354 354 Above pale Chesnut brown so arranged as to form transverse bands on sides: Sides, head, fins, with a black tinge: beneath
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CUL-DAR30.100-116    Note:    1832.09.00--1832.10.00   Zoological diary: Bahia Blanca   Text   Image
The Complete Work of Charles Darwin Online 100 Bahia Blanca 1832 Septemb: Fish 390 Caught on a sand bank in the net:— body silvery: dorsal scales iridescent with green copper; head greenish: tail yellow. Fish 391 (a) Body pale, darker above; broard silvery band on sides; common:— Fish 392 Body mottled with silver green; dorsal caudal fins lead colour: common Fish 393 Back coloured like Labrador feldspar; iris coppery: plentiful Fish 394 Above dirty reddish brown; beneath faint blue; iris
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CUL-DAR30.100-116    Note:    1832.09.00--1832.10.00   Zoological diary: Bahia Blanca   Text   Image
(Lamouroux), the latter having the peduncle twisted, branches not jointed, generally short creeping.— This would appear from structure of Coralline to be more closely allied (as Cuvier ranks it) to the Tubularia than to the Sertulariæ.— I never saw anything more beautifully luminous than this Coralline was; when rubbed in the dark every fibre might be traced by the blue light.— What was remarkable was that the light came in flashes, which appeared regularly to proceed up the branches: The coralline
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CUL-DAR30.100-116    Note:    1832.09.00--1832.10.00   Zoological diary: Bahia Blanca   Text   Image
.— legs rather shorter, feathered to the claws; feathers same structure as in ostrich; hairs about the head.— cannot fly, is taken more easily than other ostrich with the balls.— This bird is however more universally known by its eggs, which are little inferior in size to the Rhea, but of a blue green colour. It generally frequent near the sea, frequently to the South of R. Negro, San Josè, I believe near the Colorado, but not further Northward.— V 212 more particulars.— The Northern Gauchos know
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CUL-DAR30.100-116    Note:    1832.09.00--1832.10.00   Zoological diary: Bahia Blanca   Text   Image
in so many distinct springs.— The body weighs from 20 to 25 pounds.— Lizard 454 455 Monte Hermoso.— In its depressed form general appearance partakes of some of the characters of the Geckos.— Colours above singularly mottled, the small scales are coloured brown, white, yellowish red, blue, all dirty, the brown forming symetrical clouds.— Beneath white, with regular spots of brown on the belly.— Habits singular, lives on the beach, on the dry sand some way from the vegetation.— Colour of body
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CUL-DAR30.100-116    Note:    1832.09.00--1832.10.00   Zoological diary: Bahia Blanca   Text   Image
posterior opening.— 6 pair of similar equal natatory legs; base jointed, with flat row of setæ ; (acting like caudal swimming in the Macrourus ) each one formed of row of strong setæ, on jointed base; At origin of leg is a small projecting point, or rudimentary leg, with few bristles:— there were no branchial plates.— Animal could swim laterally very rapidly, generally in circular direction; antennæ retracted: Shell hard elastic.— Animal coloured blue; in open ocean South of Corrientes.— [116v
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CUL-DAR30.141-149    Note:    1832.12.00--1833.02.00   Zoological diary: Tierra del Fuego   Text   Image
Tierra del Fuego 1833 Fuegian colours blue.— I suppose therefore it nearly pure alumina.— It occurs in the Slate Mountain, I imagine from the decomposition of the beds of Feldspathic rock.— The black I have not obtained: the black is I believe only charcoal oil:— Heteromerous insects 1021...24 (not spirits) copied The habitat of these insects was the most singular I ever observed: it was in the fissures of slate rock in which the genus Capulus was adhæring to the stone alive, therefore of
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EH88202334    Note:    1833--1835   Falkland notebook   Text   Image
at the Town A blue (patches blue white veins infinitely. in curious angular) white sandstone blue red clay upon sandstone [page 91a
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EH88202334    Note:    1833--1835   Falkland notebook   Text   Image
4th [August 1833] (1) B. About 120 feet high (whitish harder more siliceous Tosca) B A blue white sandstone C blue white with hard plates of sandstone A Tosca Gypsum impressiones of shells black linear cavities [page 90a
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
so. I almost traced the very junction: the blue thinly laminated blue slate; became more rotten, cleavage slightly curvilinear; crossed by other system at right angles so that it became a mass of splinters; vertical cleavage hardly perceptible changed color becoming greenish brownish, this was close to the Purple, [the] the stratum of which was inclined at less angle now in other case, the purple blue were conformable I strongly suspect that the mechanical beds above are influenced by that law
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EH88202328    Note:    1833   Port Desire notebook   Text   Image
Hills North of B. sound several [orients] (W E (?)) centre of island more confusion Thrush in flocks Experimentize with pods of Kelp. Nitre rapidly drying: Small Hawk iris honey yellow legs bright yellow . skin above blue beak do: male feeding on Carrion! (1926)1 Blue leg Vulture. Male.Super-abundance of inarticulate Corallines: Kelp Corallines 1 Specimen not in spirits 1926 in Zoology notes, p. 399, 'Ornithological notes', p. 233; listed as Milvago leucurus in Birds, pp. 15-18. [page 54
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
which are closely connected with nature of clay-slate: I saw above in one locality the conglom a little common blue slate: All these varieties seem blended in [one] hills without much order, in another section they alternated in very numerous strata: these formations extended far to the west, dipping to west with tame outline: I must remark that certainly the dip of these curious white soft beds is less than the laminated blue slate: in one case they appeared quite conformable, in another they
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
above and are engulphed. Protruded masses of chalk. But whatever opinion we may entertain on this point, we cannot doubt that subterranean a, Gravel and ferruginous sand, rounded and angular pieces of chalk flint, with some quartz pebbles, 3 feet. b, Laminated blue clay, 8 feet. c, Yellow sand, 1 foot 6 inches. d, Dark blue clay with fragments of marine shells, 6 feet. e, Yellow loam and flint gravel, 3 feet. f, Light blue clay, 1 foot. g, Sand and loam, 12 feet. h, Yellow and white sand, loam
