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Norsk versjon | ||||
| THE INDUSTRIAL MINERAL DATABASE | |||||
| Deposit Area 1528 - 302 | |||||
| (Last updated 27.jun.2025) | |||||
Name of Deposit Area : Lyshol |
| (Object Id : 1528,302,00,00) |
| Location |
| County : | Møre og Romsdal (15) | Municipality : | Sykkylven (1528) |
| Map 1:50000: | Sykkylven (1219-4) | Map 1:250000: | Ålesund |
| Marking point: | Longitude: | 6.6364950 | Latitude: | 62.4022100 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-coord: | 377860 m. | Y-coord: | 6921221 m. |
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| Commodity |
| Main Type: | Carbonates | Sub Type: | Limestone |
| Production |
| Activity: | Mining | Reserves: | ||
| Prod. method: | Open pit and underground mining | Production: | ||
| Prod. status: | Disused, closed | Volume of dump: |
| Importance |
| Public: | Little Importance (reg. 29.10.2020) |
| Economical: | Not classified/evaluated , (Confirmed 24.feb.2014 by Agnes Raaness) |
Products |
| Element/product | Crude ore grade or quality | |
| LIME | % |
Operations |
| From - To | Activity | Comments | |
| 1880 - 1889 | Regular production | Company/Institution :Lokale | |
| Produksjon av brent kalk. | |||
| 1912 - 1920 | Regular production | Company/Institution :H. Schmidt & O. B. Nilsen. | |
| Sementproduksjon på Blindheim. Dabbet av fra 1920-tallet før den stoppet helt opp. Sist i 1930-årene var de ti en kort periode virksomhet. | |||
| 1946 - 1946 | Test mining | Company/Institution :August Musæus |
Mineralization |
| Era: | Period: | |||
| Dating: | Method: | |||
| Genesis: | Form: | |||
| Main texture: | Min. distribution: |
| Main grain size: |
| Strike/Dip: | Direction: | |||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Proterozoic | Period: |
| Province: | Caledonian Basement Province | |
| Geotec.unit: | Western Gneiss Region | |
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Formation: |
Information(s) in free text format |
| Free text |
| Bugge (1905) beskriver den som hvit og "i almindelighed middelkornig." Marmordraget kan følges fra Lyshol til Andestadvannet, en strekning på 3-400 m, men Kalkspatmarmor-drag ved Lyshol gård. Kalkbrudd drevet periodevis fra 1880-1946. Steinen ble kjørt ned til Blindheim der den ble brent i en kalkovn som nå er restaurert. (Heltzen 1996) |
Bibliography: |
| From NGU's Reference Archive: |
| Heltzen, Anders M. , 1996 |
| Bergverksdrift på Sunnmøre i gammel og ny tid. |
| ;Norsk Bergverksmuseum;RAPPORT;Skrift; No.10;70 s. pages |
| Bugge, Carl , 1905 |
| VI. Kalksten og marmor i Romsdals amt |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.43;37 pages |
| Abstract: | |
| Forkortet: In the present paper it is shown, that the Romsdalen, in the Northwestern part of Norway in the Algonkian Formation, there occur some extensive beds of lime- stone which are more fit for the carbide- and sulphite-industry than those of the Oslo region. Limestone also occurs in the environs of Trondheim and in the Northern part of Norway here occurring together with some dolomites and they commonly show rather a high percentage of magnesia. Limestones also occur in the Southern and the Western part of Norway ( Kristiansand-Stavanger-Bergen). The author has made 8 analyses of limestone from Romsdalen (p.8). Besides on pp. 10 and 11 there will be found analyses from the Oslo region, on p.13 from Northern Norway and on p.14 from the environs of Trondheim. In Romsdalen the limestone contains the following minerals: quartz, scapolite, white mica, oligoclase, apatite, pyrite, graphite, garnet, pyroxene, amphibole, biotite and occasionally a green mica. The structure of these Algonkian limestones ahow partly those features which are common with contact-metamorphic marble, partly those which are common with regional-metamorphic marble, and they are therefore likely to possess an intermediate character. |
| Bøckman, K.L. , 1967 |
| Norges kalksteins- og kvartsforekomster. |
| ;Elektrokemisk A/S;FAGRAPPORT; UTREDNINGSRAPPORT;Bergarkivet; No.BA 5245;89 + 61 pages |
| Vogt, Johan H.L. , 1897 |
| Norsk marmor |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.22;1-364 pages |
| Abstract: | |
| Forkortet: Diese Arbeit zerfällt in vier Hauptabschnitte. 1. Über die Geologie des Marmors (S.4-18). 2. Über die wichtigsten Eigenschaften des Marmors, mit besonderer Rücksicht auf die norwegischen Marmorarten daneben über Betrieb usw der Brüche (S. 18-158). 3. Über die wichtigsten norwegischen Marmorfelder, hauptsächlich in der nord- norwegischen Glimmerschiefer-Marmor-Gruppe (S. 159-268); weiter in den Trondheim-schen Schiefern (S. 269-282): im Grundgebirge (S. 282-291); in der Bergen-schen Schiefern (S. 291-296), und Contactmarmor in dem Oslo-Gebiet (S. 296-303). 4. Zum Schluss eine wirthschaftliche über die Marmorproduction der Welt und über die Entwicklung der norwegischen Marmorindustrie. |
| The fact sheet was created on 03.07.2025 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
| Copyright © 2025 Geological Survey of Norway |