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Faulted Collection

"Nature's Artistry: Witness the Majestic Waterfall Flowing Over Faulted Edge of Sandstone" Discover the breathtaking beauty of Sgwd Henrhyd (Henrhyd Falls) in Nant Llech

Background imageFaulted Collection: Waterfall flowing over faulted edge of sandstone, Sgwd Henrhyd (Henrhyd Falls), Nant Llech

Waterfall flowing over faulted edge of sandstone, Sgwd Henrhyd (Henrhyd Falls), Nant Llech, Brecon Beacons N. P. Powys
Waterfall flowing over faulted edge of sandstone, Sgwd Henrhyd (Henrhyd Falls), Nant Llech, Brecon Beacons N.P. Powys, Wales

Background imageFaulted Collection: Faulted Yellow Sands, Colin Glen

Faulted Yellow Sands, Colin Glen - a view of a waterfall with a light tone visible to the base and sides, in the rocks. (Location: Northern Ireland: County Antrim: Belfast). Date: circa early 1900s

Background imageFaulted 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 imageFaulted 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 imageFaulted 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 imageFaulted 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 imageFaulted 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 imageFaulted 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 imageFaulted 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 imageFaulted 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 imageFaulted 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 imageFaulted 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 imageFaulted 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 imageFaulted Collection: Valley of Fire, Nevada, USA

Valley of Fire, Nevada, USA
Valley of Fire state park Nevada USA

Background imageFaulted Collection: Quartz vein in granite

Quartz vein in granite. Close-up of a quartz vein (white) running through a granite rock face with multiple faults (cracks)


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"Nature's Artistry: Witness the Majestic Waterfall Flowing Over Faulted Edge of Sandstone" Discover the breathtaking beauty of Sgwd Henrhyd (Henrhyd Falls) in Nant Llech, Brecon Beacons National Park, Powys. This captivating waterfall cascades gracefully over a faulted edge of sandstone, creating a mesmerizing spectacle that will leave you in awe. Unearth the geological wonders at Colin Glen where Faulted Yellow Sands reveal themselves. These unique formations showcase nature's handiwork, as layers of sand have been disrupted and shifted over time, resulting in an intriguing landscape. Delve into the world of mineral veins with Sopwith Model XII: Denudation. This intricate model showcases how natural forces have eroded and exposed these valuable mineral deposits through a process known as denudation. Explore further with Sopwith Model VII: Surface Denudation of Veins, which unravels the fascinating story behind how surface erosion has shaped and revealed hidden mineral veins over vast expanses of land. Witness coal strata near Newcastle come to life in Sopwith Model II. Marvel at how these ancient layers have been faulted and displaced by geological forces throughout history, leaving behind a striking visual representation for all to see. Immerse yourself in intersecting mineral veins depicted by Sopwith Model VI. Observe how different vein systems intertwine beneath the Earth's surface, forming complex patterns that captivate both scientists and enthusiasts alike. Journey deeper into underground mysteries with Sopwith Model XI: Vertical Intersecting Veins. Uncover the secrets held within vertical intersections as they create intricate networks deep below our feet – a testament to nature's remarkable complexity. Experience firsthand the effects of denudation on mineral veins through Sopwith Model XII: Mineral Vein Denudation. Witness how relentless erosive processes gradually expose these valuable resources, shaping the landscape as they go.