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Nineteenth Century Collection (page 8)

Background imageNineteenth Century Collection: Northern cassowary by JG Keulemans

Northern cassowary by JG Keulemans
Hand-coloured lithograph of cassowary head by JG Keulemans (c. 1898), based on the live animals at Walter Rothschilds Museum at Tring

Background imageNineteenth Century Collection: Alfred Newton

Alfred Newton (1829-1907), Professor of Comparative Anatomy at Cambridge University in the late 19th Century. Newton was an expert ornithologist and tutored Walter Rothschild in anatomy

Background imageNineteenth Century Collection: Geologists of the 1860 s

Geologists of the 1860 s
c.1860 s. From collection of manuscript material by Benjamin Waterhouse Hawkins, donated by his granddaughter Mary Hawkins Date: circa 1860

Background imageNineteenth Century Collection: Pitta Iris, from the Gould Collection

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

Background imageNineteenth Century Collection: Rallus phippensis

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

Background imageNineteenth Century Collection: Cacatua sanguinea, from the Gould Collection

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

Background imageNineteenth Century Collection: Conopophila albogularis egg, Gould Collection

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

Background imageNineteenth Century Collection: Turnix castanota egg, from Gould Collection

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

Background imageNineteenth Century Collection: Oriolus sagittatus affinis eggs

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

Background imageNineteenth Century Collection: Dendrocygna arcuata australia eggs

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

Background imageNineteenth Century Collection: Megapodius reinwardt tumulus eggs

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

Background imageNineteenth Century Collection: Plate 134 from the John Reeves Collection

Plate 134 from the John Reeves Collection
John Reeves, a 19th Century Tea Inspector, travelled to Canton, China in order to develop a large collection of Chinese natural history drawings

Background imageNineteenth Century Collection: Numida meleagris, Helmeted Guineafowl, female

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

Background imageNineteenth Century Collection: Musophaga rossae, Rosss turaco, female

Musophaga rossae, Rosss turaco, female
Skin of turaco collected by 19th Century naturalist Emin Pasha in Tingasi, Equatorial Africa. 10/08/1883. Original NHM label: Musophaga rossae 1887.9.28.45 Date: 1887

Background imageNineteenth Century Collection: Motacilla flava, Western Yellow Wagtail, male

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

Background imageNineteenth Century Collection: Thomas Sopwith (1803-1879) & geological models

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

Background imageNineteenth Century Collection: Sopwith Model XII: Denudation of mineral veins

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

Background imageNineteenth Century Collection: Sopwith Model VII: Surface denudation of veins

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

Background imageNineteenth Century Collection: Sopwith Models: denudation & faulting

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

Background imageNineteenth Century Collection: Sopwith Model II: Coal strata near Newcastle

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

Background imageNineteenth Century Collection: Sopwith Model VII: Denudation of mineral veins

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

Background imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century 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 imageNineteenth Century Collection: Launton Meteorite

Launton Meteorite
The Launton meteorite fell on 15 February 1830 at approximately 7.30pm, Launton village in Oxfordshire. The meteorite is of the most common type of stony meteorite, known as an ordinary chondrite



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