Calciodelrioite is a rare secondary vanadium mineral that typically forms thin, colorless to tan, platy crystal crusts or coatings. It is most commonly found as an efflorescence in the oxidized zones of uranium-vanadium mines in the Colorado Plateau, often associated with other vanadium-rich minerals.

Hardness
2.5
Mohs
Luster
Subadamantine (crystals), silky (aggregates)
Streak
White
Transparency
Transparent

Is this calciodelrioite?

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 calciodelrioite with a known reference. Calciodelrioite sits at Mohs 2.5, 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.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: subadamantine (crystals), silky (aggregates).
  • 4
    Match the color range
    Compare against the expected color range: colorless, tan, reddish brown, brown.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: platy crystals.

Often confused with

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

Often found alongside calciodelrioite

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

All properties

Chemical formula
Ca(VO₃)₂·4H₂O
Mohs hardness
2.5
Density
2.451-2.503 g/cm³
Streak
White
Luster
Subadamantine (crystals), silky (aggregates)
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
Platy crystals
Cleavage
Perfect on {001}, others possible parallel [100]
Rarity
Rare
Uses
Collector
Host rock
A secondary mineral as crystalline crusts on fracture surfaces in the oxidized portions of corvusite- and montroseite-impregnated sandstone

Where rockhounds find calciodelrioite

Classic worldwide localities

  • Uravan Mineral Belt, Colorado, USA
  • La Sal District, Utah, USA

Field-hunting tip

Where it forms: A secondary mineral as crystalline crusts on fracture surfaces in the oxidized portions of corvusite- and montroseite-impregnated sandstone. If you start seeing gypsum, rossite, metarossite in float, you are in the right ground. Typical habit: platy crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify calciodelrioite?+
Mohs hardness is 2.5. Luster: subadamantine (crystals), silky (aggregates). The streak is white. Common colors include colorless, tan, reddish brown, brown.
Where is calciodelrioite found?+
Notable localities include Uravan Mineral Belt, Colorado, USA; La Sal District, Utah, USA.
Is calciodelrioite safe to handle?+
Calciodelrioite contains vanadium. Contains vanadium, which is toxic if ingested or inhaled as dust. Wash hands thoroughly after handling and avoid creating dust when breaking specimens.
What rocks look like calciodelrioite?+
Calciodelrioite is most often confused with Pascoite, Hewettite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with calciodelrioite?+
Calciodelrioite commonly co-occurs with Gypsum, Rossite, Metarossite, Celestine, Huemulite, Pascoite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does calciodelrioite form in?+
Where it forms: A secondary mineral as crystalline crusts on fracture surfaces in the oxidized portions of corvusite- and montroseite-impregnated sandstone. Working float back to the host body is the standard way to chase a fresh occurrence.
What is calciodelrioite used for?+
Calciodelrioite is used in collector.

Find calciodelrioite on the map

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