Alban Hills

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The Alban Hills (Template:Langx) are the caldera remains of a quiescent volcanic complex in Italy, located Template:Convert southeast of Rome and about Template:Convert north of Anzio. The Template:Cvt high Monte Cavo forms a highly visible peak in the centre of the caldera, but the highest point is Maschio delle Faete approximately Template:Cvt to the east of Cavo and Template:Cvt taller. There are subsidiary calderas along the rim of the Alban Hills that contain the lakes Albano and Nemi. The hills are composed of peperino (lapis albanus), a variety of tuff that is useful for construction and provides a mineral-rich substrate for nearby vineyards.

History

The hills, especially around the shores of the lakes, have been popular since prehistoric times. From the 9th to 7th century BC, there were numerous villages (such as the legendary Alba Longa and Tusculum). The area was inhabited by the Latini during the 5th to 3rd centuries BC.

The ancient Romans called Monte Cavo 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 during times when they were not accorded regular triumphs in Rome. The foundations and some of the architectural fragments of the temple were still in existence until 1777, when they were used to build the Passionist monastery by Cardinal York,<ref>{{#if: |

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In Roman times, the area was often used by the rich as a way to escape the heat and crowds of Rome, as it is today as shown by the many villas and country houses present.

Towns and cities

Template:Main The towns and villages in the Alban Hills are known as the Castelli Romani.

Volcanic activity

Aerial view showing the main caldera and several secondary ones around the rim
Topographic map of the Alban Hills showing the caldera rims

Examination of deposits have dated the four most recent eruptions to two temporal peaks, around 36,000 and 39,000 years ago.<ref name=Carmela2006/><ref>Template:Cite journal</ref> The area exhibits small localised earthquake swarms, bradyseism, and release of carbon dioxide and hydrogen sulfide 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;<ref name="Behncke">Template:Cite web</ref> some think that it may erupt again; if so, there is risk to Rome, which is only 25 to 30 km away.<ref>Template:Cite journal</ref><ref>Template:Cite book</ref>

Plutarch reports that in 406Template:NbspBC, Lake Albano surged over the surrounding hills, despite there being no rain nor tributaries flowing into the lake to account for the rise in water level.<ref>Template:Citation</ref> The ensuing flood destroyed fields and vineyards before eventually pouring into the sea. It is thought to have been a limnic eruption caused by volcanic gases, trapped in sediment at the bottom of the lake and gradually building up until suddenly releasing, causing the water to overflow.<ref>Template:Citation</ref>

There is documentary evidence which may describe an eruption in 114 BC, but the absence of Holocene geological deposits has largely discredited it as a volcanic event and instead the account is considered to be a description of a forest fire.<ref name="Behncke" />

The volcano emits large amounts of carbon dioxide<ref>Template:Cite journal</ref> which 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%.<ref>Template:Cite web</ref> Eight sheep were killed in a similar incident in October 2001.<ref>Template:Cite book citing Template:Cite journal</ref>

People

Louis Gurlitt, Alban Hills (1850)

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

Panorama

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See also

References

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