| Locality type: | Scree Slope |
| Classification |
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| Species: | Diopside |
| Formula: | CaMgSi2O6 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Diopside data |
| Locality Data: | Click here to view Canaleta, Casaccia, Upper Val Bregaglia, Bregaglia, Maloja Region, Grisons, Switzerland |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 559834 |
| Long-form Identifier: | 1:3:559834:2 |
| GUID (UUID V4): | d4ed95a3-2400-40a2-b018-a5580db83f9b |
| Nearest other occurrences of Diopside |
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| 0.8km (0.5 miles) | ⓘPiz Lunghin, Casaccia, Upper Val Bregaglia, Bregaglia, Maloja Region, Grisons, Switzerland |
| 0.9km (0.6 miles) | ⓘPiz dal Sasc, Casaccia, Upper Val Bregaglia, Bregaglia, Maloja Region, Grisons, Switzerland |
| 9.1km (5.7 miles) | ⓘForno glacier, Val Forno, Upper Val Bregaglia, Bregaglia, Maloja Region, Grisons, Switzerland |
| 11.1km (6.9 miles) | ⓘPlatta nappe, Surses, Albula Region, Grisons, Switzerland |
| 11.4km (7.1 miles) | ⓘCotschens deposit, Marmorera lake, Surses, Albula Region, Grisons, Switzerland |
| 13.2km (8.2 miles) | ⓘUralite’s plain, Sissone Valley, Chiesa in Valmalenco, Sondrio Province, Lombardy, Italy |
| 13.4km (8.3 miles) | ⓘTremogge Peak, Chiesa in Valmalenco, Sondrio Province, Lombardy, Italy |
| 13.4km (8.3 miles) | ⓘDiopside outcrop, Sissone Valley, Chiesa in Valmalenco, Sondrio Province, Lombardy, Italy |
| 14.1km (8.8 miles) | ⓘSissone Valley, Chiesa in Valmalenco, Sondrio Province, Lombardy, Italy |
| 16.6km (10.3 miles) | ⓘGiavera, Villa di Chiavenna, Sondrio Province, Lombardy, Italy |
| References |
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| Reference Search (possible matching items) |
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 | | Book (edition) | | anticlinal triclin,co anortos1ta valle antecedente. val!e ep1genet1co antrac,ta antracifero antraco-silicos...arg1ll0,calcareous arg1ll0-ferruginous argyrod1te and region arxose arm leqord leqiirnsten Ieng sandsten lerskiffer...arglllite arg1lregion ande <1rkose montant (oe cad'e). pieddro11 armatures...eau ascendanie montee, ascension, remontee rampe region ase1sm1que teneur en cendres 568 569 570 ash...trepano de hojas quebrar1taoora de mandibulas Blake canaleta de pano tiro, volaoura d1sparar, pega•, ven1ilar |  | | Report (issue) | | foreland region. The batholith is exposed at mesozonal levels, whereas the foreland region is exposed...reduced. PREVIOUS AND CURRENT RESEARCH The region is extremely remote and geochronological studies...beneath the South American Plate (Fig. 1). This region has probably been an active continental margin...of the batholith, much of the area was a forearc region where various litho-tectonic assemblages were accreted...inflation. For example, in the Tierra del Fuego region, the data of Hervé and others (1984) and Suarez |
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