1,721,019 research outputs found
I travertini di Carvanno (Brescia). The travertine of Carvanno (Brescia).
The travertine of Carvanno (Brescia) - The lithofacies of travertine of the Carvanno area are
described in detail. These deposits form the core of «Morphological Units» located at different altitudes and
formed in different times during the Pleistocene. The deposition of the travertine is probably, from the evidence
of morphological and morphostructural analyses, connected with the circulation of thermomineral waters
rising through tectonic contacts on the right of the Degagna Valley. Their subsequent levelling to terraces
is due to variations in the base level of the rivers, connected with tectonic movements
Nuovi affioramenti oligocenici nella zona del Monte S. Bartolomeo di Salò e loro implicazioni geologiche (Bresciano orientale)
Vengono descritti nuovi affioramenti di marne oligoceniche nei pressi del M. S. Bartolomeo di Saò (Lago di Garda, Brescia
Note illustrative della Carta geologica delle Prealpi bresciane tra la V. Vrenda e il M. Pizzocolo. Explanation notes of the geological map of the Brescian Prealps between Val Vrenda and M. Pizzocolo.
The geological map of the V. Vrenda-M. Pizzocolo
area (1:25.000) is the partial result of studies carried out
for several years and that are still in progress in the
Brescian Prealps.
The explanatory text briefly describes the different
rock formations as well as Quaternary informal units
and it is completed by a long bibliographical list which
can supply further information to enhance the geological
knowledge and the regional description of this area.
Several variations have modified the previous cartography
and the new data introduce elements to reinterpret
the paleogeographic evolution of the area.
New data allows an updating of the tectonic evolution
of the Prealps; the Quaternary deposits have been distinguished
into several informal stratigraphic units. Geomorphological
symbols complete the map: karst features,
fluvial erosional cliffs, moraine ridges and other
glacial and fluvioglacial features have been mapped, as
well as gravel and limestone quarries
Stratigrafia di un frammento di margine continentale giurassico: la successione di Case Caldarola (Appennino piacentino).
Carta geologica delle Prealpi bresciane tra la V. Vrenda e il M. Pizzocolo. Geological map of the Brescian Prealps between the Vrenda Valley and Mt. Pizzocolo.
Geological map of the Brescian Prealps between the Vrenda Valley and Mt. Pizzocolo. Scale: 1: 25.000. With illustrative notes at http://manhattan.unipv.it/Atti_tic/volume38.htm
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