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Humite Mineral Overview

  • Mineral name: Humite
  • Mineral class: Silicate (nesosilicate, humite group)
  • Chemical formula: (Mg,Fe)₇(SiO₄)₃(F,OH)₂
  • Crystal system: Orthorhombic
  • Mohs hardness: 6–6.5
  • Color range: Yellow, orange, brown, reddish
  • Luster: Vitreous
  • Streak: White
  • Cleavage: Poor
  • Fracture: Uneven to subconchoidal
  • Specific gravity: Approximately 3.2–3.4
  • Transparency: Transparent to translucent
  • Common locations: Italy, Russia, United States, Norway
  • Uses: Collector mineral, rare gemstone
  • Similar minerals: Olivine, chondrodite, clinohumite

Naming and Classification

Humite is a magnesium-rich silicate mineral and the namesake of the humite group, which includes:

  • Chondrodite
  • Clinohumite
  • Norbergite

It was named after Sir Abraham Hume, an English mineralogist and collector.

Physical and Optical Characteristics

Humite typically occurs as:

  • Short prismatic or granular crystals
  • Massive aggregates

Its color is usually warm-toned, including:

  • Yellow
  • Orange
  • Brown
  • Reddish hues

The luster is vitreous, giving it a glassy appearance.

With a Mohs hardness of 6–6.5, it is moderately hard.

Crystal Habit (Key Feature)

Humite crystals are often:

  • Stubby, prismatic, or granular

They may resemble:

  • Olivine crystals but typically show more variation in color

Chemical Composition and Structure

Humite is composed of:

  • Magnesium (Mg) and iron (Fe)
  • Silicon (Si)
  • Oxygen (O)
  • Fluorine (F) and hydroxyl (OH)

It has a nesosilicate structure, similar to olivine, but modified by:

  • The presence of fluorine and hydroxyl

Formation and Geological Occurrence

Humite forms in metamorphosed carbonate rocks, particularly:

Contact Metamorphism

  • Limestone or dolomite altered by nearby magma

Typical formation conditions include:

  • High temperatures
  • Magnesium-rich environments
  • Presence of fluorine-bearing fluids

It is commonly associated with:

  • Calcite
  • Dolomite
  • Spinel
  • Forsterite

Common Locations

Humite is found in several classic localities:

  • Italy: Vesuvius region (type locality)
  • Russia: Ural Mountains
  • United States: New Jersey, New York
  • Norway: Metamorphic deposits

Italian specimens are especially well known.

Uses and Practical Significance

Humite has limited practical use:

Collector Mineral

  • Attractive color and rarity
  • Interest within the humite group

Gemstone Use

  • Occasionally faceted
  • Rare due to limited availability

Similar and Related Minerals

Humite can resemble:

  • Olivine: More common and typically greener
  • Chondrodite: Closely related but more common
  • Clinohumite: Similar but monoclinic

Careful identification may require crystallographic or chemical analysis.

Identification Notes for Collectors

  • Look for yellow to brown prismatic or granular crystals
  • Note moderate hardness (6–6.5)
  • Observe vitreous luster
  • Check association with metamorphosed carbonate rocks
  • Consider presence of fluorine-bearing minerals

Humite is a magnesium-rich nesosilicate mineral, recognized for its association with metamorphosed carbonate rocks and its role within the humite group, making it a distinctive and collectible mineral.

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