Norsk versjon
	THE ORE DATABASE
	Deposit Area 2021 - 015
	(Last updated 15.feb.2005)

Importance

Public:

Little Importance (reg. 18.02.2015)

Economical:

Minor interest , (Confirmed 07.feb.2005 by Peter Ihlen)

Mineralization

	Era:	Cenozoic	Period:	Quarternary
	Dating:		Method:
	Genesis:	Clastic sediment	Form:	Irregular
	Main texture:	Pore space filling	Min. distribution:	Irregular (scattered)

Main grain size:

Very unevenly grained

Main alteration:

	Strike/Dip:		Direction:
			Plunge:

Stratigraphic classification of host rock

Era:

Period:

	Province:
	Geotec.unit:
	Tectonic complex:
	Igneous complex:

Group:

Formation:

Mineralogy

	Relationship	Mineral	Amount
	Gangue mineral	Amphibole	Major mineral (>10%)
	Gangue mineral	Garnet	Subordinate mineral (1-10%)
	Gangue mineral	Zircon	Subordinate mineral (1-10%)
	Ore mineral	Hematite	Major mineral (>10%)
	Ore mineral	Titanomagnetite	Major mineral (>10%)
	Ore mineral	Pyrite	Major mineral (>10%)
	Ore mineral	Scheelite	Accessory mineral (<1%)
	Ore mineral	Rutile	Accessory mineral (<1%)
	Ore mineral	Gold	Accessory mineral (<1%)
	Ore mineral	Sperrylite	Accessory mineral (<1%)
	Ore mineral	Silver	Accessory mineral (<1%)

Information(s) in free text format

Abstract

The deposit is situated near the southeastern bank of Karasjohka river about 500 m southwest of the old cabin at Gål'lebai'ke. Several pits have been developed in the Quarternery deposits around the cabin and southwestwards for about 600 m. The deposits are less than 0.5-1.5 m thick in areas where the bedrocks are reached (Bjørlykke 1966). The terrace consists of a top layer of alluvial sand rich in gold followed downwards by a 0.5-0.6 m thick unit of sand and gravel with large boulders nearly barren in gold. The best gold concentrations occur at the interface with the underlying undisturbed clay-rich blocky till. Strong gold enrichment is also encountered in the bottom of small depressions in the underlying bedrocks where the reworked unit of till is deposited directly on the bedrocks. The gold-rich top layer is assumed formed by alluvial redistibution of gold from the interface between reworked and undisturbed till. In 1966 about 5 kg of gold have been produced from the terrace which is estimated to contain 0.8-0.9 g gold per m3 of sand (Bjørlykke 1966).

Bibliography:

From NGU's Reference Archive:

Bjørlykke, Harald , 1966

	De alluviale gullforekomster i indre Finnmark.

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.236;1-66 pages

Abstract:

The first find of alluvial gold in Finnmarken was made by inspector (bergmester) Tellef Dahll in 1866 in sand from a small river named Nitusjokka near Karasjok. During the following 5 years gold deposits were found in all the rivers of the Tana river systm and the Alta and Reisa rivers. Gold has been found in small amount in all kinds of sand- and gravel deposits and also in the unwashed moraine deposits. The gold fields which have been subject to production or prospection work are situated at the upper parts of the rivers. The occurrences of alluvial gold in Finnmark may be classified in The following way: 1. Preglacial accumulations undisturbed by ice erosion during the ice age. 2: Preglacial accumulations disturbed and redeposited in moraines and fluvioglacial deposits. 3. Accumulations in postglacial river beds. The gold in these deposits seems chiefly to have been washed out from the moraines. Mineralogical analyses of the mineral composition of the gold-bearing sand and gravel have been carried out. The minerals of the gold-bearing deposits may be divided in two groups: 1. Minerals belonging to the surrounding solid rock. 2. Minerals which do not seem to belong to the solid rock in the neighbourhood of the deposits.

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The fact sheet was created on 24.11.2024

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