Norsk versjon
THE NATURAL STONE DATABASE
Deposit Area 301 - 618
(Last updated 20.feb.2026)

Name of Deposit Area : Sognsvann nord
(Object Id : 0301,618,00,00)

Location
County : Oslo (03) Municipality : Oslo (0301)
Map 1:50000: Oslo (1914-4) Map 1:250000: Oslo
Marking point: Longitude: 10.7293740 Latitude: 59.9839060
EU89-UTM Zone 32 (Coordinates IS confirmed)
X-coord: 596500 m. Y-coord: 6650880 m.

Commodity
Main Type: Granite and other igneous rocks Sub Type: Syenite
Brickstone(Y/N):

Importance
Public: (No data)
Economical: Not classified/evaluated

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:

Information(s) in free text format
Description
Bruddområdet ligger nord for Sognsvann og er ganske langt, mer eller mindre sammenhengende over ca. 150 m. Det følger en åsrygg som er vekslende blottet og har < 1 m avsenkning.

Photo(s) from the Deposit area:
Photo no. 1 showing Område"

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 17.03.2026

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