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A904    Beagle Library:     Fitton, William Henry. 1833. Notes on the progress of geology in England. London: Richard Taylor.   Text
14. Marl Blue. 40 Round Bath. Pectenites, Belemnites, Gryphites, highly-waved Cockles.. Ochre Balls. Mineral springs of Lincombe, Middle Hill, Cheltenham. 14. Blue Marl (25). 15. Lias Blue 25 Same as the Marl with Nautilites, Ammonites, Dentalia, and Fragments of the Enchrini.. The fertile Marl lands of Somersetshire. Twerton, Newton, Preston, Clutton, Stanton Prior, Timsbury, Paulton, Marksbury, Farmborough, Corston, Hunstreet, Burnet, Keynsham, Whitchurch, Salford, Kelston, Weston
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EH88202331    Note:    1833--1835   B. Blanca notebook   Text   Image
Little mouse (male) 5 drams 59 gr 5 dram 29.81 (apoth) Gerboise (male) 3 oz (24 apothecary Avecasina female Young T. del Finch less brilliant. head less blue back less green belly more dirty orange 437.5 3 1312.5 24 2336 [page 73a
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EH88202331    Note:    1833--1835   B. Blanca notebook   Text   Image
June 2d. [1834] The most NE point of Clarence Island does not look like Slate. hills about M. Tarn NW ?? 8th [June 1834] Bad day for all but Sailor; curious scenery constant dirty cloud driving clouds peeps of rugged snowy crags: blue glaciers: rainbows squalls outline against the lurid sky: not fit for residence of has no claims no authority here [page 81a
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EH88202334    Note:    1833--1835   Falkland notebook   Text   Image
entirely composed of blue slate, generally very siliceous: he occasionally containing Lime; often pure quartz; often much iron. I here noticed very generally was that extreme sort of contorted cleavage in which every possible curve was present many resembling small [page 61a
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A904    Beagle Library:     Fitton, William Henry. 1833. Notes on the progress of geology in England. London: Richard Taylor.   Text
Marble Rock Great Oolite Clay Upper Oolite Under Oolite Fuller's earth rock Oolite Sand Marlstone Cornbrash. Forest Marble. Bradford Clay. Great Oolite (Bath). Fuller's Earth. Inferior Oolite. Sand and Grit. Marl Vales. 25 26 27 28 29 Blue Marl Lias Blue White Red Marl and Gypsum Magnesian Limestone. Soft Sand-stone Lias new Red sandstone Marl. Blue Lias. White Lias. Red Marl. Zechstein, Conglomerate of Exeter. Coal Tracts. 30 Coal Districts Coal-measures. Millstone Grit. Mountainous. 31 32 33 34
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
resembles the blue marl of the Subapennine hills, and, like it, encloses fossil shells and corals in a beautiful state of preservation. Of these I collected a great abundance from the clay, on the south side of the harbour of Syracuse, and twenty species in the environs of Caltanisetta, all of which, with three exceptions, M. Deshayes was able to identify with recent species*. From similar blue marl, alternating with yellow sand, at Caltagirone, at an elevation of about five hundred feet above the
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EH88202328    Note:    1833   Port Desire notebook   Text   Image
17th [January 1834] Cliff of S Barranca, 60 or 70 feet high: mun after gravel time for deposit of mud from a stream. on surface many mytili with blue colour fragments of oysters: There are many pebbles. some greenish; with quartz Feldspar not very porphyritic; also some phonolite fine black Basalt; Porphyries without crystals, light ferru: colour: Port Desire (20th ) [January 1834] [Port Desire section] (1) cellular 2 common 3 Breccia 4 Porph with Quartz + common [page 15
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EH88202328    Note:    1833   Port Desire notebook   Text   Image
pale white, projecting points pale halo edge with alternate spaces of narrow white blue, the latter color being fimbriated. beneath white, excepting mouth: tentac short terminal black eye: beneath which a bifurcate membrane: high up on rocks, near top of high water crawling on confervae nearly dry: Onchidium?1 Two small Turbos same locality. Pushed on to P. Chagua, same squally weather in several places on road, mass of alluvium hardened earth containing round 1 An intertidal slug. [page 98
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EH88202329    Note:    1833--1834   Banda Oriental notebook   Text   Image
sandstone occurs above the Limestone which is as I should suppose. for certainly the grit sandstone Limestone are all of a bed occurring above or in mortar Tosca beds here occurring above. at [Tres] Vivoras above clay. But I think from general local high position the red sandstone is a superior formation R R Negro fine river with fine blue water, well wooded; pretty valley. poor straggling town. (Curious pebble[s] from coast of Uruguay. Rincon de las Gallin[ac] [page 30
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EH88202329    Note:    1833--1834   Banda Oriental notebook   Text   Image
(Though little) I suppose the Oyster bed does thicken elevate itself, if as I it is, as I imagine: flow from the Andes the above Lava will be higher than Crater hill. Lions scratch ground: killed 2 Guanacoes, Condors eat one Cordilleras in full view. Clouds Climate River, blue narrower. Lava streamlets: The general absence of pebbles in all beds. except this one lowest, shows how entirely the Porphyry pebbles depend on [page 87
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EH88202334    Note:    1833--1835   Falkland notebook   Text   Image
Within [Basin] Slate slippy much laminated fossiliferous dipping to the N ½ E 65 ; from this to Vertical 22d [March 1833] true observ Slaty sandstone, abounding with fossils dipping 14 to W by S: layer of shells a seam of hard [blue] conchoidal slate. shells parallel to seam of slate strata. covered above beneath by the vertical plates of slate dipping to N ½ E: Fissil cleavage of slate same above beneath nearly vertical: Sandstone bed about 4 feet thick [page 15a
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EH88202334    Note:    1833--1835   Falkland notebook   Text   Image
Friday 10th. [May 1833] A few miles beyond sleeping place; crossing the Salco the country became more elevated hilly. hills 3- to 500 feet high more stony. the rock generally more or less perfect gneiss; some quartz; also a little blue siliceous slate: our [course] was about NN by N. in this journey we were generally upon high land: but it was impossible to trace any very regular course of hills, after leaving the Sierra Larga: [page 36a
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EH88202334    Note:    1833--1835   Falkland notebook   Text   Image
country except Maldonado: The vendas miserably uncomfortable, as they have no rooms it is necessary to lounge all day evening amongst drunken strangers. Saturday 11th. [May 1833] Near At Minas there is a coarse blue, also pale slate: also much quartz. some pink granular dipping to NNE. There would seem to be a W E range of hills N of Minas N S, E of Minas: [page 39a
