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

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<strong>The</strong> Glacial Deposits include two drifts <strong>of</strong> distinct origin, viz.,<br />

that which travelled from <strong>the</strong> north over Lancashire <strong>and</strong> Cheshire,<br />

<strong>and</strong> that which came from Welsh sources in <strong>the</strong> south-west. <strong>The</strong><br />

two meet along a line which partly follows <strong>the</strong> Welsh border,<br />

but runs across <strong>the</strong> gentler hills <strong>of</strong> <strong>the</strong> <strong>Flint</strong>shire Coal-field.<br />

Several examples <strong>of</strong> striated rock-surfaces have been recorded, in<br />

all <strong>of</strong> which <strong>the</strong> striae point in <strong>the</strong> direction in which <strong>the</strong> Drift<br />

associated with <strong>the</strong>m has travelled. Vast numbers <strong>of</strong> boulders<br />

also have been brought from <strong>the</strong> Snowdon <strong>and</strong> Arenig ranges<br />

<strong>and</strong> dropped upon <strong>the</strong> western flanks <strong>and</strong> <strong>the</strong> tops <strong>of</strong> <strong>the</strong> Silurian<br />

<strong>and</strong> Carboniferous ranges. One <strong>of</strong> <strong>the</strong> largest <strong>of</strong> <strong>the</strong>se erratics is<br />

24 feet long, <strong>and</strong> its visible portion can scarcely fall short <strong>of</strong><br />

300 tons in weight. <strong>The</strong> fact that <strong>the</strong> Drift was borne across<br />

<strong>the</strong> outcrops <strong>of</strong> <strong>the</strong> various rocks, <strong>and</strong> nearly at right angles<br />

to <strong>the</strong>m, has led to even more variability in <strong>the</strong> nature <strong>of</strong> <strong>the</strong><br />

deposit than is usually observed.<br />

<strong>The</strong> history <strong>of</strong> <strong>the</strong> River Dee is given in some detail, <strong>and</strong> <strong>the</strong><br />

valley <strong>of</strong> this river is shown to coincide with a pre-Glacial estuary<br />

(or depression), filled with Glacial Drift. <strong>The</strong> upper part <strong>of</strong> <strong>the</strong><br />

river, however, follows a post-Glacial course through Holt,<br />

Eccleston, <strong>and</strong> Chester, <strong>the</strong> pre-Glacial valley, now completely<br />

choked with Drift, running past Dodleston <strong>and</strong> Rossett.<br />

Chapter XIII. is devoted to a detailed account <strong>of</strong> <strong>the</strong> lead-<br />

mines. <strong>The</strong> veins are separable into two sets <strong>of</strong> different direction,<br />

contents, <strong>and</strong> age. <strong>The</strong> principal lead-bearing zones in <strong>the</strong> Lower<br />

Carboniferous Rocks, <strong>and</strong> <strong>the</strong> various forms <strong>of</strong> " vein," " pipe," or<br />

" flat," in which <strong>the</strong> ore occurs, are indicated.<br />

<strong>The</strong> present Memoir has been edited <strong>and</strong> mainly written by<br />

Mr. Strahan. Mr. De Ranee's contributions are as follows :<br />

An account <strong>of</strong> <strong>the</strong> Lower Coal-Measures <strong>of</strong> Northop <strong>and</strong> Hawar-<br />

den, on pp. 66, 67, 71 ; Chapter VII., pp. 72-99, on <strong>the</strong> Middle<br />

Coal-Measures ; <strong>and</strong> notes on <strong>the</strong> Drift <strong>of</strong> his area, on pp. 132,<br />

133,. 135, 139-144. Several also <strong>of</strong> <strong>the</strong> Colliery Sections, given<br />

in Appendix L, were collected by him.<br />

<strong>The</strong> determination <strong>of</strong> <strong>the</strong> fossils collected during <strong>the</strong> re-survey<br />

was commenced by Mr. R. E<strong>the</strong>ridge, but completed by<br />

Messrs. Sharman <strong>and</strong> Newton, who are responsible also for <strong>the</strong><br />

correction <strong>of</strong> <strong>the</strong> synonymy. <strong>The</strong> lists were submitted to Mr.<br />

G. H. Morton also, who kindly noted some additions.<br />

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