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The geology of the neighbourhoods of Flint, Mold, and Ruthin ...

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PREFACE.<br />

TnE first edition <strong>of</strong> <strong>the</strong> Quarter-sheet <strong>of</strong> <strong>the</strong> Maps <strong>of</strong> <strong>the</strong> Geo-<br />

logical Survey (79 S.E.) described in <strong>the</strong> present Memoir was<br />

published in 1850, <strong>and</strong> was revised up to 1855. <strong>The</strong> western<br />

portion was principally mapped by Mr. W. T. Aveline, <strong>the</strong> Coal-<br />

Measures by Mr. D. H. Williams, <strong>and</strong> <strong>the</strong> New Red S<strong>and</strong>stone<br />

by Pr<strong>of</strong>essor E. Hull, while <strong>the</strong> lodes were inserted by Sir W. W.<br />

Smyth. <strong>The</strong> materials for <strong>the</strong> present Memoir were collected<br />

during a re-survey by Messrs. 0. E. De Ranee <strong>and</strong> A. Strahan,<br />

made on <strong>the</strong> six-inch scale, when <strong>the</strong> boundaries <strong>of</strong> <strong>the</strong> Glacial<br />

<strong>and</strong> o<strong>the</strong>r superficial deposits were traced for <strong>the</strong> first time. <strong>The</strong><br />

eastern part <strong>of</strong> <strong>the</strong> Quarter-sheet, comprising <strong>the</strong> New Red S<strong>and</strong>-<br />

stone <strong>and</strong> <strong>the</strong> <strong>Flint</strong>shire Coal-field (exclusive <strong>of</strong> <strong>the</strong> Leeswood<br />

district), was re-surveyed by Mr. De Ranee, <strong>the</strong> remainder <strong>of</strong> <strong>the</strong><br />

map by Mr. Strahan. Quarter-sheet 79 S.E. (Old Series) covers<br />

nearly <strong>the</strong> same area as Sheet 108 (New Series). <strong>The</strong> limits <strong>of</strong><br />

<strong>the</strong> latter lie about half-a-mile fur<strong>the</strong>r south <strong>and</strong> fur<strong>the</strong>r west<br />

than those <strong>of</strong> <strong>the</strong> earlier map.<br />

<strong>The</strong> area represented includes portions <strong>of</strong> <strong>the</strong> Vale <strong>of</strong> Clwyd,<br />

<strong>the</strong> Estuary <strong>of</strong> <strong>the</strong> Dee, <strong>and</strong> <strong>the</strong> intervening high ground composed<br />

<strong>of</strong> Silurian <strong>and</strong> Lower Carboniferous Rocks.<br />

Considerable changes have been made in <strong>the</strong> mapping <strong>of</strong> <strong>the</strong><br />

Vale <strong>of</strong> Clwyd. <strong>The</strong> Trias, formerly believed to overlap <strong>the</strong> Car-<br />

boniferous rocks, <strong>and</strong> to pass on to <strong>the</strong> Wenlock Shale, is now<br />

shown to be affected by a great fault, which throws down both<br />

Carboniferous <strong>and</strong> Triassic strata along <strong>the</strong> western flanks <strong>of</strong> <strong>the</strong><br />

Silurian range. To this dislocation <strong>the</strong> existence <strong>of</strong> <strong>the</strong> outlier<br />

<strong>of</strong> newer rocks in <strong>the</strong> Silurian area <strong>of</strong> North Wales is mainly<br />

due—a structure that forms a striking analogy to that <strong>of</strong> <strong>the</strong><br />

U 60799. 500.—9/90. Wt. 15530. B. & S. a 2

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