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EH88202334    Note:    1833--1835   Falkland notebook   Text   Image
been chiefly north) (NB. before Minas in the gneiss there was some siliceous blue slate) (NB. Examine peat at M. Video) After then much Syenite in abrupt paps or cones: then chiefly quartz: Our view to the East showed a much more level country: we travelling along hills the same as before: The country is precisely the same as formerly the people all look at me rather kindly [page 45a
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EH88202334    Note:    1833--1835   Falkland notebook   Text   Image
General stuff formation (1) sandstone varying much in hardness: it is generally blackish, with stalactitic particles harder. Black true cavitities. separation lines sometimes resembling beds in Buenos Ayres. parts with cleavage from currents many lines Greenish blue with little [illeg] also white beds: Above (A) thin bed of Argillo-Calcareous rock with dendritic margins vide [Lovett]1 specimens: has a alliance to B Blanca: In the section further (to SW) 1 Lovett, if correct, has not been
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
a series much inferior in thickness, consisting of a calcareous sandstone, conglomerate and schistose limestone, and beneath this again, blue marl. The whole of the above groups contain shells and zoophytes, nearly all of which are referrible to species now inhabiting the contiguous sea. a, Great limestone of Val di Noto. b, Schistose and arenaceous limestone of Florida, c. c, Blue marl with shells. d, White laminated marl. e, Blue clay and gypsum, c. without shells. Great limestone formation (a
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
Genoa. At Genoa the tertiary strata consist of blue marls like those of the northern Subapennines, and contain the same shells. On the immediate site of the town they rise to the height of only 20 feet above the sea, but they reach about 80 feet in some parts of the suburbs. At the base of a mountain not far from the suburbs there is an ancient a, Ancient sea-beach. b, Blue marl with shells. C, Inclined secondary strata of sandstone, shale, c. beach, strewed with rounded blocks of Alpine rocks
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
are often covered by a thin pellicle only of tertiary strata, which rests horizontally on the chalk and does not always conceal it. a, Siliceous sand without shells. b, Gravel. c, Sand and marl with shells. d, Blue marl with shells. E, Chalk and volcanic tuff. In the valleys of the Adour and Luy, section of all the members of the tertiary series are laid open, but the lowest blue marl, which is sometimes 200 feet thick, is not often penetrated. On the banks of the Luy, however, to the south of
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EH88202328    Note:    1833   Port Desire notebook   Text   Image
9th. [January 1834] Arrived Port St Julian. Went on shore with Captain. Came in at night. 10th [January 1834] Up harbor mud-banks. late at night Country rather better appearance: Mud in St. Julian constant rolling of pebbles: Gecko, being kept for some days colour uniform colour grey Compare with Blowpipe Mytilus1 with blue shells from Barranca 16th [January 1834] Pebbles at top of woods Mount of usual ferruginous colour: plain of diff. height: oysters Turritella high up: Then a 1 A mussel
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EH88202331    Note:    1833--1835   B. Blanca notebook   Text   Image
in evening like frogs: few Vultures watching for them to be killed: too much appearance danger (like salted meat) dog bark jump up: Pteru-Pteru when playing at cards by firelight cry heads inclined horrible looking men: Game at balls distance 35 yards but about one in 4 or 5 times: could throw them at between 50 60: Carranches do not run like Cuervos1 eggs in cliffs. colour oveiro cry like Spanish G N: at Sauce saw other sort, legs bill blue, feathers light brown. except crown of head eyes
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
enormous masses still resplendent clear dark blue cloudless sky (some little Puna1 ) very little vegetation, no birds or insects. Old Indian house. after crossing great pile of alluvium Cuesta del [Indio]. striking bed of lake: cattle: Slept with Vaccaros. Valle del Yeso. Cold Summit purple rock. Condor. 2 large white eggs no nest lay in November or December a whole year before can fly. are called condors 1 'The short breathing from the rarefied air is called by the Chilenos, Puna', Beagle
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
with the slope which for a distance of nearly 10 miles forms a considerable angle with the Pampas vegetation exactly like R. Negro. Where Porphyry low ranges were nothing but pebbles from them. Further in the plain [large] rounded blocks of Granite: NB. Beside (ejected?) red Porphyry, there were other hills of whitish do did not start till midday, ascended volcanic beds view of Pampas: dark blue, from rising Eastern sun: striking line of glittering water lost in immense distance: very level to
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
Alameda pretty, very kept. Cordilleras tame: scenery no comparison with St Jago: very quiet. Big bones. R. Quarto Los Gigantes Governor polite old man everyone polite in these countries the commonest peons looking at a old black woman with large goitre touched his hat respectfully evidently as an apology for looking at her: (29th). [March 1835] no Blue Sparrow = Aparea = Queriquincha1 very fine grapes: extreme heat dust of plain. Goitres 1 Nine-banded armadillo. See specimen in spirits 375
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
Soda? other brooks higher up purgative: Greywacke (16) alternates with fine blue laminated clay slate (17), which certainly is more abundant more [page 158a
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
in the interior: dip of nearly all the slate is high 45° to 80° I really cannot tell whether cleavage or strata. the main band runs N S a great formation, the lower ban ridge chiefly runs NE SW: the dip at in these high hills dips all westerly or towards the hills; ascending (Blue clay slate in very regular strata traversed at rt 's by many quartz veins) found the Clay Slate covered by purple variety in all parts, this again by a coarse softish white Breccia Conglomerate (18) particles of
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
other bays of the Mediterranean, which are surrounded by bold rocky coasts. The general resemblance of the Albenga strata to the Subapennine beds is very striking, the lowest division consisting of blue marl, which is covered by sand and yellow clay, and the highest by a mass of stratified shingle, sometimes consolidated into a conglomerate. Dr. Sasso has collected about 200 species of shells from these beds, and it appears, by his catalogue, that they agree, for the most part, with the
