Caption
This
zoom-panorama is centered in Civita di Bagnoregio, a small hilltown in upper Latium , essentially medieval, rises in a landscape formed of volcanic tuff and badlands (clays).
It is reachable by walking across a long pedestrian bridge over the badlands. Due to the isolation the city preserves its original medieval character.
Its debris are in the continuous process of transportation along the two main rivers down to the Tirrenian sea.
That soil-transportation, forms a continuous white belts
(visible on the right side of the panorama), similar to large areas of New Mexico.
A large block of tuff is hanging down its side with a visible black vertical fracture on the far left part of the village (look for the
descriptive hotspot in the interactive picture).
Note:
This interactive picture has a total of 5
hotspot:
4 clickable
hotspot and 1 non-clickable
descriptive hotspot.
Scientific digression:
In these areas where drainage density is high, surface erosion processes predominate where clays are present. A cap of consistent volcanic products preserve the site where the village is settled. In some places the volcanic cliff hill is mined to the base from the continuous erosion of small rivers and from the action of rains and the wind.
The erosion and soil transportation is supposed to be in about 7 cm per year.