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Yamhamelachite

A valid IMA mineral species
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Salty Edge of the Dead Sea

Dead Sea
Formula:
KCrP2O7
Colour:
green
Lustre:
Vitreous
Hardness:
4
Specific Gravity:
3.035 (Calculated)
Crystal System:
Monoclinic
Name:
Its name is derived from the Hebrew for the Dead Sea: Yam Ha-Melach (ים מלח, the Sea of Salt)
Known synthetic analogue. Unique combination of elements (at the upload time).

The first approved Cr diphosphate mineral.

Other diphosphate minerals (also known from the type-locality area) include anastasenkoite, lisanite, nabateaite, and shasuite.

Also compare pyrocoproite, pyrophosphite, arnhemite, canaphite, and wooldridgeite.

Other Cr-bearing phosphate minerals are embreyite and vauquelinite, but these are chromate-phosphates.

In a few cases V is marginally more abundant than Cr, indicating the presence of a potentially new mineral with the formula KVP2O7 (Galuskin et al., 2025).


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Unique IdentifiersHide

Mindat ID:
471049
Long-form identifier:
mindat:1:1:471049:9

IMA Classification of YamhamelachiteHide

Classification of YamhamelachiteHide

8.FA.20

8 : PHOSPHATES, ARSENATES, VANADATES
F : Polyphosphates, Polyarsenates, [4]-Polyvanadates
A : Polyphosphates, etc., without OH and H2O; dimers of corner-sharing RO4 tetrahedra.

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
YmmIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of YamhamelachiteHide

Vitreous
Transparency:
Transparent
Colour:
Green
Hardness:
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Conchoidal
Density:
3.035 g/cm3 (Calculated)

Chemistry of YamhamelachiteHide

Mindat Formula:
KCrP2O7
Element Weights:
Element% weight
O42.257 %
P23.373 %
Cr19.618 %
K14.752 %

Calculated from ideal end-member formula.
O
P
Cr
K

Crystallography of YamhamelachiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/c
Setting:
P21/c
Cell Parameters:
a = 7.3574(3) Å, b = 9.9336(4) Å, c = 8.1540(4) Å
β = 106.712(5)°
Ratio:
a:b:c = 0.741 : 1 : 0.821
Unit Cell V:
570.77 ų (Calculated from Unit Cell)
Z:
4

X-Ray Powder DiffractionHide

Type Occurrence of YamhamelachiteHide

General Appearance of Type Material:
aggregates in which the size of grains not exceeding 25-30 μm
Place of Conservation of Type Material:
Type material is deposited in the collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 115162, Russia, registration number 6074/1
Geological Setting of Type Material:
Small outcrop of phosphide-bearing breccia with cement composed of gehlenite-flamite paralava was discovered in the Hatrurim Basin, occurs at the phosphide-enriched boundary between an altered sedimentary xenolith and the gehlenite-flamite paralava.
Associated Minerals at Type Locality:

Other Language Names for YamhamelachiteHide

Related Minerals - Strunz-mindat GroupingHide

8.FA.Phosphocyclite-(Fe)Fe2+2(P4O12)Mon. 2/m : B2/b
8.FA.Phosphocyclite-(Ni)Ni2(P4O12)Mon. 2/m : B2/b
8.FA.GrahampearsoniteCa2P2O7Tet. 4 : P41
8.FA.BakakiniteCa2V2O7Tric. 1 : P1
8.FA.LisaniteCaNiP2O7Tric. 1 : P1
8.FA.ShasuiteCaNi3(P2O7)2Mon. 2/m : P21/c
8.FA.NabateaiteFe2P2O7Tric. 1 : P1
8.FA.SamraiteNi2P2O7Mon. 2/m : P21/c
8.FA.AnastasenkoiteCaFe2+(P2O7)Tric. 1 : P1
8.FA.05Blossiteα-Cu2(V2O7)Orth. mm2 : Fdd2
8.FA.10Ziesiteβ-Cu2(V2O7)Mon. 2/m : B2/b
8.FA.15'UM1999-17:O:PbV'Pb4V2O9 or Pb4(VO4)2O
8.FA.15ChervetitePb2(V2O7)Mon. 2/m : P21/c
8.FA.20'Pyrocoproite'(K,Na)2Mg(P2O7)Mon.
8.FA.20'Pyrophosphite'K2Ca(P2O7)Mon.
8.FA.25Petewilliamsite(Ni,Co)30(As2O7)15Mon. 2 : B2

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 0.0000% 0 α, β, γ
Thorium (Th) 0.0000% 0 α, β, γ
Potassium (K) 14.7520% 4,573 β, γ

For comparison:

  • Banana: ~15 Bq per fruit
  • Granite: 1,000–3,000 Bq/kg
  • EU exemption limit: 10,000 Bq/kg

Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.

Interactive Simulator:

Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!

Activity: –

DistanceDose rateRisk
1 cm
10 cm
1 m

The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

Other InformationHide

Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for YamhamelachiteHide

References for YamhamelachiteHide

Localities for YamhamelachiteHide

Showing 1 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Israel (TL)
 
  • Southern District
    • Beersheba Subdistrict
      • Tamar Regional Council
        • Hatrurim Basin
          • Wadi Zohar
Galuskin +1 other reference
 
and/or  
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