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
analogous to those which the contact of a fused mass might be supposed to produce. a, Granite. b, Limestone. c, Blue argillaceous schist. The above diagram from a sketch of Dr. Macculloch, represents the junction of the granite of Glen Tilt in Perthshire, with a mass of stratified limestone and schist. The granite, in this locality, often sends forth so many veins as to reticulate the limestone and schist, the veins diminishing towards their termination to the thickness of a leaf of paper or a
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
see purple blue clay slate apparently conformable right beneath the white rocks dipping about 30° westerly. I am still more strongly inclined to suspect that Falkland case here occurs: following the valley we have the white rocks (such as top of yesterdays mountain, this is just in the N S line seen running up the country but rather lower; there is not here so much of the purple rocks: see purple blue clay slate apparently conformable right beneath the white rocks dipping about 30° westerly. I
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
blue marl. In such cases we may suppose the deltas of rivers and torrents to have gained upon the bed of a sea where blue marl had previously been deposited. The upper arenaceous group above described sometimes passes into a calcareous sandstone, as at San Vignone. It contains lapidified shells more frequently than the marl, owing probably to the more free percolation of mineral waters, which often dissolve and carry away the original component elements of fossil bodies and substitute others in
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
natural archway, called by us, The Hole in the Wall. In this arched chasm the surf beat on the rocks with so much violence as to break fifty feet from their base, although but little wind was blowing at the time. The country looked like a large park, varied with hill and dale; exhibiting at times, through a luxuriant valley, the distant prospect of blue mountainous ridges. Upon their second approach to the coast of Natal, the landscape was equally beautiful; clusters of trees, hills, vales
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EH88202329    Note:    1833--1834   Banda Oriental notebook   Text   Image
Coexistence in feeling in Polyclinum Clytia1 flashes of light?? Cellaria [Crisia]2 Flustra c. [Thur] With exception of Porph. pebbles upper alluvium all quiet no anticlinal lines: High plains with gravel: low with earth: at time of upheaval. or Porph pebbles: Shells converted into silex yellow Carb of Lime. Ossiferous3 gypsum generally entirely destitute of shells: Paris Experimentation on shells in Sicily. Blue clay with Gypsum without shells Lyell Vol III P 644 1 'Clytia formerly included
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
white clouds. beneath brilliant where we were: hid the equally level Pampas. Entered the [band] clouds the region of bushes stopped at one oclock. In mist whole day. (Los Arenales) 24th [March 1835] Vegetation spring bushes. many flowers like Patagonia: Blue Orange finch long-tailed tit: tufted do. red-tail Furnarius. Guanaco dung in heap: just the same in appearance (Ulloa):1 very many mice: Biscatcha on a peak: very different aspect: more bushy tail. tinge of red in breast: Viviparous
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
(39: 40) The regular gold ores (41). (like clay) a veins just opened; contains some Pyrites deep down thought to be good sign. At the houses (Blue [Baize]): grand curious Porphyry beds of Lava: (42) a loose fragment but I do not doubt from same locality (43) The very limit where crystalline rock joins to a greenish rock like following: (44: 45) occur with the white aluminous sandstones: organic impressions comes from bed (1) in last section. (46) Metallic vein said to contain silver in above
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EH88202333    Note:    1833--1835   St. Fe notebook   Text   Image
of S. Stone, with more perfect generally a trace of gryphite1 (100) the most perfect shell an oyster (101). There was a white Limestone with line of little quartz pebbles white or red, like shot: above the Limestone same thickness of same color harder heavier (than those above) Conglomerate, matrix with slight trace of crystal (98). above this I believe Limestone, which [on] the first contains a hardened blue marl (102) with nodules of Limestone: we then have (Bed 2): I doubt whether this
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EH88202334    Note:    1833--1835   Falkland notebook   Text   Image
only gravel. It must be same for at Pozo there was green to blue sandstone Tosca. Here also salt lake banks of a well with nitre encrusting (Slept night as before Foxes howling around no water) R Colorado 12th [August 1833] about 3 leagues from sea plain very gradually lowers onto plain with clover Lachuza no spiny bushes called Pampas. I suspect must be Tosca plain of other side of River green short turf character of coast the same s aid to stretches to Union Bay with flat islands mud banks
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
. A diagonal lamination is often observable in the calcareous sandy beds analogous to that represented in the first volume (chap. xiv. diagram No. 6), and to that exhibited in many sections of the English crag, to which we shall afterwards allude. In some parts of the island this sandy calcareous division b, seems to be represented by yellow sand, exactly resembling that so frequently superimposed on the blue shelly marl of the Subapennines in the Italian peninsula. Thus, near Grammichele, on
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
along the shore, and projects about 60 yards in advance of the general line of cliff. One of its edges, at c, rests upon a. Chalk with flints. b. Gravel, of broken and half-rounded flints. c. Laminated blue clay. d. Sand and yellow loam. the blue clay beds of the crag, in such a manner as to imply that the mass had been undermined when the crag was deposited, unless were suppose, as some have done, that this chalk is a great detached mass enveloped by crag. For, [page] 18
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A904    Beagle Library:     Fitton, William Henry. 1833. Notes on the progress of geology in England. London: Richard Taylor.   Text
, imbedded. 1. Chalk (5). 2. Sand.. 70 The fertile vales intersecting Salisbury Plain and the Downs. 2. Greensand (6).Firestone. 3. Clay. 30 Between the Black Dog and Berkley. 3. Blue Marl (7). 4. Sand and Stone 30 5. Clay 15 Hinton, Norton, Woolverton, Bradford Leigh. Imbedded is a thin stratum of calcareous Grit. The stones flat, smooth, and rounded at the edges. 5. Forest Marble(17 18). 6. Forest Marble 10 A mass of Anomi and high-waved Cockles, with calcareous Cement. The cover of the upper bed of
