Studio Shot Collection (page 5)

Clypeaster altus, a fossil echinoid
Clypeaster altus, 13 cm anterior to posterior, from the Miocene of Malta, oral view

Syringopora, fossil coral
Silicified colony of the tabulate coral Syringopora from the British Carboniferous. The tubular corallites are about 2 mm in diameter

Heliolites, coral
Small colony, 4 cm wide, of the tabulate coral Heliolites from the Silurian of England

Calcite (Calcium Carbonate) variant iceland spar
A cleaved rhomb of iceland spar showing double refraction from near Eskifjordr, Iceland

Agriocharis ocellata eggs
Eggs of Ocellated Turkey, Agriocharis ocellata, laid at the aviary at Knowsley Hall, Lancashire, from the Natural History Museum collections at Tring

Eopsaltria leucura
Mangrove Robin, Eopsaltria leucura, collected by John Gilbert in East Bay, Port Essington, Northern Territory, Australia

Pitta Iris, from the Gould Collection
Rainbow Pitta, Pitta Iris, specimen, collected by Captain Chambers in Australia between 1839 and 1841 Date: 1839

Xenus cinereus
Terek sandpiper, Xenus cinereus, specimen, collected by Captain William Chambers in the Cobourg Peninsula in Port Essington, Northern Territory, Australia

Rallus phippensis
Buff-banded Rail, Rallus phippensis, collected by JB Jukes in Port Essington, Northern Territory, Australia on August 1843 Date: 1843

Cacatua sanguinea, from the Gould Collection
Little Corella, Cacatua sanguinea, specimen collected by RA Bankier in Port Essington, Northern Territory, Australia, 14th December 1840 Date: 1840

Conopophila albogularis egg, Gould Collection
Egg of Rufous-banded honeyeater, Conopophila albogularis, collected by John Gilbert in Port Essington, Northern Territory, Australia on December 5th 1840 Date: 1840

Turnix castanota egg, from Gould Collection
Egg of the Chestnut-backed Buttonquail, Turnix castanota, collected by John Gilbert in Port Essington, Northern Territory, Australia, 5th March 1841 Date: 1841

Oriolus sagittatus affinis eggs
Eggs of Olive-backed oriole, Oriolus sagittatus affinis, found by John Gilbert in Port Essington, Northern Territory, Australia, 4th December 1840 Date: 1840

Dendrocygna arcuata australia eggs
Eggs of wandering whistling duck, Dendrocygna arcuata, collected by John Gilbert in Australia, 4th March 1841. All five are type specimens. Date: 1841

Eulabeornis castaneoventris egg
Egg of Chestnut Rail, Eulabeornis castaneoventris, collected in Port Essington, Northern Territory, Australia

Megapodius reinwardt tumulus eggs
Eggs of the orange-footed scrubfowl, Megapodius reinwardt tumulus, collected by John MacGillivray in Port Essington, Northern Territory, November 1844 Date: 1844

Numida meleagris, Helmeted Guineafowl, female
Skin of guineafowl collected by 19th Century naturalist Emin Pasha in Tingasi, Equatorial Africa. 17/8/1883. Original NHM label: Numida ptilorhyncha 1887.9.28.28. Date: 1887

Motacilla flava, Western Yellow Wagtail, male
Skin of Western Yellow Wagtail collected by 19th Century naturalist Emin Pasha in Tingasi, Equatorial Africa. 02/10/1883. Original NHM label: Budytes flava 1887.9.28.156 Date: 1887

Hemibrycon taeniurus, Mountain spring sardine

Goliathus goliatus, goliath beetle
An x-ray image of the goliath beetle, Goliathus goliatus, showing shotgun wounds

Thomas Sopwith (1803-1879) & geological models
Thomas Sopwith (1803 - 1879) was an eminent geologist and civil engineer who pioneered methods of representing geological features

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

Sopwith Model VII: Surface denudation of veins
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

Sopwith Models: denudation & faulting
Models showing the effect of denudation and faulting on how rock strata appear at the surface. Thomas Sopwith (1803 - 1879)

Sopwith Model II: Coal strata near 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

Sopwith Model VII: Denudation of mineral veins
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

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

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

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

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

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

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

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

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

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

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

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

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

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

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