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Adige River valley

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Journal Article
Published: 01 January 1963
Bulletin de la Société Géologique de France (1963) S7-V (5): 782–789.
...Jean Paul Rampnoux Abstract The NE-SW trending Stivo-Cornetto anticline (Trento province) forms a line of crests separating the Sarca valley from the Adige river valley. The entirely marine sequence includes Liassic and Dogger subreefal limestones succeeded by Malm, Cretaceous and lower Eocene deep...
Image
Representative diagram of the Zielbach-<span class="search-highlight">Adige</span> system evolution. (A) Immediat...
Published: 01 May 2014
Figure 10. Representative diagram of the Zielbach-Adige system evolution. (A) Immediately after the deglaciation of the main Venosta Valley, the Adige River deposits sediment in the whole valley width, partially following the early development of the Töllbach fan. (B) At ca. 12,000 yr B.P
Journal Article
Journal: GSA Bulletin
Published: 22 March 2018
GSA Bulletin (2018) 130 (9-10): 1457–1473.
... by up to two millennia. Debris-flow sediment supply from the Gadria-Strimm system drove the evolution of this valley segment between 12 and 6.25 k.y. B.P., first deflecting, then damming the course of the Adige River, forming a lake, and affecting the shape and size of the neighboring fans. Our data...
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Image
(A) Lateglacial to Holocene sediment yield (black line) associated with the...
Published: 22 March 2018
for evaluating Lateglacial to Holocene climatic fluctuations. Bø/Al—Bølling/Allerød; YD—Younger Dryas. (B) Longitudinal profile of the Adige River thalweg showing the location of the major paraglacial fans hosted in the valley (vertical exaggeration 4×). The profile crosses the top of each fan surface
Image
Sedimentation rates calculated for the <span class="search-highlight">Adige</span> <span class="search-highlight">River</span> (solid triangles) and fo...
Published: 01 May 2014
Figure 8. Sedimentation rates calculated for the Adige River (solid triangles) and for the Zielbach fan (dashed upsidedown triangles). In the figure are shown the regression lines used for the calculations of the deglaciation age in the main Venosta Valley (see text for details).
Series: Geological Society, London, Special Publications
Published: 01 January 2011
DOI: 10.1144/SP351.13
EISBN: 9781862395992
...Abstract Abstract Deep-seated gravitational slope deformations (DSGSDs) are fairly common phenomena in the Eastern Italian Alps. The Celentino DSGSDs (Trentino–Alto Adige Region, Peio Valley) extends over an area of approximately 5 km 2 between 2400 and 1050 m a.s.l. (metres above sea level...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2014
GSA Bulletin (2014) 126 (5-6): 773–790.
...Figure 10. Representative diagram of the Zielbach-Adige system evolution. (A) Immediately after the deglaciation of the main Venosta Valley, the Adige River deposits sediment in the whole valley width, partially following the early development of the Töllbach fan. (B) At ca. 12,000 yr B.P...
FIGURES | View All (11)
Journal Article
Published: 01 February 2008
Italian Journal of Geosciences (2008) 127 (1): 163–171.
... Valley power plants Southern Europe Tagliamento River Trentino-Alto Adige Italy Vaiont Landslide Veneto Italy ...
Journal Article
Journal: Geology
Published: 01 May 2012
Geology (2012) 40 (5): 455–458.
.../G20639.1 . Hinderer M. , 2001 , Late Quaternary denudation of the Alps, valley and lake fillings and modern river loads : GeodinamicaActa , v. 14 , p. 231 – 263 , doi:10.1016/S0985-3111(01)01070-1 . Hungr O. Morgan G.C. Kellerhals R. , 1984 , Quantitative analysis...
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Journal Article
Journal: Geology
Published: 01 December 2012
Geology (2012) 40 (12): 1067–1070.
...-glacial river network also provides an estimate of distribution and magnitude of glacial erosion and associated isostatic adjustment, suggesting an increase of valley-scale topographic relief and decrease of mean elevation throughout glaciation. We assume that the topography of a nonglaciated mountain...