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
now prevailing. Suppose, for example, there were three masses extending over every continent, the upper of chalk and chloritic sand; the next below, of blue argillaceous limestone; and the third and lowest, of red marl and sandstone; we must imagine that all the rivers and currents of the world had been charged, at the first period, with red mud and sand; at the second, with blue calcareo-argillaceous mud; and at a subsequent epoch, with chalky sediment and chloritic sand. But if the ocean
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A747    Beagle Library:     British Association for the Advancement of Science. 1833. Report of the first and second meetings, at York in 1831 and at Oxford in 1832, including its proceedings, recommendations, and transactions. London: John Murray.   Text
2. The solar spectrum and that of artificial flames, whether formed by prisms of transparent solids and fluids, or by grooves in metallic and transparent bodies, or by the diffraction of light passing through a narrow aperture, consist of three spectra of equal length, beginning and terminating at the same points (viz. a Red, a Yellow, and a Blue Spectrum), and having their maximum of illumination at different points of their length, and their minimum at their two extremities. 3. All the seven
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A747    Beagle Library:     British Association for the Advancement of Science. 1833. Report of the first and second meetings, at York in 1831 and at Oxford in 1832, including its proceedings, recommendations, and transactions. London: John Murray.   Text
, to another primary spectrum superposed in the same way; and similarly the chemical rays. He makes the following statements with respect to the heating rays. 1st, There is no proof whatever of the existence of invisible rays of any kind beyond the red or the blue extremity of the spectrum. Sir W. Herschel's experiments prove the existence of heat beyond the visible extremity of the spectrum which he used; but Sir D. Brewster has succeeded in rendering the spectrum visible at every point where
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A747    Beagle Library:     British Association for the Advancement of Science. 1833. Report of the first and second meetings, at York in 1831 and at Oxford in 1832, including its proceedings, recommendations, and transactions. London: John Murray.   Text
and by myself in the beginning of 1831 in an ore of lead from Wanlock Head, and before Sefstr m had published anything upon the subject. It approaches nearest to chromium in its properties, and lies in a natural arrangement between that metal and molybdenum. It is characterized by giving, in the form of oxide, blue salts with acids, with oxygen forming a peculiar acid, which fuses at a red heat without decomposition, and on cooling is reddish brown and crystalline, and which gives with bases
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
blue basalt with olivine. They vary in breadth from two to twenty feet and upwards, and usually project from the face of the cliffs, as represented in the annexed drawing (No. 19). They consist of harder materials than the strata which they traverse, and therefore waste away less rapidly under the influence of that repeated congelation and thawing to which the rocks in this zone of Etna are exposed. The dikes are, for the most part, vertical, but sometimes they run in a tortuous course through
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
inclined at an angle of 45 , and even more. a, Pebbles of chalk flint, and of rolled pieces of white chalk. b, Loam overlying a. c, c, Blue and brown clay. [page] 17
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
Crag and other formations*. This disposition of the layers is illustrated in the accompanying diagram, in which I have represented carefully the stratification of a coarse argillaceous schist, which I examined in the Pyrenees, part of which approaches in character to a green and blue roofing slate, while part is extremely quartzose, the whole mass passing downwards into micaceous schist. The vertical section here exhibited is about three feet in height, and the layers are sometimes so thin
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
as the day made us visible to the natives, they were observed making preparations on the Mafoomo side of the water to pay us a visit. The first who came was Jem of the Water, as he called himself. This fellow was in the native costume, which is literally worse than nothing, consisting only of a straw tube, about a foot long, with a shred of blue dungaree hanging from its upper end. He was ornamented by a necklace of charms, composed of small shells, eagles' talons, brass buttons, coloured beads
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
principally on the water's edge. The rivers are innumerable, but few are of any importance, some ejecting a muddy deposit, which discolours the sea for six or seven miles, bringing with it drift-timber and floating islets, on which water-fowl of various species were frequently observed at roost. The boundary of the river water was perfectly defined, and its light green colour afforded a remarkable contrast to the deep blue of the surrounding ocean. So great is the rush of the floods from the
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
seamen, and English Bill, as interpreter, formed the embassy; they took as a present a small quantity of leaf tobacco, some dungaree, or coarse blue cotton, and two bottles of rum. They were also accompanied by one of Makasany's Secretaries, who levied contributions of water-melons, pemba,* and fruits, for the use of the party, at several villages which they passed through. After a most fatiguing march of nearly sixteen * Beer made from millet. [page] 21
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
Their sheep are of the Tartar or large-tailed breed, with hair instead of wool; the price demanded for one was a fathom and a half of blue or check dungaree, and numbers of these, together with fowls and goats, were purchased for trifling pieces of the same stuff. For six fathoms, the old king sold fourteen ounces of good ambergris, worth, perhaps, twenty pounds. He had with him about as much more, but would not part with it, having procured as much cloth as he desired. Several women visited
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
mutual interest. The trade of Inhamban consists principally in ivory, and bees'wax, about one hundred thousand pounds of the former being annually conveyed to Mozambique. This article is obtained from the natives for blue dungaree, fishhooks, needles, c.; and so highly do they prize the last of these, that one of our seamen for a single needle procured two fullgrown fowls. The natives about Inhamban are entirely independent of the Portuguese, and, although they are ready to traffic with them, will
