.mw-parser-output .hidden-begin{box-sizing:border-box;width:100%;padding:5px;border:none;font-size:95%}.mw-parser-output .hidden-title{font-weight:bold;line-height:1.6;text-align:left}.mw-parser-output .hidden-content{text-align:left}@media all and (max-width:500px){.mw-parser-output .hidden-begin{width:auto!important;clear:none!important;float:none!important))You can help expand this article with text translated from the corresponding article in Italian. (May 2010) Click [show] for important translation instructions. View a machine-translated version of the Italian article. Machine translation, like DeepL or Google Translate, is a useful starting point for translations, but translators must revise errors as necessary and confirm that the translation is accurate, rather than simply copy-pasting machine-translated text into the English Wikipedia. Do not translate text that appears unreliable or low-quality. If possible, verify the text with references provided in the foreign-language article. You must provide copyright attribution in the edit summary accompanying your translation by providing an interlanguage link to the source of your translation. A model attribution edit summary is Content in this edit is translated from the existing Italian Wikipedia article at [[:it:Pizzo Strinato]]; see its history for attribution. You may also add the template ((Translated|it|Pizzo Strinato)) to the talk page. For more guidance, see Wikipedia:Translation.
Pizzo Strinato
Highest point
Elevation2,836 m (9,304 ft)
Coordinates46°4′N 10°5′E / 46.067°N 10.083°E / 46.067; 10.083
Geography
Pizzo Strinato is located in Lombardy
Pizzo Strinato
Pizzo Strinato
Parent rangeBergamo Alps

Pizzo Strinato is a mountain of Lombardy, Italy. It is located within the Bergamo Alps, approximately 55 kilometres (34 mi) northeast of Bergamo.[1] It rises 1,379 metres (4,524 ft) above Lago Belviso to the east and 703 metres (2,306 ft) above Lago del Barbellino to the northwest, forming a ridge with Monte Torena and Monte Costone between the two lakes.

Like many mountains in the region, it consists mostly of alternating sedimentary layers of S3 acidic volcanics extending the Collio Formation, which are deformed into sigmoid shapes by repeated minor thrust deformations on the north face and by the more significant D4 deformation event on the southeast face.[2]

Its highest ledges are home to the rare Eight-petal avens.[3]

References

[edit]
  1. ^ "Vetta Pizzo Strinato". www.maxpiantoni.it. Retrieved 2020-01-10.
  2. ^ Albini, S; Battaglia, D; Bellini, G; Bigoni, C; Carminati, E; Ceriani, S; Forcella, F; Gosso, G; Guizzetti, D; Oliva, A; Rebay, G; Siletto, G. B.; Spalla, M. I. (1994). "Alpine deformations and pre-Alpine remnants in the north-eastern Orobic Alps, Southalpine Belt" (PDF). Quad. Geodin. Alp. Quat 2: 35. Retrieved 15 March 2023.
  3. ^ DONADELLI, G; FERRANTI, R (2011). "Nuove segnalazioni floristiche per la provincia di Sondrio (Lombardia, Italia settentrionale)" (PDF). Il Naturalista Valtellinese. 22: 29–55. Retrieved 15 March 2023.

46°04′15″N 10°05′36″E / 46.07083°N 10.09333°E / 46.07083; 10.09333


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