Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Fourth Beach Occurrence, Nome Mining District, Nome Census Area, Alaska, USAi
Regional Level Types
Fourth Beach OccurrenceOccurrence
Nome Mining DistrictMining District
Nome Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
64° 33' 2'' North , 165° 23' 9'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Nome3,806 (2018)5.6km
Mindat Locality ID:
197532
Long-form identifier:
mindat:1:2:197532:4
GUID (UUID V4):
0


Considered too low grade to be of economic interest.
Location: Fourth Beach is the highest elevation auriferous strandline now known on the Nome coastal plain (Hopkins and others, 1960; Nelson and Hopkins, 1972; Tagg and Greene, 1973; Cobb, 1973 [B 1374, figure 29, p. 87]). The elevation of the Fourth Beach strandline is 125 feet. It is preserved at the base of Anvil Mountain, where it is buried by colluvium. The map location is about on Cooper Gulch at a surface elevation of 250 feet. It is in the west-central part of section 12, T. 11 S., R. 34 W., Kateel River Meridian. The location is accurate within about 500 feet.
Geology: Fourth Beach represents the farthest advance of the sea in Quaternary time, and it has been recognized only at the base of Anvil Mountain. It formed as a true strandline beach by waves impinging upon bedrock. Unlike Third Beach, which terminates landward on a prominent scarp marked by long-continued erosion at that sea level, Fourth Beach is an inconspicuous strandline that evidently formed during a relatively short seastand. It is not generally rich enough to mine. Probably some of the gold that was concentrated at Fourth Beach sea level was eroded seaward before the beach was buried by mass-wasting deposits. Hopkins and others (1960, p. 47-48) noted that the sediments of Fourth Beach are overlain by drift of the Nome River glaciation and that the seaward edge of the deposits is truncated at the Third Beach escarpment. They postulated that Fourth Beach may have formed during some part of Submarine Beach time or during an otherwise unidentified interglacial interval. Nelson and Hopkins (1972) diagrammatically show Fourth Beach at the base of Anvil Mountain (also see Cobb, 1973 [B 1374, figure 29]).
Workings: There is no substantial production from Fourth Beach. Gold originally concentrated on this beach could have been eroded and reconcentrated in alluvial deposits below the beach.
Age: Pleistocene.

Commodities (Major) - Au
Development Status: None
Deposit Model: Placer Au; buried, strandline beach deposit (Cox and Singer, 1986; model 39a).

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


1 valid mineral.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Gold1.AA.05Au
Unclassified
'Garnet Group'-X3Z2(SiO4)3

List of minerals for each chemical element

OOxygen
O Garnet GroupX3Z2(SiO4)3
SiSilicon
Si Garnet GroupX3Z2(SiO4)3
AuGold
Au GoldAu

Other Databases

Link to USGS - Alaska:NM259

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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