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
, honey, pompions, milk, and various sorts of shells, all which they willingly parted with for dollars, beads, blue dungaree (which they called clout), looking-glasses, and in fact nearly anything European. For French bottles these people would give nearly all they possessed, while an English one was despised. It may also here be remarked, that empty bottles are of great value upon the whole eastern coast of Africa, which our sailors soon became aware of much to the detriment of the captain's and
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
, on his last return to Mr. Arlett, had filled his trunk with mud, which, having turned him on his back, and forced open his mouth, he blew down his throat, injecting a large quantity into the stomach. It was this that produced the inflated appearance of Mr. Arlett's countenance, for he was almost in a state of suffocation, and for three days after this adventure, he occasionally vomited quantities of blue sand. When he encountered the elephant, he had a [page] 21
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
Bay. The rocks upon this coast appear of two or three different kinds, but principally sand-stone inhorizontal strata, in which petrifactions are imbedded; others are of primitive or volcanic substance of harder and more irregular structure. We saw many rivers completely blocked up by sandy beaches, but which, like Nourse's, were probably in the rainy season broad and rapid streams. As we advanced farther northward, the land was composed of red intermixed with tinges of blue clay and yellow
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A828    Beagle Library:     Stephens, James Francis. 1833. Description of Chiasognathus Grantii a new lucanideous insect forming the type of an undescribed genus, together with some brief remarks upon its structure and affinities. Transactions of the Cambridge Philosophical Society 4: 209-17.   Text
longitudinal wrinkles at the base, the inferior process very glossy and impunctate, colour rich copper, tinted with brilliant shades of a golden hue, the base and its appendage rich blue-green and iridescent; the curvatures bronzed-black; head bright golden-green, varying in tint with the light, the disc very glossy, remotely, but finely, punctate, bluish; the lateral and posterior margins of a variable golden hue, with the spinous processes of [page] 21
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A747    Beagle Library:     British Association for the Advancement of Science. 1833. Report of the first and second meetings, at York in 1831 and at Oxford in 1832, including its proceedings, recommendations, and transactions. London: John Murray.   Text
prove that immediately behind the retina and in connexion with it, there is a coloured membrane of a peculiar nature, distinct from the pigmentum nigrum. The eyes taken for the purpose of experiment were those of the ox and the sheep, in each of which the part in question, of a fine blue or green colour, appears at the back of the globe of the eye, immediately in contact with the retina, having behind it the true pigmentum. To prove the difference between this membrane and the pigmentum, the author
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A747    Beagle Library:     British Association for the Advancement of Science. 1833. Report of the first and second meetings, at York in 1831 and at Oxford in 1832, including its proceedings, recommendations, and transactions. London: John Murray.   Text
not oh any peculiar secreted matter, but on the general laws for thin plates. Examined with a fine achromatic microscope of Chevalier's construction, blood-vessels, and even the red globules contained in them, were visible in the membrane. By careful dissection in water, it is separable in distinct layers from the choroid. Its colour is frequently different in the same species of animals; it is usually blue in the ox, the pigment in the same animal being of a rich brown; in the cat and fox the
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
considering in the first place the more modern periods Geological structure of Sicily Formations of the Val di Noto of newer Pliocene period Divisible into three groups Great limestone Schistose and arenaceous limestone Blue marl with shells Strata subjacent to the above Volcanic rocks of the Val di Noto Dikes Tuffs and Peperinos Volcanic conglomerates Proofs of long intervals between volcanic eruptions Dip and direction of newer Pliocene strata of Sicily 62 CHAPTER VII. Marine and volcanic
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
LIST OF PLATES AND WOOD-CUTSIN THE THIRD VOLUME. PLATES. Frontispiece. View of the volcanos around Olot, in Catalonia. See p. 186. This view is taken from a sketch by the author; an attempt is made to represent by colours the different geological formations of which the country is composed. The blue line of mountains in the distance are the Pyrenees, which are to the north of the spectator, and consist of primary and ancient secondary rocks. In front of these are the secondary formations
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
analogous to that observed in the basin of the Seine*. But no two sets of strata could well be more dissimilar in mineral composition, and they were only recognized to belong to the same era, by aid of the specific identity of their organic remains. The discordance, in other respects, was as complete as could well be imagined, for the principal marine formation in the one country consisted of blue clay, in the other of white limestone, and a variety of curious rocks in the neighbourhood of Paris had
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
CHAPTER VI. Newer Pliocene formations Reasons for considering in the first place the more modern periods Geological structure of Sicily Formations of the Val di Noto of newer Pliocene period Divisible into three groups Great limestone Schistose and arenaceous limestone Blue marl with shells Strata subjacent to the above Volcanic rocks of the Val di Noto Dikes Tuffs and Peperinos Volcanic conglomerates Proofs of long intervals between volcanic eruptions Dip and direction of newer Pliocene
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
Etna, sometimes attaining a thickness of three hundred feet, or more, without any intermixture of volcanic matter. Crystals of selenite are dispersed through the clay, accompanied by a few shells, almost entirely of recent Mediterranean species. This formation of blue marl and yellow sand greatly resembles in character that of the Italian Subapennine beds, and, like them, often presents a surface denuded of vegetation, in consequence of the action of the rains on soft incoherent materials. In
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
