Kalinite is a potassium aluminum sulfate mineral that typically forms as a powdery, efflorescent crust or fibrous mass in mining environments or volcanic fumaroles. It is highly water-soluble and delicate, often requiring dry storage conditions to prevent degradation or dissolution.

Hardness
2-2.5
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent to translucent

Is this kalinite?

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 kalinite with a known reference. Kalinite sits at Mohs 2-2.5, 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: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: white, colorless.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: fibrous, water soluble.

Often confused with

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

Often found alongside kalinite

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

All properties

Chemical formula
KAl(SO₄)₂·11H₂O
Mohs hardness
2-2.5
Density
1.75 g/cm³
Streak
White
Luster
Vitreous
Transparency
Transparent to translucent
Crystal system
Monoclinic
Crystal habit
Fibrous, water soluble
Cleavage
None
Rarity
Uncommon
Uses
Collector
Host rock
A rare secondary mineral observed in the oxidized zone of mineral deposits, as efflorescences on alum slates, in caves, and as a volcanic sublimate

Where rockhounds find kalinite

Classic worldwide localities

  • Turkey Creek, Jefferson Co., Colorado, USA
  • Alum mine, Silver Peak district, Esmeralda Co., Nevada, USA
  • Alma pyrite mine, Alameda Co., California, USA
  • Mount Wingen, New South Wales, Australia
  • Quetena, west of Calama, Antofagasta, Chile
  • Found on volcanoes in the Lipari Islands and Sicily, Italy, and on the Kamchatka Peninsula, Russia

Field-hunting tip

Where it forms: A rare secondary mineral observed in the oxidized zone of mineral deposits, as efflorescences on alum slates, in caves, and as a volcanic sublimate. If you start seeing jarosite, pisanite in float, you are in the right ground. Typical habit: fibrous, water soluble. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify kalinite?+
Mohs hardness is 2-2.5. Luster: vitreous. The streak is white. Common colors include white, colorless.
Where is kalinite found?+
Notable localities include Turkey Creek, Jefferson Co., Colorado, USA; Alum mine, Silver Peak district, Esmeralda Co., Nevada, USA; Alma pyrite mine, Alameda Co., California, USA; Mount Wingen, New South Wales, Australia; Quetena, west of Calama, Antofagasta, Chile.
What rocks look like kalinite?+
Kalinite is most often confused with Tschermigite, Alunogen. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with kalinite?+
Kalinite commonly co-occurs with Jarosite, Pisanite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does kalinite form in?+
Where it forms: A rare secondary mineral observed in the oxidized zone of mineral deposits, as efflorescences on alum slates, in caves, and as a volcanic sublimate. Working float back to the host body is the standard way to chase a fresh occurrence.
What is kalinite used for?+
Kalinite is used in collector.

Find kalinite on the map

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