Biphosphammite is a rare, water-soluble ammonium phosphate mineral typically found as white crusts or efflorescences in guano deposits. It is extremely fragile and hygroscopic, often requiring airtight storage to prevent dissolution by atmospheric moisture.

Hardness
1-2
Mohs
Luster
Dull, earthy; crystals rarely vitreous
Streak
White to pale buff
Transparency
Semitransparent

Is this biphosphammite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch biphosphammite with a known reference. Biphosphammite sits at Mohs 1-2, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white to pale buff.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: dull, earthy; crystals rarely vitreous.
  • 4
    Match the color range
    Compare against the expected color range: brown, colorless, gray white.
  • 5
    Look at form & habit
    Crystal system: tetragonal. Typical habit: crusts, efflorescent coatings.

Often confused with

Biphosphammite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside biphosphammite

Minerals reported to co-occur with biphosphammite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
(NH₄)(H₂PO₄)
Mohs hardness
1-2
Density
2.04 g/cm³
Streak
White to pale buff
Luster
Dull, earthy; crystals rarely vitreous
Transparency
Semitransparent
Crystal system
Tetragonal
Crystal habit
Crusts, efflorescent coatings
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
An alteration product of phosphammite in guano, due to loss of NH4 (Guañape Island, Peru); a byproduct of the reaction between the liquid fraction of bat guano and urea (Murra-el-elevyn Cave, Australia)

Where rockhounds find biphosphammite

Classic worldwide localities

  • Guañape Island, south of Trujillo, Peru
  • Murra-el-elevyn Cave, Cocklebiddy, and in Petrogale Cave, near Madura, Western Australia
  • Gcwihaba Cave, 280 km west of Maun, northwestern Botswana

Field-hunting tip

Where it forms: An alteration product of phosphammite in guano, due to loss of NH4 (Guañape Island, Peru); a byproduct of the reaction between the liquid fraction of bat guano and urea (Murra-el-elevyn Cave, Australia). If you start seeing phosphammite, syngenite in float, you are in the right ground. Typical habit: crusts, efflorescent coatings. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify biphosphammite?+
Mohs hardness is 1-2. Luster: dull, earthy; crystals rarely vitreous. The streak is white to pale buff. Common colors include brown, colorless, gray white.
Where is biphosphammite found?+
Notable localities include Guañape Island, south of Trujillo, Peru; Murra-el-elevyn Cave, Cocklebiddy, and in Petrogale Cave, near Madura, Western Australia; Gcwihaba Cave, 280 km west of Maun, northwestern Botswana.
What rocks look like biphosphammite?+
Biphosphammite is most often confused with Mascagnite, Struvite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with biphosphammite?+
Biphosphammite commonly co-occurs with Phosphammite, Syngenite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does biphosphammite form in?+
Where it forms: An alteration product of phosphammite in guano, due to loss of NH4 (Guañape Island, Peru); a byproduct of the reaction between the liquid fraction of bat guano and urea (Murra-el-elevyn Cave, Australia). Working float back to the host body is the standard way to chase a fresh occurrence.
What is biphosphammite used for?+
Biphosphammite is used in collector.

Find biphosphammite on the map

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