Walker - 1967 - A geography of Italy
Walker - 1967 - A geography of Italy
Walker - 1967 - A geography of Italy
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PART III: REGIONAL GEOGRAPHY<br />
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controlled from above and do not help sufficiently in remedying the lack <strong>of</strong><br />
working capital; that poderi o f 15 ha (still less quote o f 3) can no longer be considered<br />
viable units and that to create more peasant family farms is to imderpm<br />
an inefficient system incapable o f surviving the economic climate <strong>of</strong> the Common<br />
Market; that the schemes were aimed too much at providing work and too little at<br />
encouraging efficient production; that in the context o f a rapidly expanding<br />
industrial country such peasant settlement schemes were irrelevant. No doubt<br />
there is much substance in these strictures, in particular as regards the size <strong>of</strong><br />
holdings, but the shortcomings o f the reform must be seen against the strong<br />
political and social pressures o f the late 1940s. As far as the Maremma was concerned<br />
the maintenance o f the status quo was indefensible. In fact, thanks very<br />
largely to the skill and experience o f the Tuscan peasant, the Ente Maremma can<br />
claim a substantial measure o f success.<br />
Tuscany, like Sardinia, possesses a rich variety o f minerals but for the most<br />
part the deposits are small and scattered. The mining o f lignite, some o f which is<br />
used in thermal electric plants, is significant in view o f the poverty o f the area in<br />
other forms o f energy. The better-quality lignites are found in the Miocene<br />
sediments o f Grosseto province but the vast majority o f the production (roughly<br />
half o f <strong>Italy</strong>’s 1,000,000 tons) is now o f inferior fuel extracted from the Pliocene<br />
and Pleistocene lacustrine deposits o f the upper Arno and Siena districts. The<br />
iron ore o f eastern Elba (haematite, magnetite and limonite), mined since<br />
Etruscan times, is smelted with imported coal at Piombino; the furnaces <strong>of</strong><br />
Port<strong>of</strong>erraio, damaged during the war, have not been rebuilt. Salt, borax and<br />
gypsum in the Cecina valley and pyrites from Gavorrano and Rovi provide the<br />
raw materials for a number o f small chemical plants. In the M . Amiata area<br />
antimony and mercury are mined; the latter have become relatively more important<br />
since the loss o f the Idria mines to Yugoslavia in 1946. Other minerals<br />
represented are ferro-manganese in M. Argentario and silver-lead and copper at<br />
Massa Marittima. The architecture o f Tuscany is enriched by a variety <strong>of</strong><br />
building stones, among them the marbles o f Montagnola and the Apuan Alps.<br />
The economy <strong>of</strong> Tuscany is still heavily inclined towards agriculture, and its<br />
industries, based for the most part on the processing o f agricultural products and<br />
minerals, are mainly organized in small units; the steel works <strong>of</strong> Piombino, the<br />
shipyards o f Leghorn and the motor-cycle plant at Pontedera are exceptional.<br />
Yet despite this agricultural bias and the poor showing o f industry, traits common<br />
to most o f the Centre and South, Tuscany’s demographic evolution seems<br />
to be more in step with that o f the North. With some local exceptions the pressure<br />
o f population on the agricultural resources has been less severe than in most <strong>of</strong><br />
peninsular <strong>Italy</strong>, and although emigration never reached proportions experienced<br />
in many other areas (Veneto, Calabria) the population rose only 23% to its<br />
present 3,291,000 between 1911 and 1961 - much less than the national average.<br />
In fact, only Liguria, Piedmont and Friuli-Venezia Giulia have lower birth rates<br />
than Tuscany ( i 3 '4 %o). The population density varies widely from over 240 per<br />
170