Phillipsite-K is a zeolite mineral known for its complex cruciform penetration twinning, often forming radiating 'x-shaped' crystal clusters. It is typically found in the vesicles of basaltic rocks and other volcanic environments where it forms through the alteration of glassy volcanic material.

Hardness
4-5
Mohs
Luster
Vitreous
Streak
White
Transparency
Translucent

Is this phillipsite-k?

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 phillipsite-k with a known reference. Phillipsite-K sits at Mohs 4-5 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Phillipsite-K leaves a white streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Phillipsite-K typically shows a vitreous luster.
  • 4
    Match the color range
    Compare against the expected color range: white, colorless, yellow, red, brown.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: cruciform penetration twins, radiating clusters, prismatic.

Often confused with

Phillipsite-K vs. its common look-alikes — and how to tell them apart in the field.

Often found alongside phillipsite-k

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

All properties

Chemical formula
(K,Na,Ca)₃₋₄(Si,Al)₁₆O₃₂·12H₂O
Mohs hardness
4-5
Density
2.2 g/cm³
Streak
White
Luster
Vitreous
Transparency
Translucent
Crystal system
Monoclinic
Crystal habit
Cruciform Penetration Twins, Radiating Clusters, Prismatic
Cleavage
Distinct On {010} and {110}
Rarity
Common
Uses
Collector
Host rock
Basaltic Volcanic Rocks, Cavities in Amygdaloidal Basalts
Typical price
$10-50 per specimen

Where rockhounds find phillipsite-k

Classic worldwide localities

  • Vesuvius, Italy
  • Giessen, Germany
  • Table Mountain, Colorado, USA
  • Giant's Causeway, Northern Ireland
  • Skye, Scotland

Field-hunting tip

Look in basaltic volcanic rocks, cavities in amygdaloidal basalts country — that is the host setting where phillipsite-k typically forms. If you start seeing calcite, analcime, natrolite in float, you are in the right ground. Field specimens usually show a cruciform penetration twins, radiating clusters, prismatic habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify phillipsite-k?+
Mohs hardness is 4-5. It typically shows a vitreous luster. The streak is white. Common colors include white, colorless, yellow, red.
Where is phillipsite-k found?+
Notable localities include Vesuvius, Italy; Giessen, Germany; Table Mountain, Colorado, USA; Giant's Causeway, Northern Ireland; Skye, Scotland.
How much is phillipsite-k worth?+
Typical asking prices fall in the range of $10-50 per specimen. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like phillipsite-k?+
Phillipsite-K is most often confused with Harmotome, Chabazite, Stilbite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with phillipsite-k?+
Phillipsite-K commonly co-occurs with Calcite, Analcime, Natrolite, Apophyllite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does phillipsite-k form in?+
Phillipsite-K typically forms in basaltic volcanic rocks, cavities in amygdaloidal basalts. Working float back to the host body is the standard way to chase a fresh occurrence.
What is phillipsite-k used for?+
Phillipsite-K is used in collector.

Find phillipsite-k on the map

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