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Home > Images Dated > 2014 > January > 14 Jan 2014

Images Dated 14th January 2014

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32 Items

Background imageImages Dated 14th January 2014: 13887755

13887755

Background imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 13869590

13869590

Background imageImages Dated 14th January 2014: 13869670

13869670

Background imageImages Dated 14th January 2014: 13884391

13884391

Background imageImages Dated 14th January 2014: 13869585

13869585

Background imageImages Dated 14th January 2014: 13849145

13849145

Background imageImages Dated 14th January 2014: 13830057

13830057

Background imageImages Dated 14th January 2014: 13829979

13829979

Background imageImages Dated 14th January 2014: 13829971

13829971

Background imageImages Dated 14th January 2014: 13829887

13829887

Background imageImages Dated 14th January 2014: 13829895

13829895

Background imageImages Dated 14th January 2014: 13834447

13834447

Background imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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 imageImages Dated 14th January 2014: 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


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