(Last updated: 28.01.2010)
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Norsk versjon | ||||
| THE NATURAL STONE DATABASE | |||||
| Occurence 3301 - 602 Solbergelva 1 | |||||
| (Object Id: 15389) (Last updated: 28.01.2010) |
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| Location |
| County: | Buskerud | Municipality: | Drammen (3301) |
| Map 1:50000: | Lier (1814-4) | Map 1:250000: | Oslo |
| Coordinate system: | EU89-UTM Zone 32 |
| East: | 561100 m. | North: | 6626060 m. |
| Longitude: | 10.0878410 | Latitude: | 59.7678610 |
| Show on map |
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| Resource |
| Resource Type: | Granite and other igneous rocks | Resource Subtype: | Granite | |
| Brickstone(Y/N): | N |
| Importance |
| Raw material meaning: | Little Importance (reg. 18.02.2015) |
| Historical: | Yes , (Confirmed 14.sep.2004 by Leif Furuhaug) |
| Resources and production |
| Activity: | Stone quarrying | Reserves: | ||
| Operating method: | Open pit mining | Historical production: |
Deposit rock |
| Lithology: | Weathering colour: | |||
| 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: |
Information(s) in free text format |
| Description |
| 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. |
| Location |
| Forekomsten er beliggende like NØ for bebyggelsen i Solbergelva. |
| Photo(s) from the Deposit area: |
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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. |
Name of Locality: Solbergelva 2 |
| (Object Id: 15393 602,01,00) |
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| Location |
| County: | Buskerud | Municipality: | Drammen (3301) |
| Map 1:50000: | Lier (1814-4) | Map 1:250000: | Oslo |
| Coordinate system: | EU89-UTM Zone 32 |
| East: | 561240 m. | North: | 6626040 m. |
| Longitude: | 10.0903270 | Latitude: | 59.7676610 |
| Show on map |
|
|
| Resource |
| Resource Type: | Granite and other igneous rocks | Resource Subtype: | Granite | |
| Brickstone(Y/N): |
| Importance |
| Historical: | Yes , (Confirmed 14.sep.2004 by Leif Furuhaug) |
| Resources and production |
| Activity: | Stone quarrying | Reserves: | ||
| Operating method: | Open pit mining | Historical production: |
Information(s) in free text format |
| Description |
| Drammensgranitt lik den som ellers er i området. Ca. 80 m langt bruddområde langs sti i tett barskog. |
| Location |
| Dette bruddet ligger ca. 150 m øst for hovedbruddet. |
| Photo(s) from the Deposit area: |
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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. |
Name of Locality: Solbergelva 3 |
| (Object Id: 15395 602,02,00) |
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| Location |
| County: | Buskerud | Municipality: | Drammen (3301) |
| Map 1:50000: | Lier (1814-4) | Map 1:250000: | Oslo |
| Coordinate system: | EU89-UTM Zone 32 |
| East: | 561053 m. | North: | 6625980 m. |
| Longitude: | 10.0869970 | Latitude: | 59.7671580 |
| Show on map |
|
|
| Resource |
| Resource Type: | Granite and other igneous rocks | Resource Subtype: | Granite | |
| Brickstone(Y/N): |
| Importance |
| Historical: | Yes , (Confirmed 14.sep.2004 by Leif Furuhaug) |
| Resources and production |
| Activity: | Stone quarrying | Reserves: | ||
| Operating method: | Open pit mining | Historical production: |
Information(s) in free text format |
| Description |
| Forekomsten er et lite brudd på 15mx15m. |
| Location |
| Beliggenhet til bruddet er ca. 50 m syd for hovedforekomsten. |
| Photo(s) from the Deposit area: |
|
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. |
Name of Locality: Solbergelva 4 |
| (Object Id: 15403 602,03,00) |
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| Location |
| County: | Buskerud | Municipality: | Drammen (3301) |
| Map 1:50000: | Lier (1814-4) | Map 1:250000: | Oslo |
| Coordinate system: | EU89-UTM Zone 32 |
| East: | 561169 m. | North: | 6625950 m. |
| Longitude: | 10.0890540 | Latitude: | 59.7668630 |
| Show on map |
|
|
| Resource |
| Resource Type: | Granite and other igneous rocks | Resource Subtype: | Granite | |
| Brickstone(Y/N): |
| Importance |
| Historical: | Yes , (Confirmed 17.sep.2004 by Leif Furuhaug) |
| Resources and production |
| Activity: | Stone quarrying | Reserves: | ||
| Operating method: | Open pit mining | Historical production: |
Information(s) in free text format |
| Description |
| Lite brudd i tett granskog. |
| Location |
| Bruddet ligger nær hovedbuddet og Solbergelva 3. |
| Photo(s) from the Deposit area: |
|
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. |
Name of Locality: Solbergelva 5 |
| (Object Id: 15405 602,04,00) |
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| Location |
| County: | Buskerud | Municipality: | Drammen (3301) |
| Map 1:50000: | Lier (1814-4) | Map 1:250000: | Oslo |
| Coordinate system: | EU89-UTM Zone 32 |
| East: | 561190 m. | North: | 6625939 m. |
| Longitude: | 10.0894080 | Latitude: | 59.7667700 |
| Show on map |
|
|
| Resource |
| Resource Type: | Granite and other igneous rocks | Resource Subtype: | Granite | |
| Brickstone(Y/N): |
| Importance |
| Historical: | Yes , (Confirmed 17.sep.2004 by Leif Furuhaug) |
| Resources and production |
| Activity: | Stone quarrying | Reserves: | ||
| Operating method: | Open pit mining | Historical production: |
Information(s) in free text format |
| Description |
| Bruddet er noe større enn de andre lokalitetene her, lengden på uttaksområdet er ca. 20 m og avsenkningen 1-2 m. |
| Location |
| Dette er det nederste av bruddene i Solbergelva. Det ligger like over bebyggelsen, inntil en hesteinnhegning. |
| Photo(s) from the Deposit area: |
|
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. |
| The fact sheet was created on 20.04.2024 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
| Copyright © 2024 Geological Survey of Norway |