Thomas Ashby and Philip Lake

Biographical details

Thomas Ashby and Philip Lake 1911 Encyclopædia Britannica, Volume 2… (1911)

The Tanaro (Tanarus) , though largely fed by tributaries from the Ligurian Apennines, itself rises in the Maritime Alps, while the rivers on the south and south-west of the range are short and unimportant. The south side of the range rises steeply from the sea, leaving practically no coast strip: its slopes are sheltered and therefore fertile and highly cultivated, and the coast towns are favourite winter resorts (see Riviera) .
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Thomas Ashby and Philip Lake 1911 Encyclopædia Britannica, Volume 2… (1911)

Snow lies on the highest peaks of the Apennines for almost the whole year. The range produces no minerals, but there are a considerable number of good mineral springs, some of which are thermal (such as Bagni di Lucca, Monte Catini, Monsummano, Porretta, Telese, &c.) , while others are cool (such as Nocera, Sangemini, Cinciano, &c.) , the water of which is both drunk on the spot and sold as table water elsewhere. (T. As.)
Geology.—The Apennines are the continuation of the Alpine chain, but the individual zones of the Alps cannot be traced into the Apennines.
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Thomas Ashby and Philip Lake 1911 Encyclopædia Britannica, Volume 2… (1911)

The inner zone of crystalline and schistose rocks which forms the main chain of the Alps, is absent in the Apennines except towards the southern end. The Apennines, indeed, consist almost entirely of Mesozoic and Tertiary beds, like the outer zones of the Alps. Remnants of a former inner zone of more ancient rocks may be seen in the Apuan Alps, in the islands off the Tuscan coast; in the Catena Metallifera, Cape Circeo and the island of Zannone, as well as in the Calabrian peninsula.
Source: Wikisource

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