English version | |||||
NATURSTEINSDATABASEN | |||||
Registrering 3301 - 602 Solbergelva 1 | |||||
(Objekt Id: 15389) (Sist oppdatert: 28.01.2010) |
|
Lokalisering |
Fylke: | Buskerud | Kommune: | Drammen (3301) |
Kart 1:50000: | Lier (1814-4) | Kart 1:250000: | Oslo |
Koordinatsystem: | EU89-UTM Zone 32 |
Øst: | 561100 m. | Nord: | 6626060 m. |
Lengdegrad: | 10.0878410 | Breddegrad: | 59.7678610 |
Kartvisning |
|
Ressurs |
Ressurstype: | Granitt og andre størkningsbergarter | Ressursundertype: | Granitt | |
Murestein(Y/N): | N |
Betydning |
Råstoffbetydning: | Liten betydning (reg. 18.02.2015) |
Historisk: | Ja , (Stadfestet 14.sep.2004 av Leif Furuhaug) |
Ressurser og produksjon |
Aktivitet: | Steinbrudd | Reserver: | ||
Driftsmetode: | Dagbrudd | Historisk produksjon: |
Forekomstbergart |
Litologi: | Forvitringsfarge: | |||
Genese: | Form: | |||
Hovedtekstur: |
Kornstørrelse: | Hovedomvandling: |
Strøk/Fall: | Retning: | |||
Feltstupning: |
Stratigrafisk klassifikasjon av vertsbergart |
Æra: | Periode: |
Provins: | ||
Geotek.enhet: | ||
Tektonisk complex: | ||
Intrusivt komplex: |
Gruppe: | Formasjon: |
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: |
|
Litteraturfortegnelser: |
Fra NGU's Referansearkiv.: |
Oxaal, John , 1916 |
Norsk granit |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 sider |
Abstrakt: | |
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 lokalitet: Solbergelva 2 |
(Objekt Id: 15393 602,01,00) |
|
Lokalisering |
Fylke: | Buskerud | Kommune: | Drammen (3301) |
Kart 1:50000: | Lier (1814-4) | Kart 1:250000: | Oslo |
Koordinatsystem: | EU89-UTM Zone 32 |
Øst: | 561240 m. | Nord: | 6626040 m. |
Lengdegrad: | 10.0903270 | Breddegrad: | 59.7676610 |
Kartvisning |
|
Ressurs |
Ressurstype: | Granitt og andre størkningsbergarter | Ressursundertype: | Granitt | |
Murestein(Y/N): |
Betydning |
Historisk: | Ja , (Stadfestet 14.sep.2004 av Leif Furuhaug) |
Ressurser og produksjon |
Aktivitet: | Steinbrudd | Reserver: | ||
Driftsmetode: | Dagbrudd | Historisk produksjon: |
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: |
|
Litteraturfortegnelser: |
Fra NGU's Referansearkiv.: |
Oxaal, John , 1916 |
Norsk granit |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 sider |
Abstrakt: | |
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 lokalitet: Solbergelva 3 |
(Objekt Id: 15395 602,02,00) |
|
Lokalisering |
Fylke: | Buskerud | Kommune: | Drammen (3301) |
Kart 1:50000: | Lier (1814-4) | Kart 1:250000: | Oslo |
Koordinatsystem: | EU89-UTM Zone 32 |
Øst: | 561053 m. | Nord: | 6625980 m. |
Lengdegrad: | 10.0869970 | Breddegrad: | 59.7671580 |
Kartvisning |
|
Ressurs |
Ressurstype: | Granitt og andre størkningsbergarter | Ressursundertype: | Granitt | |
Murestein(Y/N): |
Betydning |
Historisk: | Ja , (Stadfestet 14.sep.2004 av Leif Furuhaug) |
Ressurser og produksjon |
Aktivitet: | Steinbrudd | Reserver: | ||
Driftsmetode: | Dagbrudd | Historisk produksjon: |
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: |
|
Litteraturfortegnelser: |
Fra NGU's Referansearkiv.: |
Oxaal, John , 1916 |
Norsk granit |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 sider |
Abstrakt: | |
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 lokalitet: Solbergelva 4 |
(Objekt Id: 15403 602,03,00) |
|
Lokalisering |
Fylke: | Buskerud | Kommune: | Drammen (3301) |
Kart 1:50000: | Lier (1814-4) | Kart 1:250000: | Oslo |
Koordinatsystem: | EU89-UTM Zone 32 |
Øst: | 561169 m. | Nord: | 6625950 m. |
Lengdegrad: | 10.0890540 | Breddegrad: | 59.7668630 |
Kartvisning |
|
Ressurs |
Ressurstype: | Granitt og andre størkningsbergarter | Ressursundertype: | Granitt | |
Murestein(Y/N): |
Betydning |
Historisk: | Ja , (Stadfestet 17.sep.2004 av Leif Furuhaug) |
Ressurser og produksjon |
Aktivitet: | Steinbrudd | Reserver: | ||
Driftsmetode: | Dagbrudd | Historisk produksjon: |
Opplysning(er) i fritekstformat |
Beskrivelse |
Lite brudd i tett granskog. |
Beliggenhet |
Bruddet ligger nær hovedbuddet og Solbergelva 3. |
Bilde(r) fra forekomstområdet: |
|
Litteraturfortegnelser: |
Fra NGU's Referansearkiv.: |
Oxaal, John , 1916 |
Norsk granit |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 sider |
Abstrakt: | |
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 lokalitet: Solbergelva 5 |
(Objekt Id: 15405 602,04,00) |
|
Lokalisering |
Fylke: | Buskerud | Kommune: | Drammen (3301) |
Kart 1:50000: | Lier (1814-4) | Kart 1:250000: | Oslo |
Koordinatsystem: | EU89-UTM Zone 32 |
Øst: | 561190 m. | Nord: | 6625939 m. |
Lengdegrad: | 10.0894080 | Breddegrad: | 59.7667700 |
Kartvisning |
|
Ressurs |
Ressurstype: | Granitt og andre størkningsbergarter | Ressursundertype: | Granitt | |
Murestein(Y/N): |
Betydning |
Historisk: | Ja , (Stadfestet 17.sep.2004 av Leif Furuhaug) |
Ressurser og produksjon |
Aktivitet: | Steinbrudd | Reserver: | ||
Driftsmetode: | Dagbrudd | Historisk produksjon: |
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: |
|
Litteraturfortegnelser: |
Fra NGU's Referansearkiv.: |
Oxaal, John , 1916 |
Norsk granit |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.76;1-220 sider |
Abstrakt: | |
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. |
Faktaarket ble generert 28.03.2024 |
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