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Sopwith Model VI: Intersecting mineral veinsThis Model, rather than representing the strata as they would appear at the surface, shows how a seam of coal can be displaced in the subsurface by various modes of faulting
Sopwith Model XI: Vertical intersecting veinsThis model, when separated, shows the complex interface between faulted strata of rocks. Thomas Sopwith (1803 - 1879) was an eminent geologist
Sopwith Model XII: Mineral vein denudationThis model shows the influence of surface denudation and faulting on inclined strata, with increased complexity to the situation in Model VII
Sopwith Model VIII: Overcutting of strataThis model shows overcut strata: when the layers of rock are inclined at a gentler angle than the eroded slope, the resulting vee pattern points uphill
Sopwith Model VII: Surface denudationThis model shows the influence of surface denudation and faulting on otherwise flat, horizontal strata. The discontinuity between the beds as viewed at the surface can be seen
Sopwith Model X: Denuded basset of strataThis model shows undercut strata: when the layers of rock are inclined at a steeper angle than the eroded slope, the resulting vee pattern points downhill
Sopwith Model V: Dislocations of coal strataThis model shows that while very little coal may appear at ground level, coal seams (subject to faults and dislocations) can be found below the ground
Sopwith Model IV: Fallacious coal indicationsThis model depicts the scenario where from the surface an abundance of coal appears to exist, but there is actually very little quantity below
Sopwith Model III: Dislocation of strataThis model represents the side of a valley of denudation, with undisturbed horizontal beds of sedimentary rock when fully assembled
Sopwith Model I: Stratified rocks / denudationBlack lines in this model represent coal seams, between lighter shales and sandstones. When separated the lower section shows a gently inclined valley floor
Sopwith Model II: Coal strata nr NewcastleUnlike the models of generic situations this representation of coal strata was specific to a particular surveyed location in England showing several thin, and mostly hidden, coal seams
Cover of Thomas Sopwiths Geological Model SetThomas Sopwith (1803 - 1879) was an eminent geologist and civil engineer who pioneered methods of representing geological features
Thomas Sopwiths Geological Model SetThomas Sopwith (1803 - 1879) was an eminent geologist and civil engineer who pioneered methods of representing geological features
Elderly lady not overly generous with her tipping" Have you got change for a threepenny-piece, Adolphus? I want to give the porter a gratuity." The porter appears to already be expecting the impending disappointment! Date: 1894
Tramp asks a horrified lady for a hairpin to clean his pipeA Tramp asks a horrified smart lady, seated on a park bench for a hairpin to clean his pipe! Weary Willy seating himself beside nervous Miss Jones) - Will yer lend me a nairpin, Lidy
Outlying rocks, Bermuda 1873A photograph taken during the voyage of H.M.S. Challenger (1872-1876), funded by the British Government for scientific purposes
Rock structure, Burmuda 1873A photograph taken during the voyage of H.M.S. Challenger (1872-1876), funded by the British Government for scientific purposes
Fossilised Tellinella rostralis, tellin bivalveFossilised specimen of a Tellin bivalve from Ecocene Belgium, 58 million years ago. Bivalves are hinged molluscs which first appeared in the Middle Cambrian some 500 million years ago
Peculiar stratifications just outside the dockyards, BermudaA photograph taken during the voyage of H.M.S. Challenger (1872-1876), funded by the British Government for scientific purposes
Rock formation, Bermuda 1873A photograph taken during the voyage of H.M.S. Challenger (1872-1876), funded by the British Government for scientific purposes
Fossil tooth of some extinct monstrous unknown animal from WPlate 1 from Strata Identified by Organized Fossils by William Smith (1816-1819) (Mastodon arvernensis Croizet & Jobert from Norwich Crag, Pleistocene)
Lower Chalk
William Smiths geological tableFig 2 from Delineation of Strata of England and Wales (1815) by William Smith
Volcanic eruptionA flood basalt eruption. One of a series (including image numbers 185 to 190) showing various forms of volcanic eruption
Slipped StrataA fine example of slipped strata, on the rocky Pembrokeshire coast, at Port Stinian, near St. David s, Wales. Date: 1950s
Societys 3 OrdersA cleric, a noble and a peasant represent the three strata of French society before the Revolution. Sadly, mutual hugging will soon change to lethal recrimination Date: eighteenth century
Lulworth Cove StrataContorted strata in the famous cliffs at Lulworth Cove, Dorset, England. Date: 1960s
Strata Florida AbbeyThe remains of the magnificent West Doorway at Strata Florida Abbey, Cardiganshire, Wales, founded in 1091 by the Cistercian Order. Date: founded 1091
Sandstone StrataSandstone rock strata. Date: 1960s
Quarry Strata ExposedView of a quarry section or cutting showing the exposed strata Date: circa 1860
Excavations at TroyAn interesting sketch showing the aftermath of Schliemanns excavations at the site of Troy. He had actually cut through Homerian levels and revealed earlier foundations! Date: 1888
Stratification DiagramsTwo diagrams to explain stratification: the books represent the different stratas in a depth of about 5 miles; the hand indicates depth of the coal strata Date: 19th century
Middleton Dale, DerbyshireLimestone Rock in Middleton Dale, Derbyshire
Class System in ChinaA cartoon of the Chinese class sytem, with people at the base surmounted by Clergy, who are supporting the Army (Braves), below Mandarins, with The Emperor at the very peak