the Subapennines, and he classed all the tertiary strata of Italy, from Piedmont to Calabria, as parts of the same system. Certain mineral characters, he observed, were common to the whole, for the strata consist generally of light brown or blue marl, covered by yellow calcareous sand and gravel. There are also, * Above, p. 54. [page] 15
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
discovery of an entire head or skeleton. Cadibona. Another example of an isolated lacustrine deposit, belonging possibly to the Miocene period, is that which occurs at Cadibona, between Savona and Carcare. Its position is described in the annexed section, which does not however a. Blue marl and yellow sand (older Pliocene). b. Sand, shale and coal of Cadibona (Miocene?). c. Green sand, c. of the Bormida (Miocene). d. Chloritic and micaceous schist, serpentine, c. pretend to accuracy in regard to the
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
green-sand.' It sometimes consists of loose siliceous sand, containing grains of silicate of iron, but often of firm beds of sandstone and chert. 2. Blue clay or calcareous marl, called provincially Gault. 3. Lower green-sand, a very complex group consisting of grey, yellowish, and greenish sands, ferruginous sand and sandstone, clay, chert, and siliceous limestone. 4. Weald clay, composed for the most part of clay without intermixture of calcareous matter, but sometimes including thin beds of
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
green-sand ('firestone,' or 'malm rock,' as it is sometimes called) is almost absent in the tract here alluded to. It is, in fact, seen at Beachy Head to thin out to an inconsiderable stratum of loose green-sand; but farther to the westward it is of great thickness, and contains hard beds of blue chert and limestone. Here, accordingly, we find that it produces a corresponding influence on the scenery of the country, for it runs out like a step beyond the foot of the chalk-hills, and
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
traction. The only thing that surprised us was to observe that many of the gentlemen enjoyed their delicious Havannah cigars in the ball-room without offending the ladies' nerves. In one of the churches may be seen the figure of St. Patrick decked in his original costume of green coat, yellow brogues, blue stockings, covering a purely Irish calf, a small hat stuck on one side of his head so as to leave fair space for a sprig of shillaleh to take effect upon the other; and his hand embellished
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
brought with them several hippopotamus' teeth, and one small elephant's tusk, requiring in exchange blue cotton stuffs for covering their heads and loins. By their information, it appeared that the river in that part was known among them by the name of Mahong, from a chief who had lately died and was succeeded by his son Chamborel. In the afternoon a young hippopotamus was perceived from one of the boats floundering about on the broad mud flat that skirted the right shore; [page] 8
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
number of wives that each man has is in proportion to his means. This Prince, or as English Bill called him, King, was a young man of short stature, with an intelligent good-humoured countenance. The only articles of clothing he wore were a neat blue jacket, and a red night-cap, decorated with a great profusion of beads and trinkets. From the extent of his domain, and the grain in his fields, he was accounted rich, of which Bill, by the way, took care to inform me, by saying, in his broken
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
the ship's company. Blue dungaree, or, as it is termed by the natives, lap, (corruption of cloth,) was the article in greatest request, and next to that, axes, knives, tobacco, and small black or white paste beads, which constitute the currency of the country. Rum, although much coveted, was not considered by the natives as an article of trade, but was accepted with avidity and thanks; they make two different kinds of liquor, one called Ep hl , and the other W c hny . The former is prepared in
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
some taste in their costume: they were habited in blue spencers, with long sleeves, fitting tight to the body, and ending just below the bosom, where the skin, for the breadth of an inch, was left exposed; this was succeeded by two pieces of cloth, the one serving as a petticoat, and the other as a gown, which were fastened by the ends being carefully tucked in between the body and the first folds that embraced it. None of them wore trinkets or ornaments of any kind, excepting a very few who
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
were easily acquired by the natives. The merchants having made their arrangements with Makasany, he allowed them huts in one of his own villages, not far from their vessels, when the trade commenced, but was carried on very slowly, according to the custom of all savages. The mode of bartering for elephants' teeth is as follows: they are brought to the place of exchange after they have been examined and sometimes weighed; the merchant puts down a certain quantity of blue calico or dungaree, beads
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
for slaves on the east coast. They are purchased with blue dungaree, coloured cloths, arms, gunpowder, brass and pewter, red coloured beads in imitation of coral, cutlery, and various other articles. The free blacks of the country and banyans carry on the trade inland for the merchants; and the arrival of one of these people among the tribes with his pedlar's stock is the signal for general warfare, when the weak become victims to the strong. Great faith is kept towards these mercantile agents
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A817.1    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 1.   Text
was discovered to be a boat. We arrested our course instantly, feeling confident that nothing so small would be out so far from the land from any other cause than necessity. As she approached, we perceived her to be a large canoe, with a sail formed by a small piece of blue dungaree and an old cotton sheet. In her sat four black men, haggard and emaciated in their appearance, while a fifth lay stretched at full length under the seats, apparently in a dying state. They lowered their sail, and
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
tooka, was rather shorter and of a darker tinge than his brother, the king, and by no means of so sedate a carriage. He generally dressed in a blue coat, epaulettes, and cocked hat, and his favourite amusement was shooting, during which he was always accompanied by a strong guard, rode on horseback, and was delighted whenever he could get an English officer to join him. His manners were particularly lively and prepossessing, and although not endowed with such extraordinary talents as his
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
