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Where is Gabbro found?

Gabbro

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Gabbro occurs in specific geological environments. Knowing where to look, and in what kind of rock, is the difference between going home empty-handed and finding a great specimen.

Where to find Gabbro

Oceanic Crust

Gabbro is a major constituent of the lower oceanic crust, forming beneath mid-ocean ridges. It can be found exposed in ophiolite complexes, which are fragments of oceanic crust and upper mantle thrust onto continental margins (e.g., Oman, Cyprus, Newfoundland).

Layered Intrusions

Large, economically significant layered mafic intrusions worldwide contain vast quantities of gabbro. Examples include the Bushveld Complex (South Africa), Stillwater Complex (USA), and Skaergaard Intrusion (Greenland).

Continental Rifts and Hotspots

Gabbroic intrusions are associated with continental rifting environments and large igneous provinces (LIPs) formed by mantle plumes (e.g., Duluth Complex, USA; Siberian Traps, Russia).

Mountain Ranges

Gabbro can be found in eroded mountain ranges where deep-seated igneous intrusions have been uplifted and exposed (e.g., parts of the Appalachian Mountains, USA; Scottish Highlands, UK).

Collecting tips

  1. Look for Dark, Coarse-Grained Rocks. Gabbro is distinctly dark and its individual mineral grains are visible without magnification. This distinguishes it from fine-grained basalt.
  2. Check for Mineral Composition. Identify the presence of dark pyroxene and lighter, often iridescent, plagioclase feldspar. A hand lens can be very useful for this.
  3. Consider the Geological Context. Gabbro is typically found in areas associated with ancient oceanic crust (ophiolites), large intrusive complexes, or areas of significant mafic magmatism.
  4. Examine Weathered Surfaces. While fresh gabbro is dark, weathered surfaces can sometimes appear brownish or greenish due to alteration of mafic minerals.

Quick Check

Color:
Dark (black, dark green, dark gray)
Luster:
Vitreous to dull
Streak:
White to very light gray (from plagioclase), or no streak (from mafic minerals)

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