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English version | ||||
| NATURSTEINSDATABASEN | |||||
| Forekomstområde 625 - 602 | |||||
| (Sist oppdatert 28.jan.2010) | |||||
Navn på deposit area : Solbergelva 1 |
| (Objekt Id : 0625,602,00,00) |
| Forekomstområdet tilhører provinsen : Drammensgranitt |
| Lokalisering |
| Fylke : | Buskerud (06) | Kommune : | Nedre Eiker (0625) |
| Kart 1:50000: | Lier (1814-4) | Kart 1:250000: | Oslo |
| Markeringspunkt: | Lengdegrad: | 10.0878410 | Breddegrad: | 59.7678610 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 561100 m. | Y-koord: | 6626060 m. |
|
|
| Materialtype |
| Hovedtype: | Granitt og andre størkningsbergarter | Subtype: | Granitt | |
| Brickstone(Y/N): | N |
| Production |
| Activity: | Steinbrudd | Reserves: | ||
| Prod. method: | Dagbrudd | Production: | ||
| Prod. status: | Nedlagt | Volume of dump: |
| Betydning |
| Offentlig: | Little Importance (reg. 18.02.2015) |
| Economical: | Lite viktig , (Confirmed 14.sep.2004 by Leif Furuhaug) |
| Historical: | Yes , (Confirmed 14.sep.2004 by Leif Furuhaug) |
Deposit rock |
| Lithology: | Weathering colour: | |||
| Era: | Period: | |||
| Dating: | Method: | |||
| Genesis: | Form: | |||
| Main texture: |
| Main grain size: | Main alteration: |
| Strike/Dip: | Direction: | |||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Period: |
| Province: | ||
| Geotec.unit: | ||
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Formation: |
Opplysning(er) i fritekstformat |
| Beskrivelse |
| Bruddet har vært drevet på en ca 2,5 m høy benk og dekker ei flate på 30 mx40 m. Flata er svakt hellende mot syd (SF090°/10°). Forekomsten ligger i samme draget som Aronsløkka, Kjøsterud og Åserud, og bergarten skiller seg lite fra disse forekomstene. |
| Beliggenhet |
| Forekomsten er beliggende like NØ for bebyggelsen i Solbergelva. |
| Bilde(r) fra forekomstområdet: |
|
Bibliography: |
| From NGU's Reference Archive: |
| Oxaal, John , 1916 |
| Norsk granit |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 pages |
| Abstract: | |
| This work is a report of granite and the granite industry in Norway. It contains a description of the various fields of granite and similar rocks from a scientific as well as from a technical and economical standpoint. The geological occurrence of the various rocks, their chemical and mineralogical composition, are thoruoughlyoughly treated, also the questions of practical interest, as the quality and other technical properties, further the problems of location and conditions for transport, conditions for quarrying and otherquestions of interest in the utilization of the various occurrences of granite. Granite: This chapter consideres first the mineralogical and chemical composition of the granite, and the various types of granite resulting from the varying composition; thereafter the most important structural types and how these are dependent on the geological appearance of the rock. Lakkolites and other froms assumed by granite masses when injected into the crust of the earth, are mentioned; some examples of beautifully formed lakkolites are also mentioned. The question of sheet structure and rift in the granite are of great importance in its utilization, and are of interest both practically and theoretically. |
Navn på locality : Solbergelva 2 |
| (Objekt Id : 0625,602,01,00) |
| Lokalisering |
| Fylke : | Buskerud (06) | Kommune : | Nedre Eiker (0625) |
| Kart 1:50000: | Lier (1814-4) | Kart 1:250000: | Oslo |
| Markeringspunkt: | Lengdegrad: | 10.0903270 | Breddegrad: | 59.7676610 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 561240 m. | Y-koord: | 6626040 m. |
|
|
| Materialtype |
| Hovedtype: | Granitt og andre størkningsbergarter | Subtype: | Granitt | |
| Brickstone(Y/N): |
| Production |
| Activity: | Steinbrudd | Reserves: | ||
| Prod. method: | Dagbrudd | Production: | ||
| Prod. status: | Nedlagt | Volume of dump: |
| Betydning |
| Historical: | Yes , (Confirmed 14.sep.2004 by Leif Furuhaug) |
Opplysning(er) i fritekstformat |
| Beskrivelse |
| Drammensgranitt lik den som ellers er i området. Ca. 80 m langt bruddområde langs sti i tett barskog. |
| Beliggenhet |
| Dette bruddet ligger ca. 150 m øst for hovedbruddet. |
| Bilde(r) fra forekomstområdet: |