low shed of rocky slabs. The earth was strewed with the bones of oxen, either slain there for an offering or as a burial-feast. There were also some sticks placed around, with small streamers of blue and white cloth pendent from them, and a China coffee-cup, carefully propped up over the grave. We again continued along shore until we made Nareenda Bay, the islands at the north entrance of which afford excellent harbours, and are approachable in most directions. Sancasse, the largest of them, is
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
means handsome, but gaudily dressed in white gowns, yellow silk handkerchiefs pinned over their shoulders, broad tinsel sashes round their waists, white open-worked silk stockings, and red kid shoes. Their hair was neatly plaited into a variety of small cords, knotted at the end, and hanging down in front as low as their eyebrows; but, when walking, they wore large French bonnets decorated with artificial flowers. Rafarla had on a plain blue coat with a pair of gold epaulettes, white waistcoat
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
a fish weighing about fifty pounds, which had, in all probability, been carried thither by the wolves or jackalls. We continued our course to Benguela, passing the low sandy point of Victoria, or St. Francis, after which we saw several native villages of straw huts; off one of these we hoisted our colours, which the inhabitants returned by holding up a small red flag with a black or blue cross upon it. The country was generally much more diversified, the valleys fertile [page] 23
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
an English slaver. Umbrellas here seemed to be emblematic of rank, for not a chief approached in his canoe without one held over his head by an attendant. There was nothing remarkable in the appearance of these people; all were perfectly black, but their noses were not so flat, or their lips so large, as amongst the generality of negroes. Their clothing consisted in a single wrapper of blue dungaree or printed cloth round their loins, hanging on one side to their ankles, while in front of their
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
to receive us, he was not to be seen, and it was intimated that we might remain outside until it suited his convenience. But, as such an arrangement did not suit ours, in spite of the Duke's entreaties, Captain Vidal entered, when we all followed him, and ascended by means of an awkward ladder to the first floor, where we found King Passol sitting at a table with his hat on, and clothed in a loose flowing garment of striped blue and white cloth. He was a tall, muscular, ugly-looking black
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
krall to be slain without distinction. One of his people in his presence happened, upon one occasion, to have something in his countenance, perhaps of the ridiculous, which had a tendency to disturb the serenity of the king's features. Take that man away and kill him, he makes me laugh, said Chaka. Like another Blue-beard, his embraces are a sentence of death. He says he wishes to live for ever, and his affectation of being so many years in acquiring the full maturity of a man seemed to be founded
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A817.2    Beagle Library:     Owen, William Fitz William. 1833. Narrative of voyages to explore the shores of Africa, Arabia, and Madagascar; performed in H.M. Ships Leven and Barracouta. 2 vols. London: Richard Bentley. Volume 2.   Text
many in consequence are driven to the necessity of subsisting one-third of the year on wild herbs. The slaves have no certain allowance, but live as they can, which is often by robbing their masters. For the purchase of grain in the interior it is necessary every season to send goods in advance, and the prices vary according to the produce. In years of great abundance, the blue dungaree is valued at fourteen cruzados the piece, and other articles at various prices; when the season has not
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A828    Beagle Library:     Stephens, James Francis. 1833. Description of Chiasognathus Grantii a new lucanideous insect forming the type of an undescribed genus, together with some brief remarks upon its structure and affinities. Transactions of the Cambridge Philosophical Society 4: 209-17.   Text
impunctate posteriorly, and produced into an abbreviated ridge, composed of two lunules; the colour is intense golden-green, with the anterior and posterior margins rich purplish-copper, varying in certain positions of light to blue and violet, especially towards the posterior angles, and the fove on the lateral margin are fine purplish-green; scutellum of this last tint, impunctate, its base clothed with short pale hairs in the centre; elytra very finely granulated throughout, except the humeral
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
strata, called 'the upper marine formation,' in the basin of the Seine, might be represented by all the Subapennine clays and yellow sand. English Crag. Several years before, an English naturalist, Mr. Parkinson, had observed, that certain shelly strata, in Suffolk, which overlaid the blue clay of London, contained distinct fossil species of testacea, and that a considerable portion of these might be identified with species now inhabiting the neighbouring sea . These overlying beds, which were
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
part of the bed of the sea is exposed to the excavating action of currents, while the greater part, remote from continents and islands, probably receives no new deposits whatever, being covered for ages with the clear blue waters uncharged with sediment. Here the relics of organic beings, lying in the ooze of the deep, may decompose like the leaves of the forest in autumn, and leave no wreck behind, but merely supply nourishment, by their decomposition, to succeeding races of marine animals and
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
hard blue lava of modern date has been furrowed in this manner by the rolling of blocks down a steep declivity. L 2 [page] 14
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A505.3    Beagle Library:     Lyell, Charles. 1833. Principles of geology, being an attempt to explain the former changes of the earth's surface, by reference to causes now in operation. 3 vols. London: John Murray. vol. 3.   Text
the recent predominate almost to the exclusion of the extinct. We shall now consider more particularly the characters of those Subapennine beds which we refer to the older Pliocene period. Subapennine marls. The most important member of the Subapennine formation is a marl which varies in colour from grayish brown to blue. It is very aluminous, and usually contains much calcareous matter and scaled of mica. It often exhibits no lines of division throughout a considerable thickness, but in other
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