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Sopwith Model XII: Denudation of mineral veinsThis 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 veinsThis 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 VII: Denudation of mineral veinsThis 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 veinsThis 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 veinsThis 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 denudationThis 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 denudationThis 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