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Strata Collection (page 2)

Background imageStrata Collection: Sopwith Model VI: Intersecting mineral veins

Sopwith Model VI: Intersecting mineral veins
This 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

Background imageStrata Collection: Sopwith Model XI: Vertical intersecting veins

Sopwith Model XI: Vertical intersecting veins
This model, when separated, shows the complex interface between faulted strata of rocks. Thomas Sopwith (1803 - 1879) was an eminent geologist

Background imageStrata Collection: Sopwith Model XII: Mineral vein denudation

Sopwith Model XII: Mineral vein denudation
This model shows the influence of surface denudation and faulting on inclined strata, with increased complexity to the situation in Model VII

Background imageStrata Collection: Sopwith Model VIII: Overcutting of strata

Sopwith Model VIII: Overcutting of strata
This 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

Background imageStrata Collection: Sopwith Model VII: Surface denudation

Sopwith Model VII: Surface denudation
This 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

Background imageStrata Collection: Sopwith Model X: Denuded basset of strata

Sopwith Model X: Denuded basset of strata
This 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

Background imageStrata Collection: Sopwith Model V: Dislocations of coal strata

Sopwith Model V: Dislocations of coal strata
This 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

Background imageStrata Collection: Sopwith Model IV: Fallacious coal indications

Sopwith Model IV: Fallacious coal indications
This model depicts the scenario where from the surface an abundance of coal appears to exist, but there is actually very little quantity below

Background imageStrata Collection: Sopwith Model III: Dislocation of strata

Sopwith Model III: Dislocation of strata
This model represents the side of a valley of denudation, with undisturbed horizontal beds of sedimentary rock when fully assembled

Background imageStrata Collection: Sopwith Model I: Stratified rocks / denudation

Sopwith Model I: Stratified rocks / denudation
Black lines in this model represent coal seams, between lighter shales and sandstones. When separated the lower section shows a gently inclined valley floor

Background imageStrata Collection: Sopwith Model II: Coal strata nr Newcastle

Sopwith Model II: Coal strata nr Newcastle
Unlike 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

Background imageStrata Collection: Cover of Thomas Sopwiths Geological Model Set

Cover of Thomas Sopwiths Geological Model Set
Thomas Sopwith (1803 - 1879) was an eminent geologist and civil engineer who pioneered methods of representing geological features

Background imageStrata Collection: Thomas Sopwiths Geological Model Set

Thomas Sopwiths Geological Model Set
Thomas Sopwith (1803 - 1879) was an eminent geologist and civil engineer who pioneered methods of representing geological features

Background imageStrata Collection: Elderly lady not overly generous with her tipping

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

Background imageStrata Collection: Tramp asks a horrified lady for a hairpin to clean his pipe

Tramp asks a horrified lady for a hairpin to clean his pipe
A 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

Background imageStrata Collection: Outlying rocks, Bermuda 1873

Outlying rocks, Bermuda 1873
A photograph taken during the voyage of H.M.S. Challenger (1872-1876), funded by the British Government for scientific purposes

Background imageStrata Collection: Rock structure, Burmuda 1873

Rock structure, Burmuda 1873
A photograph taken during the voyage of H.M.S. Challenger (1872-1876), funded by the British Government for scientific purposes

Background imageStrata Collection: Fossilised Tellinella rostralis, tellin bivalve

Fossilised Tellinella rostralis, tellin bivalve
Fossilised 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

Background imageStrata Collection: Peculiar stratifications just outside the dockyards, Bermuda

Peculiar stratifications just outside the dockyards, Bermuda
A photograph taken during the voyage of H.M.S. Challenger (1872-1876), funded by the British Government for scientific purposes

Background imageStrata Collection: Rock formation, Bermuda 1873

Rock formation, Bermuda 1873
A photograph taken during the voyage of H.M.S. Challenger (1872-1876), funded by the British Government for scientific purposes

Background imageStrata Collection: Fossil tooth of some extinct monstrous unknown animal from W

Fossil tooth of some extinct monstrous unknown animal from W
Plate 1 from Strata Identified by Organized Fossils by William Smith (1816-1819) (Mastodon arvernensis Croizet & Jobert from Norwich Crag, Pleistocene)

Background imageStrata Collection: Lower Chalk

Lower Chalk

Background imageStrata Collection: William Smiths geological table

William Smiths geological table
Fig 2 from Delineation of Strata of England and Wales (1815) by William Smith

Background imageStrata Collection: Volcanic eruption

Volcanic eruption
A flood basalt eruption. One of a series (including image numbers 185 to 190) showing various forms of volcanic eruption

Background imageStrata Collection: Slipped Strata

Slipped Strata
A fine example of slipped strata, on the rocky Pembrokeshire coast, at Port Stinian, near St. David s, Wales. Date: 1950s

Background imageStrata Collection: Societys 3 Orders

Societys 3 Orders
A 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

Background imageStrata Collection: Lulworth Cove Strata

Lulworth Cove Strata
Contorted strata in the famous cliffs at Lulworth Cove, Dorset, England. Date: 1960s

Background imageStrata Collection: Strata Florida Abbey

Strata Florida Abbey
The remains of the magnificent West Doorway at Strata Florida Abbey, Cardiganshire, Wales, founded in 1091 by the Cistercian Order. Date: founded 1091

Background imageStrata Collection: Sandstone Strata

Sandstone Strata
Sandstone rock strata. Date: 1960s

Background imageStrata Collection: Quarry Strata Exposed

Quarry Strata Exposed
View of a quarry section or cutting showing the exposed strata Date: circa 1860

Background imageStrata Collection: Excavations at Troy

Excavations at Troy
An 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

Background imageStrata Collection: Stratification Diagrams

Stratification Diagrams
Two 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

Background imageStrata Collection: Middleton Dale, Derbyshire

Middleton Dale, Derbyshire
Limestone Rock in Middleton Dale, Derbyshire

Background imageStrata Collection: Class System in China

Class System in China
A 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



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