Green hornblende is a common rock-forming amphibole found in a wide variety of igneous and metamorphic environments. It is characterized by its distinct dark green to black-green color and its tendency to form elongated, prismatic crystals with characteristic 56 and 124-degree cleavage angles.
Is this green hornblende?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch green hornblende with a known reference. Green Hornblende sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white to pale gray.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to pearly.
- 4Match the color rangeCompare against the expected color range: dark green, blackish green, brownish green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, elongated, bladed, massive.
Often confused with
Green Hornblende vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Streak differs, so Green Hornblende leaves white to pale gray, Augite leaves gray-green.

How to tell apart: Streak differs, so Green Hornblende leaves white to pale gray, Arfvedsonite leaves deep bluish gray, gray-green.
Often found alongside green hornblende
Minerals reported to co-occur with green hornblende. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Na)₂₋₃(Mg,Fe,Al)₅Si₆(Si,Al)₂O₂₂(OH,F)₂
- Mohs hardness
- 5-6
- Density
- 3.0-3.4 g/cm³
- Streak
- White to pale gray
- Luster
- Vitreous to pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, elongated, bladed, massive
- Cleavage
- Perfect in two directions at 56 and 124 degrees
- Rarity
- Common
- Uses
- Collector, Geological indicator
- Host rock
- igneous and metamorphic rocks
Where rockhounds find green hornblende
1 mapped spotsClassic worldwide localities
- Ontario, Canada
- New York, USA
- Norway
- Finland
- Italy
Field-hunting tip
Where it forms: igneous and metamorphic rocks. If you start seeing quartz, plagioclase, biotite in float, you are in the right ground. Typical habit: prismatic crystals, elongated, bladed, massive. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in South Carolina. Start trip planning there.