|
Bibliography: |
| From NGU's Reference Archive: |
| Oxaal, John , 1916 |
| Norsk granit |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 pages |
| Abstract: | |
| This work is a report of granite and the granite industry in Norway. It contains a description of the various fields of granite and similar rocks from a scientific as well as from a technical and economical standpoint. The geological occurrence of the various rocks, their chemical and mineralogical composition, are thoruoughlyoughly treated, also the questions of practical interest, as the quality and other technical properties, further the problems of location and conditions for transport, conditions for quarrying and otherquestions of interest in the utilization of the various occurrences of granite. Granite: This chapter consideres first the mineralogical and chemical composition of the granite, and the various types of granite resulting from the varying composition; thereafter the most important structural types and how these are dependent on the geological appearance of the rock. Lakkolites and other froms assumed by granite masses when injected into the crust of the earth, are mentioned; some examples of beautifully formed lakkolites are also mentioned. The question of sheet structure and rift in the granite are of great importance in its utilization, and are of interest both practically and theoretically. |
Navn på locality : Solbergelva 3 |
| (Objekt Id : 0625,602,02,00) |
| Lokalisering |
| Fylke : | Buskerud (06) | Kommune : | Nedre Eiker (0625) |
| Kart 1:50000: | Lier (1814-4) | Kart 1:250000: | Oslo |
| Markeringspunkt: | Lengdegrad: | 10.0869970 | Breddegrad: | 59.7671580 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 561053 m. | Y-koord: | 6625980 m. |
|
|
| Materialtype |
| Hovedtype: | Granitt og andre størkningsbergarter | Subtype: | Granitt | |
| Brickstone(Y/N): |
| Production |
| Activity: | Steinbrudd | Reserves: | ||
| Prod. method: | Dagbrudd | Production: | ||
| Prod. status: | Nedlagt | Volume of dump: |
| Betydning |
| Historical: | Yes , (Confirmed 14.sep.2004 by Leif Furuhaug) |
Opplysning(er) i fritekstformat |
| Beskrivelse |
| Forekomsten er et lite brudd på 15mx15m. |
| Beliggenhet |
| Beliggenhet til bruddet er ca. 50 m syd for hovedforekomsten. |
| Bilde(r) fra forekomstområdet: |
|
Bibliography: |
| From NGU's Reference Archive: |
| Oxaal, John , 1916 |
| Norsk granit |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 pages |
| Abstract: | |
| This work is a report of granite and the granite industry in Norway. It contains a description of the various fields of granite and similar rocks from a scientific as well as from a technical and economical standpoint. The geological occurrence of the various rocks, their chemical and mineralogical composition, are thoruoughlyoughly treated, also the questions of practical interest, as the quality and other technical properties, further the problems of location and conditions for transport, conditions for quarrying and otherquestions of interest in the utilization of the various occurrences of granite. Granite: This chapter consideres first the mineralogical and chemical composition of the granite, and the various types of granite resulting from the varying composition; thereafter the most important structural types and how these are dependent on the geological appearance of the rock. Lakkolites and other froms assumed by granite masses when injected into the crust of the earth, are mentioned; some examples of beautifully formed lakkolites are also mentioned. The question of sheet structure and rift in the granite are of great importance in its utilization, and are of interest both practically and theoretically. |
Navn på locality : Solbergelva 4 |
| (Objekt Id : 0625,602,03,00) |
| Lokalisering |
| Fylke : | Buskerud (06) | Kommune : | Nedre Eiker (0625) |
| Kart 1:50000: | Lier (1814-4) | Kart 1:250000: | Oslo |
| Markeringspunkt: | Lengdegrad: | 10.0890540 | Breddegrad: | 59.7668630 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 561169 m. | Y-koord: | 6625950 m. |
|
|
| Materialtype |
| Hovedtype: | Granitt og andre størkningsbergarter | Subtype: | Granitt | |
| Brickstone(Y/N): |
| Production |
| Activity: | Steinbrudd | Reserves: | ||
