English version
NATURSTEINSDATABASEN
Forekomstområde 602 - 601
(Sist oppdatert 12.feb.2010)

Navn på deposit area : Aronsløkka 1
(Objekt Id : 0602,601,00,00)
Forekomstområdet tilhører provinsen : Drammensgranitt

Lokalisering
Fylke : Buskerud (06) Kommune : Drammen (0602)
Kart 1:50000: Lier (1814-4) Kart 1:250000: Oslo
Markeringspunkt: Lengdegrad: 10.1229470 Breddegrad: 59.7634350
EU89-UTM Zone 32 (Coordinates IS confirmed)
X-koord: 563080 m. Y-koord: 6625600 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: 300 m3

Betydning
Offentlig: Little Importance (reg. 18.02.2015)
Economical: Lite viktig , (Confirmed 09.sep.2004 by Leif Furuhaug)
Historical: Yes , (Confirmed 09.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
Skrottipp på 30x10 m tyder på relativt stor produksjon. Bergarten er rød, middelskornet og massiv granitt, typisk Drammensgranitt. Det antas at stein fra bruddene langs denne stien for det meste ble brukt ti husmurer nede i byen.
Beliggenhet
I sørhellinga nord for Drammen, mellom Bråtan og Solbergelva, ligger en rekke gamle brudd i Drammensgranitt. En gang/sykkelsti går på nordsiden av bebyggelsen i Solbergelva. Forekomstene ligger langs denne stien. Aronsløkka 1 ligger ved østenden av stien, der denne går over til bilvei.

Bilde(r) fra forekomstområdet:
Photo no. 1 showing Bruddet med noen utbrudte blokker"

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 : Aronsløkka 2
(Objekt Id : 0602,601,01,00)

Lokalisering
Fylke : Buskerud (06) Kommune : Drammen (0602)
Kart 1:50000: Lier (1814-4) Kart 1:250000: Oslo
Markeringspunkt: Lengdegrad: 10.1218850 Breddegrad: 59.7636230
EU89-UTM Zone 32 (Coordinates IS confirmed)
X-koord: 563020 m. Y-koord: 6625619 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 09.sep.2004 by Leif Furuhaug)

Opplysning(er) i fritekstformat
Beskrivelse
Samme bergart som hovedforekomsten, og sannsynligvis gått til samme anvendelse.
Beliggenhet
Forekomsten ligger 50 m vest for hovedforekomsten.

Bilde(r) fra forekomstområdet:
Photo no. 1 showing Bruddet med noen utbrudte blokk"

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 : Aronsløkka 3
(Objekt Id : 0602,601,02,00)

Lokalisering
Fylke : Buskerud (06) Kommune : Drammen (0602)
Kart 1:50000: Lier (1814-4) Kart 1:250000: Oslo
Markeringspunkt: Lengdegrad: 10.1208160 Breddegrad: 59.7642320
EU89-UTM Zone 32 (Coordinates IS confirmed)
X-koord: 562958 m. Y-koord: 6625686 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 05.okt.2004 by Leif Furuhaug)

Opplysning(er) i fritekstformat
Beskrivelse
Ingen aktivitet her, men viser hvor massiv og godt egnet for bryting bergarten er.
Beliggenhet
Lokaliteten ligger140 m VNV for hovedforekomsten.

Bilde(r) fra forekomstområdet:
Photo no. 1 showing Stor bergartsflate"

Navn på locality : Aronsløkka 4
(Objekt Id : 0602,601,03,00)

Lokalisering
Fylke : Buskerud (06) Kommune : Drammen (0602)
Kart 1:50000: Lier (1814-4) Kart 1:250000: Oslo
Markeringspunkt: Lengdegrad: 10.1201230 Breddegrad: 59.7641770
EU89-UTM Zone 32 (Coordinates IS confirmed)
X-koord: 562920 m. Y-koord: 6625679 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 09.sep.2004 by Leif Furuhaug)

Opplysning(er) i fritekstformat
Beskrivelse
Samme bergart som hovedforekomsten, og sannsynligvis gått til samme anvendelse.
Beliggenhet
Ligger 175 m VNV for hovedforekomsten.

Bilde(r) fra forekomstområdet:
Photo no. 1 showing Bruddområde med noen blokker"

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 : Aronsløkka 5
(Objekt Id : 0602,601,04,00)

Lokalisering
Fylke : Buskerud (06) Kommune : Drammen (0602)
Kart 1:50000: Lier (1814-4) Kart 1:250000: Oslo
Markeringspunkt: Lengdegrad: 10.1183020 Breddegrad: 59.7646020
EU89-UTM Zone 32 (Coordinates IS confirmed)
X-koord: 562816 m. Y-koord: 6625725 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 09.sep.2004 by Leif Furuhaug)

Opplysning(er) i fritekstformat
Beskrivelse
Samme bergart som hovedforekomsten, og sannsynligvis gått til samme anvendelse.
Beliggenhet
Ligger 280 m VNV for hovedforekomsten, like N for lysløype.

Bilde(r) fra forekomstområdet:
Photo no. 1 showing Brytningsområde"

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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