| Locality type: | Outcrop |
| Classification |
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| Species: | Scolecite |
| Formula: | CaAl2Si3O10 · 3H2O |
| Confirmation |
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| Validity: | Confirmed |
| Confirmation Methods: | Visually Identified |
| Data |
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| Mineral Data: | Click here to view Scolecite data |
| Locality Data: | Click here to view Krossanes, Hamarsfjörður, Djúpavogshreppur, Múlaþing, Eastern Region, Iceland |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 821985 |
| Long-form Identifier: | 1:3:821985:5 |
| GUID (UUID V4): | 6fee948d-54da-49eb-9b79-f4798f971ccc |
| Nearest other occurrences of Scolecite |
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| 10.2km (6.4 miles) | ⓘTitlingshagi, Berufjörður, Djúpavogshreppur, Múlaþing, Eastern Region, Iceland |
| 18.9km (11.8 miles) | ⓘFossárfell, Berufjörður, Djúpavogshreppur, Múlaþing, Eastern Region, Iceland |
| 20.2km (12.5 miles) | ⓘBerufjarðara, Berufjarðará Valley, Berufjörður, Djúpavogshreppur, Múlaþing, Eastern Region, Iceland |
| 21.4km (13.3 miles) | ⓘDjupidalur, Breiðdalsvík, Fjarðabyggð, Eastern Region, Iceland |
| 21.6km (13.4 miles) | ⓘÓsfjall, Breiðdalsvík, Fjarðabyggð, Eastern Region, Iceland |
| 22.0km (13.7 miles) | ⓘSkriðudalur, Breiðdalur, Fjarðabyggð, Eastern Region, Iceland |
| 24.1km (15.0 miles) | ⓘAusturhorn Intrusion, Hornafjörður, Southern Region, Iceland |
| 60.5km (37.6 miles) | ⓘQuarry at Oddskarðsvegur, Neskaupstaður, Fjarðabyggð, Eastern Region, Iceland |
| References |
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| Reference Search (possible matching items) |
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 | | Journal (article/letter/editorial) | | Basal Complex of the Austurhorn Intrusion (SE Iceland) DEPARTMENT OF EARTH SCIENCES, INSTITUTE OF GEOCHEMISTRY...TheTertiary Austurhorn intrusive complex in SE Iceland represents an exhumed magma chamber that has recorded...Geological map of the Austurhorn intrusion in SE Iceland (after Blake, 1966). The Hvalnesfjall gabbro crops...1999; Preston, 2001). In Iceland several intrusive complexes occur on the eastern side of the island (i...located in southeastern Iceland (Fig. 1). As most active central volcanoes in Iceland typically erupt magmas |  | | Journal (article/letter/editorial) | | grade of metamorphism was attained in the axial region of the geosyncline where these and Lower Jurassic...a hot-spring and fumarole area in the volcanic region of New Zealand, numerous wells have been drilled...described a consistent sequence epidote-prehnite-scolecite in olivine basalts of Ben More, Mull, which he...to be quantitatively insignificant, although scolecite and chabazite are reported by NIGGLI et al. (1940)...through the two-phase region of water the slopes must change rapidly, but above this region they will be steep |
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