E;*+ - Geological Curators

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Model No. Equivalent Model No. in 1841 Set Description 1 Horizontal valley of denudation in horizontal strata. Horizontal hill of denudation in horizontal strata. Inclined valley of denudation in horizontal strata. Inclined hill of denudation in horizontal strata. Coal strata near Newcastle-on-Tyne Modelled topography in horizontal strata. Dislocation of strata in Carboniferous rocks. Erosion surface, with parallel contours, in horizontal strata. Repeated normal fault offset of horizontal strata; plane surface topography. Repeated normal fault offset of nearly horizontal strata; with full topographic expression. Crossing normal faults in horizontal strata, with surface expression of one horizontal coal seam. Repeated n oml fault offset, with trough faulting, in horizontal strata, with full topographic expression. Crossing normal faults in horizontal strata, with full topographic expression. Valley in horizontal strata (topography more pronounced than in Model Ia). Vertical intersection of mineral veins; plane surface topography. Denudation of mineral veins; full topographic expression. Vertical strata crossing a valley; full topographic expression. Strata inclined upstream in a valley; denuded basset of inclined strata. Strata inclined downstream steeper than valley slope; undercutting of strata. 16 Inclined strata in plane surface topography. 17 Vertical strata in plane suiface topography. Table 3 Comparison of the models shown on the working drawings with the twelve models published in 1841.
Fig. 1 Lithograph of Model V, Dislocations of Coal Strata, from Sopwi th' S description of the models (1841). Above: elevation of one vertical face of the model; the pecked line inclined left to right is the oblique cut line. Below: the outcrop of faulted strata on the inclined cut across the model.
Page 1: E;*+ 'C.. THE WORST CURATED CEZ)&WI
Page 4 and 5: Technical: The Burnt Dope Technique
Page 6 and 7: Although an informative biography o
Page 8 and 9: COLLECTIONS AND COLLECTORS OF NOTE
Page 10 and 11: 1. Nov. 8 1802 Mar. 26 1804 April 2
Page 12 and 13: for the engineer in such a way that
Page 14 and 15: edge of the model being north, we h
Page 16 and 17: It is evident that three-inch lengt
Page 18 and 19: Model 5 - This is the inverted offc
Page 20 and 21: Sopwith, T. 1829. Geological sectio
Page 22 and 23: Forsterls 1821 Section of the Strat
Page 27: Fig. 2 A four-inch version of Model
Page 33: COLOUR ROCK TYPE LOCAL ROCK NAME SY
Page 37: Fig. 5b The reverse side of the ori
Page 41 and 42: A COLLECTIONS RESEARCH UNIT FOR THE
Page 43 and 44: i i cH.ARAmm SEl' GENEEW GUIDE LINE
Page 46 and 47: THE HUNTERIAN. Presentation at the
Page 49 and 50: GCG Newsletter Vol. 2 no. 7 WHERE I
Page 51 and 52: 5 COLLECTlONS AND INFORMATION LOST
Page 53 and 54: may shed further light on the myste
Page 55 and 56: 7 0 @ COLLECTIONS AND INFORMATION F
Page 57 and 58: i --- A member of this Socicv who ;
Page 59 and 60: L 95. HUDLESTON, Wilfrid Hudleston
Page 61 and 62: Northumberland and Durham - P. S. D
Page 63 and 64: -. THE BURNT DOPE TECHNIQUE AND OTH
Page 65 and 66: COMPUTER CONTROLLED DATA BANK SYSTE
Page 68 and 69: LAPMASTER 15 is a new addition to t
Page 70 and 71: 3) are up to 60 or 70 children on e
Page 72 and 73: its highly fossiliferous nature and
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NOTICES Building and Ornamental Sto
Page 76 and 77:
PARK, A. 1979. The Geology of Lanca
Page 78 and 79:
Automated Thin Sectioning Systems I
Page 80:
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E;*+ - Geological Curators

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