| Prod. method: | Dagbrudd | Production: | ||
| Prod. status: | Nedlagt | Volume of dump: |
| Betydning |
| Historical: | Yes , (Confirmed 17.sep.2004 by Leif Furuhaug) |
Opplysning(er) i fritekstformat |
| Beskrivelse |
| Lite brudd i tett granskog. |
| Beliggenhet |
| Bruddet ligger nær hovedbuddet og Solbergelva 3. |
| Bilde(r) fra forekomstområdet: |
|
Bibliography: |
| From NGU's Reference Archive: |
| Oxaal, John , 1916 |
| Norsk granit |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 pages |
| Abstract: | |
| This work is a report of granite and the granite industry in Norway. It contains a description of the various fields of granite and similar rocks from a scientific as well as from a technical and economical standpoint. The geological occurrence of the various rocks, their chemical and mineralogical composition, are thoruoughlyoughly treated, also the questions of practical interest, as the quality and other technical properties, further the problems of location and conditions for transport, conditions for quarrying and otherquestions of interest in the utilization of the various occurrences of granite. Granite: This chapter consideres first the mineralogical and chemical composition of the granite, and the various types of granite resulting from the varying composition; thereafter the most important structural types and how these are dependent on the geological appearance of the rock. Lakkolites and other froms assumed by granite masses when injected into the crust of the earth, are mentioned; some examples of beautifully formed lakkolites are also mentioned. The question of sheet structure and rift in the granite are of great importance in its utilization, and are of interest both practically and theoretically. |
Navn på locality : Solbergelva 5 |
| (Objekt Id : 0625,602,04,00) |
| Lokalisering |
| Fylke : | Buskerud (06) | Kommune : | Nedre Eiker (0625) |
| Kart 1:50000: | Lier (1814-4) | Kart 1:250000: | Oslo |
| Markeringspunkt: | Lengdegrad: | 10.0894080 | Breddegrad: | 59.7667700 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 561190 m. | Y-koord: | 6625939 m. |
|
|
| Materialtype |
| Hovedtype: | Granitt og andre størkningsbergarter | Subtype: | Granitt | |
| Brickstone(Y/N): |
| Production |
| Activity: | Steinbrudd | Reserves: | ||
| Prod. method: | Dagbrudd | Production: | ||
| Prod. status: | Nedlagt | Volume of dump: |
| Betydning |
| Historical: | Yes , (Confirmed 17.sep.2004 by Leif Furuhaug) |
Opplysning(er) i fritekstformat |
| Beskrivelse |
| Bruddet er noe større enn de andre lokalitetene her, lengden på uttaksområdet er ca. 20 m og avsenkningen 1-2 m. |
| Beliggenhet |
| Dette er det nederste av bruddene i Solbergelva. Det ligger like over bebyggelsen, inntil en hesteinnhegning. |
| Bilde(r) fra forekomstområdet: |
|
Bibliography: |
| From NGU's Reference Archive: |
| Oxaal, John , 1916 |
| Norsk granit |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 pages |
| Abstract: | |
| This work is a report of granite and the granite industry in Norway. It contains a description of the various fields of granite and similar rocks from a scientific as well as from a technical and economical standpoint. The geological occurrence of the various rocks, their chemical and mineralogical composition, are thoruoughlyoughly treated, also the questions of practical interest, as the quality and other technical properties, further the problems of location and conditions for transport, conditions for quarrying and otherquestions of interest in the utilization of the various occurrences of granite. Granite: This chapter consideres first the mineralogical and chemical composition of the granite, and the various types of granite resulting from the varying composition; thereafter the most important structural types and how these are dependent on the geological appearance of the rock. Lakkolites and other froms assumed by granite masses when injected into the crust of the earth, are mentioned; some examples of beautifully formed lakkolites are also mentioned. The question of sheet structure and rift in the granite are of great importance in its utilization, and are of interest both practically and theoretically. |
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