English version
	NATURSTEINSDATABASEN
	Forekomstområde 602 - 602
	(Sist oppdatert 28.jan.2010)

Betydning

Offentlig:

Liten betydning (reg. 18.02.2015)

Økonomisk:

Lite viktig , (Stadfestet 13.sep.2004 av Leif Furuhaug)

Historisk:

Ja , (Stadfestet 13.sep.2004 av Leif Furuhaug)

Forekomstbergart

	Litologi:		Forvitringsfarge:
	Æra:		Periode:
	Datering:		Metode:
	Genese:		Form:
	Hovedtextur:

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

Forekomsten ligger i Åssida i Drammen, i samme draget og like vest for Aronsløkka (BU0010). Adkomst og beskrivelse forøvrig er som for Aronsløkka.

Bilde(r) fra forekomstområdet:

Foto nr. 1 viser "Store blokker" Foto nr. 2 viser "Store blokker"

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 : Kjøsterud 2

(Objekt Id : 0602,602,01,00)

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Lokalisering

Fylke :

Buskerud (06)

Kommune :

Drammen (0602)

Kart 1:50000:

Lier (1814-4)

Kart 1:250000:

Oslo

Markeringspunkt:

Lengdegrad:

10.1117760

Breddegrad:

59.7667550

EU89-UTM Zone 32

(Koordinatene ER bekreftet)

X-koord:

562446 m.

Y-koord:

6625959 m.

Materialtype

	Hovedtype:	Granitt og andre størkningsbergarter	Subtype:	Granitt
			Murestein(Y/N):

Produksjon

	Aktivitet:	Steinbrudd	Reserver:
	Prod. metode:	Dagbrudd	Produksjon:
	Prod. status:	Nedlagt	Tippvolum:

Betydning

Historisk:

Ja , (Stadfestet 13.sep.2004 av Leif Furuhaug)

Opplysning(er) i fritekstformat

Beliggenhet

Brudd like vest for hovedforekomst Kjøsterud.

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 : Kjøsterud 3

(Objekt Id : 0602,602,02,00)

---

Lokalisering

Fylke :

Buskerud (06)

Kommune :

Drammen (0602)

Kart 1:50000:

Lier (1814-4)

Kart 1:250000:

Oslo

Markeringspunkt:

Lengdegrad:

10.1112950

Breddegrad:

59.7664070

EU89-UTM Zone 32

(Koordinatene ER bekreftet)

X-koord:

562419 m.

Y-koord:

6625919 m.

Materialtype

	Hovedtype:	Granitt og andre størkningsbergarter	Subtype:	Granitt
			Murestein(Y/N):

Produksjon

	Aktivitet:	Steinbrudd	Reserver:
	Prod. metode:	Dagbrudd	Produksjon:
	Prod. status:	Nedlagt	Tippvolum:

Betydning

Historisk:

Ja , (Stadfestet 13.sep.2004 av Leif Furuhaug)

Opplysning(er) i fritekstformat

Beskrivelse

Brudd på 1-2 m høy benk som det er kilt ut blokk fra.

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 : Kjøsterud 4

(Objekt Id : 0602,602,03,00)

---

Lokalisering

Fylke :

Buskerud (06)

Kommune :

Nedre Eiker (0625)

Kart 1:50000:

Lier (1814-4)

Kart 1:250000:

Oslo

Markeringspunkt:

Lengdegrad:

10.1089840

Breddegrad:

59.7665170

EU89-UTM Zone 32

(Koordinatene ER bekreftet)

X-koord:

562289 m.

Y-koord:

6625930 m.

Materialtype

	Hovedtype:	Granitt og andre størkningsbergarter	Subtype:	Granitt
			Murestein(Y/N):

Produksjon

	Aktivitet:	Steinbrudd	Reserver:
	Prod. metode:	Dagbrudd	Produksjon:
	Prod. status:	Nedlagt	Tippvolum:

Betydning

Historisk:

Ja , (Stadfestet 13.sep.2004 av Leif Furuhaug)

Opplysning(er) i fritekstformat

Beskrivelse

Dette bruddet er anlagt ved å kile ut blokk fra en granittbenk.

Beliggenhet

Bruddet ligger like vest for forrige lokalitet (Kjøsterud 3).

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 : Kjøsterud 5

(Objekt Id : 0602,602,04,00)

---

Lokalisering

Fylke :

Buskerud (06)

Kommune :

Drammen (0602)

Kart 1:50000:

Lier (1814-4)

Kart 1:250000:

Oslo

Markeringspunkt:

Lengdegrad:

10.1107800

Breddegrad:

59.7672710

EU89-UTM Zone 32

(Koordinatene ER bekreftet)

X-koord:

562389 m.

Y-koord:

6626015 m.

Materialtype

	Hovedtype:	Granitt og andre størkningsbergarter	Subtype:	Granitt
			Murestein(Y/N):

Produksjon

	Aktivitet:	Steinbrudd	Reserver:
	Prod. metode:	Dagbrudd	Produksjon:
	Prod. status:	Nedlagt	Tippvolum:

Betydning

Historisk:

Ja , (Stadfestet 17.sep.2004 av Leif Furuhaug)

Opplysning(er) i fritekstformat

Beliggenhet

Dette bruddet ligger noe høyere opp i lia enn de andre Kjøsterud-bruddene. Like ved lysløype.

Bilde(r) fra forekomstområdet:

Foto nr. 1 viser "Bruddet"

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.

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