Alban Hills

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The Alban Hills.
The Alban Hills.

The Alban Hills (Italian Colli Albani) are the site of a quiescent volcanic complex in Italy, located 20 km southeast of Rome and about 24 km north of Anzio.

The dominant peak is the Monte Cavo, at 950 m (3,115 ft, 41.76° N 12.73° E). There are two small calderas which contain lakes, Lago Albano (41.712° N 12.703° E) and Lake Nemi (41.747° N 12.668° E). The rock of the hills is called Peperino (lapis albanus) a particular Tuff, a combination of ash and small rocks that is useful for construction, and provides a mineral-rich substrate for grape vines.

The ancient Romans called them Albanus Mons. On the summit was the sanctuary of Jupiter Latiaris, in which the consuls celebrated the Feriae Latinae, and several generals celebrated victories here when they were not accorded regular triumphs in Rome. The temple has not survived, but the Via Triumphalis leading up to it may still be seen.

The hills, especially around the shores of the lakes, have been popular since prehistoric times, from the IX to VII century BC there were numerous villages (see the legendary Alba Longa and Tusculum).

In Roman times these villages were inhabited as a way to escape the heat and crowds of Rome, and there are many villas and country houses to be seen.

Travelers of the past from all periods and nations, without guides, learned alone to look at and love this land. It was the Pope Piccolomini, (Pope Pius II), one of the most illustrious personages of the Renaissance who rediscovered these hills in his "Commentaries" in which facts, emotions and historical records are described, redirects the attention of tourists, the fascination of an incomparable landscape, rich with hills, high plains, lakes, woods, gardens, villas and panoramas. On the slopes of Alban Hills, centre of the "Vetus Latium", one can understand better the synthesis of Rome, it soul and the reasons for its "grandeur".

The towns and villages present today on Alban Hills area known as the Castelli Romani:

Volcanic lakes view from Monte Cavo.
Volcanic lakes view from Monte Cavo.

Writers and artists who have produced work about this area include:

Examination of deposits have dated the two most recent eruptions to around 37,000 and 41,000 years ago.[1] The area exhibits small localised earthquake swarms, bradyseism, and release of carbon dioxide and hydrogen sulphide into the atmosphere. The uplift and earthquake swarms have been interpreted as caused by a slowly growing spherical magma chamber 5-6 kilometres below the surface; some think that it may erupt again;[2] if so, there is risk to Rome, which is only 25 to 30 km away.

There is documentary evidence of an eruption in 114 BC, but the absence of holocene geological deposits has largely discredited it as a volcanic event[3] and instead the account is considered to be a description of a forest fire.

The volcano emits large amounts of carbon dioxide. This can potentially reach lethal concentrations if it accumulates in depressions in the ground in the absence of wind. The asphyxiation of 29 cows in September 1999 prompted a detailed survey, which found that concentration of the gas at 1.5 m above the ground in a residential area on the northwestern flank sometimes exceeded the occupational health threshold of 0.5%.[4] Eight sheep were killed in a similar incident in October 2001.[5]

  1. ^ http://www.ingv.it/~roma/profilo/fondazione/sezioni/romauno/webuf2/marra/table1.html
  2. ^ http://boris.vulcanoetna.com/ALBANI.html
  3. ^ http://boris.vulcanoetna.com/ALBANI.html
  4. ^ http://www.esc.cam.ac.uk/ivhhn/guidelines/gas/co2.html
  5. ^ http://www.ipcc.ch/activity/srccs/SRCCS_Chapter5.pdf

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