Lennilenapeite is a rare phyllosilicate mineral typically found in the famous metamorphosed ore deposits of Franklin and Sterling Hill, New Jersey. It appears as brown to greenish-brown micaceous flakes or platy masses that are visually similar to stilpnomelane but distinguishable by its specific chemical composition and crystallography.

Hardness
~3
Mohs
Luster
Vitreous to resinous
Streak
Brown
Transparency
Translucent

Is this lennilenapeite?

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 lennilenapeite with a known reference. Lennilenapeite sits at Mohs ~3, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: brown.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous to resinous.
  • 4
    Match the color range
    Compare against the expected color range: brownish black, green, light green, dark brown.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: aggregates, platy.

Often confused with

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

Often found alongside lennilenapeite

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

All properties

Chemical formula
K₄Mn₄₈[Si₆₄Al₈]O₁₆₄(OH)₅₂·nH₂O
Mohs hardness
~3
Density
2.72 g/cm³
Streak
Brown
Luster
Vitreous to resinous
Transparency
Translucent
Crystal system
Triclinic
Crystal habit
Aggregates, platy
Cleavage
Perfect on {001}, imperfect on fhk0g
Rarity
Rare
Uses
Collector, Scientific research
Host rock
Apparently as both a primary and a late-stage low-temperature hydrothermal mineral in a metamorphosed stratiform zinc deposit

Where rockhounds find lennilenapeite

Classic worldwide localities

  • Franklin, Sussex Co., New Jersey, USA

Field-hunting tip

Where it forms: Apparently as both a primary and a late-stage low-temperature hydrothermal mineral in a metamorphosed stratiform zinc deposit. If you start seeing nelenite, tirodite, franklinite in float, you are in the right ground. Typical habit: aggregates, platy. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify lennilenapeite?+
Mohs hardness is ~3. Luster: vitreous to resinous. The streak is brown. Common colors include brownish black, green, light green, dark brown.
Where is lennilenapeite found?+
Notable localities include Franklin, Sussex Co., New Jersey, USA.
What rocks look like lennilenapeite?+
Lennilenapeite is most often confused with Stilpnomelane, Biotite, Phlogopite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with lennilenapeite?+
Lennilenapeite commonly co-occurs with Nelenite, Tirodite, Franklinite, Willemite, Sphalerite, Dolomite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does lennilenapeite form in?+
Where it forms: Apparently as both a primary and a late-stage low-temperature hydrothermal mineral in a metamorphosed stratiform zinc deposit. Working float back to the host body is the standard way to chase a fresh occurrence.
What is lennilenapeite used for?+
Lennilenapeite is used in collector, scientific research.

Find lennilenapeite on the map

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