There are several monuments, and among them one to Mr. William Phillipps, probably father of the gentleman who removed to Camelford as an attorney, and grandfather to the three brothers mentioned above. He is stated to have been of Treveans, and to have died on the 12th of April 1712, in the 62d year of his age. The turnpike road leading from St. Columb by Wade Bridge and Camelford to Launceston, nearly surrounds this Church. It was for some years the great line of communication to the west of Cornwall, till in 1767 a commencement was made on a more direct line over Tregoss Moors on one side of Bodmin, and Temple Moors on the other. This road so entirely superseded the former as to cause an entire loss of capital to those who contributed towards making it; and the road itself fell back into a state of repair inferior to that of most parish roads. It has, however, recently been taken up as a new concern, and in 1835 a stage coach has been established on it. The Editor has heard from the Rev. William Phillipps, who died in 1794, that the making of this road was taken up as a matter of patriotism; and that to assist the undertaking, he cut with his own hands the figures on the granite mile stones, which still remain. The entry of this parish, in the Taxation of Pope Nicholas, is thus: “Sech (and in a note, Eccƚia S[~c]e Thete) taxat’ ut sequitur. £. _s._ _d._ Prebend’ Mag’ri Osbt^i 4 10 0 Prebend’ Mag’ri W. de Wymondeston 4 10 0 Vicar’ ejusdem 1 0 0” St. Teath measures 4,721 statute acres. Annual value of the Real Property as £. _s._ _d._ returned to Parliament in 1815 5,041 0 0 Poor Rate in 1831 800 2 0 Population,――{ in 1801, | in 1811, | in 1821, | in 1831, { 911 | 857 | 990 | 1280 giving an increase of 40½ per cent. in 30 years. It is not improbable but that the 8 printed in the place of hundred, under the return of 1811, should have been a 9. Present Vicar, the Rev. Joseph Fayrer, collated by the Bishop of Exeter in 1830. GEOLOGY, BY DOCTOR BOASE. This parish is situated on rocks belonging to the calcareous series. On the eastern boundary, however, near the church, the slate is nearly connected with the porphyritic series; here at Treburget is a lead mine in a blue pyrituous slate; the lodes run north-east and south-west, varying from two feet to five feet in thickness. The matrix of the ores consists of angular pieces of slate like fragments cemented by quartz, in which galena, blend, iron pyrites, and spathous iron occur.