Page:Great Neapolitan Earthquake of 1857 Vol 2.djvu/459

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INDEX.

ancient towns in, i. 28, 29; provincial towns in, i. 30, 31.

Itry, position of, ii. 153.

Jamaica shock, ii. 364.
Joints, fractures usually follow, i. 44.

Killed and wounded, return of, in commumes of the province of Basilicata, ii. 162.

La Cava, traces of the earthquake at, i. 231.
Laderana, entrance of the valley of the, i. 424; lignite beds of the, i. 431.
Lakes, temporary, explanation of formation of, ii. 371.
Lando and Tumo, valleys of the, ii. 36.
Landslip, great, and fissure in the piano of Mattine, near Viggiano, ii. 15.
Landslips, initial, all fissures are, ii. 363.
Landslips, great, ii. 366.
Lardner, Dr., account by, of the earthquake Dec. 16, i. 210.
La Sala, changed character of the limestone near, i. 333; road to, i. 334; extent of, i. 335; structures at, more or less fissured, but few actually demolished, i. 335; house of the Sotto Intendente, i. 330; pictures and pendule at Intendenzia, i. 338, 330; table and lamps of secretary to Sotto Intendente, i. 341, 342; church of, i. 343; fall of church tower, i. 344; church bells at, i. 345; angle of emergence inferred at, i. 346; wave-path perturbations at, i. 347; good observation of the sun at, ii. 32.
Laviano, grand scenery near, ii. 135; position of, ii. 136; Palazzo Carmine at, ii. 137; experience of occupiers of the palazzo, ii. 138; mysterious light heard of at, ii. 139; shock and sound at, ii. 139.
Level, changes of, accompanying earthquake, i. 217; any deductions from, whether of elevation or of depression, not to be depended upon, i. 219; permanent changes of, examination round the coast as to, i. 225; no evidences of; i. 227.

Lieti, Palazzo (Naples), fissures at, i. 207.
Limestone and clays, wave transits through, i. 385.
Limestone masonry, effects due to, i. 93.
Limestone, nummulitic and hippurite, i. 169.
Local effect, grand modifying conditions of; ii. 360.
Lupino, scarcely any damage done at, i. 249.
L, values of the coefficient, i. 149.

Magnetic declination at Auletta, observations to determine local, i. 259; declinations near Salvitello, ii. 34; relations, ii. 376.
Maldo, Valley of the, slipping rocks in the, ii. 134.
Mancini, Padre Vincenzio, information derived from, i. 274.
Maorno, Lago, a dreary pool, i. 406.
Maps, references to isoseismals on, ii. 253; good, necessity of, ii. 361.
Maps—Seeismic map A, with wave-paths and isoseismal curves.—Report to Royal Society of London: map B, showing the physical features of the Neapolitan earthquake of December 16, 1857.—Approximate comparison of seismal areas, map C.—Comparative map, D, of the seismic bands of the Mediterranean, vol. ii. 379. Earthquake of December 16, 1857: Map E.— No. 1. Diagram of observed maxima and minima wave emergences, and resulting depth of focus. No. 2. Diagram of mean wave emergences, and deduced mean focal depth, vol. ii. 248, 253.
Marine observatory, Naples, meteorological tables of the, ii. 166, 167.
Maris, sub-Appenine, i. 168.
Marsico Nuovo, situation of, ii. 29; original fissures in produced by the twisting movements, transferred quite round the walls, by transverse vibrations, i. 87.

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