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The universal geography : earth and its inhabitants

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14 THE BRITISH ISLES.<br />

Farther west still, amongst the many bays which indent the coasts of Devon<br />

<strong>and</strong> Cornwall, the foremost place belongs to Plymouth Sound, which ranks with<br />

Chatham <strong>and</strong> Portsmouth as a great naval station.<br />

If we now turn to a consideration of the principal features of Irel<strong>and</strong>, we<br />

shall find that they differ essentially from those presented by the more favoured<br />

sister isl<strong>and</strong>. Less varied in <strong>its</strong> contour, it exhib<strong>its</strong> likewise greater simplicity in<br />

Fig. 8.—PLYMorTH Sound <strong>and</strong> the Hamoaze.<br />

From an Admiralty Chart. Scale 1 : 150,000.<br />

iKettk^ -^<br />

Si y .' .. A ~-.- •-.^-'' '"v<br />

'y / ^<br />

<strong>its</strong> geological structure. Broadly speaking, it may be described as consisting of a<br />

great central plain of carboniferous limestone, stretching across from sea to sea,<br />

<strong>and</strong> bounded in nearly aU directions by mountain masses composed of the most ancient<br />

geological formations.* <strong>The</strong> highl<strong>and</strong>s of the north-east, north-west, <strong>and</strong> west<br />

consist of the same crystalline <strong>and</strong> Silurian rocks which are so extensively developed<br />

in Scotl<strong>and</strong>. <strong>The</strong> south-eastern highl<strong>and</strong>s likewise consist of Silurian strata pene-<br />

trated by granite, <strong>and</strong> overlying Cambrian rocks, thus repeating the features which<br />

• E. Hull, "<strong>The</strong> Physical Geology aud Geography of Irel<strong>and</strong>."

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