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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Rock

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About RockHide

A rock is a naturally-occurring solid aggregate of one or more minerals, mineraloids or, in some cases, organic material. Sediments are the unconsolidated equivalent of these. Other related materials, including some man-made materials, are included within this categorization, along with the major classifications for meteorites.

Strictly, any naturally formed aggregate or mass of mineral matter, whether or not coherent, constituting an essential and appreciable part of the Earth's crust. Ordinarily, a consolidated or coherent and relatively hard, naturally formed mass of mineral matter; stone. In instances, a single mineral forms a rock, such as calcite, serpentine, kaolin, and a few others, but the vast majority of rocks consist of several minerals. It can include glasses and mineraloids eg. obsidian, or solid organic material, e.g., coal.

Reference: American Geosciences Institute


Unique IdentifiersHide

Mindat ID:
50468
Long-form identifier:
mindat:1:1:50468:1

Similar NamesHide

RikkiA synonym of Native Sulphur

Sub-divisions of RockHide

Pronunciation of RockHide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Age distributionHide

Recorded ages:
Neoarchean to Quaternary : 2580 ± 200 Ma to 0 Ma - based on 106 recorded ages.
Sample ages:
Sample IDRecorded ageGeologic TimeDating method
10.082 ± 0.3 to 0.065 ± 0.1 MaPleistoceneK-Ar
21.1 MaPleistoceneK-Ar
32.6 to 1.8 MaCenozoic
45.332 to 2.588 MaCenozoicgeological evidence
511.9 MaMioceneK-Ar
618.9 to 7.1 MaMioceneK-Ar whole rock
723.2 ± 1.0 to 22.1 ± 0.9 MaCenozoic
835 ± 1.60 MaEoceneK-Ar whole rock
958.4 ± 2.3 MaPaleoceneK-Ar
1070 ± 6 MaLate/Upper CretaceousK-Ar
11107 ± 4 MaEarly/Lower CretaceousK-Ar
12125 ± 4 MaEarly/Lower CretaceousK-Ar
13229 MaLate/Upper TriassicRb-Sr whole rock
14291 ± 6 MaCisuralian
15367.8 ± 4.7 to 362.8 ± 2.2 MaLate/Upper DevonianRb-Sr
16462 MaMiddle OrdovicianSm-Nd isochron
17893 MaTonian
181250 MaEctasianSHRIMP
191685 MaStatherianSm-Nd carbonatite whole rock sample
202580 ± 200 MaNeoarcheanU-Pb zircon
Sample references:
IDLocalityReferenceNotes
1Mount Etinde, Buea, Fako, Southwest Region, Cameroonnosean-leucite nephelinite
2  "  "
3Khanneshin complex, Reg District, Helmand, Afghanistan
4Mau Volcanic Area, Narok County, Kenya
5Tokatoka, Kaipara District, Northland Region, New Zealand
6West Qinling, Li County, Longnan, Gansu, China
7Fuerteventura, Las Palmas Province, Canary Islands, Spain
8Ozrem occurrence, Gornji Milanovac, Moravica District, Central Serbia, Serbia
9Orbey, Vosges Volcanic Field, Vosges, Grand Est, France
10Osečná Complex, Osečná, Liberec District, Liberec Region, Czech Republic
11Swangkre, West Khasi Hills District, Meghalaya, India
12Wadi Araba nephelinite occurrences, Suez Governorate, Egypt
13Datong Occurrence, Pingcheng District, Datong, Shanxi, ChinaBased on 2 whole rock samples, biotite and feldspar.
14Exeter Volcanic Series, Exeter, Devon, England, UK
15Sokli carbonatite complex, Tulppio, Savukoski, Lapland, Finland
16Pinghe, Nanjiang Co., Bazhong, Sichuan, China
17Central Yunnan Province, Yuanmou County, Chuxiong, Yunnan, ChinaRecrystallized (metamorphosed) carbonatitic lavas
18Lyons River Sills, Gifford Creek Complex, Mount Augustus area, Upper Gascoyne Shire, Western Australia, Australia
19Central Yunnan Province, Yuanmou County, Chuxiong, Yunnan, China
20Siilinjärvi Carbonatite Intrusion, Siilinjärvi, North Savo, Finland

Chemical AnalysisHide

Oxide wt%:
 123
SiO243.14 %39.75 %46.85 %
Al2O312.07 %15.11 %22.30 %
TiO23.11 %3.97 %0.30 %
Fe2O32.00 %2.00 %3.07 %
FeO10.97 %11.42 %2.21 %
MgO10.32 %6.45 %0.09 %
MnO0.17 %0.22 %0.13 %
Na2O2.93 %3.66 %15.76 %
CaO12.72 %13.17 %1.4 %
K2O0.95 %1.8 %3.58 %
P2O50.40 %1.19 %0.03 %
ZrO20.41 %
H2O1.46 %
Cl2.86 %
F0.29 %
CO30.16 %
Total:98.78 %98.74 %100.9 %
Sample references:
IDLocalityReferenceNotes
1Mont Royal, Montréal, Québec, CanadaWet chemical analysis by G. Woussen and B.M.Gunn. The Fe2O3 percentage is arbitrarily set to 2%.
2  "  "Wet chemical analysis by G. Woussen and B.M.Gunn. The Fe2O3 percentage is arbitrarily set to 2%.
3Ilímaussaq complex, Kujalleq, GreenlandAverage of 7 analyses of naujaite consisting of K‑feldspar/perthite (25.7 vol%), nepheline (9.9 vol%), pyroxenes (6.6 vol%), amphiboles (5.6 vol%), aenigmatite(1.7 vol%), eudialyte (4.9 vol%), sodalite (40.2 vol%), analcime (3.6 vol%), natrolite (1.7 vol%), fluorite (0.1 vol%), apatite (tr), opaques (tr). The analytical method not given, presumably wet chemical.

Internet Links for RockHide

References for RockHide

Reference List:
 
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