Faulting Collection

Millook Haven, Poundstock, Cornwall. 1905
A view of the beach at Millook Haven showing the contorted strata in the cliffs. There is a man standing in the left foreground

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 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 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

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In the quaint coastal village of Millook Haven, Poundstock, Cornwall, back in 1905, a groundbreaking study on faulting was conducted. Led by the renowned geologist Thomas Sopwith and his team of experts, they embarked on an expedition that would shed light on the intricate workings of our planet's geological formations. Using various models developed by Sopwith himself, such as the Sopwith Model XII which focused on denudation of mineral veins and the Sopwith Model VII which explored surface denudation of veins, they delved deep into understanding faulting processes. These models proved to be invaluable tools in unraveling nature's secrets. One particular model that caught their attention was the Sopwith Model II. It revealed fascinating insights into coal strata near Newcastle and showcased how faulting played a significant role in shaping these deposits over time. The team marveled at how intersecting mineral veins were formed as depicted by the Sopwith Model VI and further studied vertical intersecting veins using the precise measurements provided by the Sopwith Model XI. As their research progressed, they discovered that faulting not only caused denudation but also led to dislocations within coal strata as demonstrated by both the Sopwith Models V and IV respectively. This realization challenged previously held beliefs about fallacious coal indications prevalent during that era. The findings from this comprehensive study emphasized how crucial it is to comprehend faulting mechanisms for accurate geological interpretations. By meticulously examining surface denudation through detailed observations with instruments like those used in the Sopwith Models VII and XII, researchers gained valuable knowledge about mineral vein denudation. This captivating journey through time showcases how dedicated scientists like Thomas Sopwith paved new paths in understanding Earth's dynamic processes. Their meticulous exploration forever changed our perception phenomena while leaving an indelible mark on scientific history.