FIGURES
Journal Article
Published: 01 October 2008
Italian Journal of Geosciences (2008) 127 (3): 519–532.
... Trentino), from the NE part of the Early Pemian Collio Basin to the west, up to the Val Rendena to the east. The prevalent whitish to greyish alluvial fan and braided river deposits of this formation composed dominantly of vein quartz and volcanic fragments and reaching a maximum thickness of about 100 m...
Journal Article
Published: 01 February 2018
Italian Journal of Geosciences (2018) 137 (1): 31–37.
...Francesca Castorina; Stefano Claudio Vaiani ABSTRACT The freshwater influence in the 87 Sr/ 86 Sr ratio of mollusk shells were analyzed within a late Quaternary subsurface succession of the Po River Delta (core 187-S1). Sr isotope ratios of the Po and others rivers’ (Brenta, Adige and Reno) waters...
FIGURES
Journal Article
Published: 08 April 2022
Journal of the Geological Society (2022) jgs2021-156.
... was confined within incised valleys ( Fontana et al. 2008 ). From then onward, a marine transgression occurred (i.e. post-glacial sea-level rise), and a highstand phase led to the upbuilding of the main alluvial ridges in the plain ( Favero and Serandrei Barbero 1980 ), including the Po and Adige Rivers...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2015
GSA Bulletin (2015) 127 (1-2): 113–130.
... Geologica Italiana , v. 24 , p. 71 – 77 . Galadini F. Galli P. , 1999 , Palaeoseismology related to the displaced Roman archaeological remains at Egna (Adige Valley, northern Italy) : Tectonophysics , v. 308 , p. 171 – 191 , doi:10.1016/S0040-1951(99)00080-3. Galadini F. Galli...
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Journal Article
Published: 01 February 2016
Italian Journal of Geosciences (2016) 135 (1): 95–108.
... the intellectual efforts of the author are aimed, essentially, at an attempt to reconcile the new discoveries of the geology of his time with the revealed truth of the Sacred Scriptures (see R omano , 2015 ). In describing the hydrographical status of the River Adige, and the alleged diversion...
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Journal Article
Published: 01 November 2008
Geochemistry: Exploration, Environment, Analysis (2008) 8 (3-4): 267–277.
.... The highest mountains are located in the Alps and include Monte Bianco (4810 m), Monte Rosa (4634 m) and Monte Cervino (4478 m). The largest lakes also occur in northern Italy and include Garda (370 km 2 ), Maggiore (212 km 2 ) and Como (146 km 2 ). The most important Italian rivers are the Po (652 km), Adige...
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Journal Article
Published: 01 February 2009
Italian Journal of Geosciences (2009) 128 (1): 201–215.
... earthquake is a key event for the seismicity of the whole Alps, because it is cited in almost all annals of Europe but it still presents substantial doubts about its precise epicentral area. In fact, only a delimitation of the main damaged area, in the southern Verona plain, along the River Adige, has been...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1953
AAPG Bulletin (1953) 37 (4): 601–653.
... under the heading of pre-Apennine foothills. Developments in the plain north of the foothills are considered under the headings of the central Po Plain and the eastern Po Plain; the latter is confined to the low land between the Adige and Reno rivers, the northern part of which is commonly known...
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Journal Article
Published: 01 March 2004
European Journal of Mineralogy (2004) 16 (2): 297–307.
... used in ceramic production, clays were also sampled in areas surrounding the archaeological sites, from alluvial deposits of the respective hydrographic basins: the river Po for Adria, the Adige for Este, the Brenta for Padova, and Würm deposits of the Brenta for Altino ( Maritan, 2002 ). Clay...
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Journal Article
Published: 02 December 2020
Environmental & Engineering Geoscience (2021) 27 (1): 95–111.
.... The Gadria catchment is located in the Vinschgau-Venosta Valley, eastern Italian Alps, and belongs to the Adige River basin ( Figure 1a ). At the fan apex, the catchment has a drainage area of 6.3 km 2 and ranges in elevation from 1,394 to 2,945 m a.s.l. ( Figure 1b ). The Gadria is underlain by paragneiss...