amphibolite
C2Pronunciation
UK
- /æmfˈɪbəlˌaɪt/
US
- /æmfˈɪbəlˌaɪt/
Description
- dark-colored metamorphic rock
- mainly amphibole (hornblende) + plagioclase
- formed under intense heat and pressure
- often speckled or banded
Imagine rocks getting squeezed and cooked deep underground – that's how amphibolites are born! They are a type of metamorphic rock, meaning they started as something else (usually basalt or gabbro) and were transformed by intense heat and pressure. Amphibolites are usually dark-colored, often with striking black or dark-green minerals like hornblende, giving them a speckled or slightly banded appearance. You might find these rocks in mountain ranges where tectonic plates have collided, telling a story of ancient geological forces.
While not as famous as marble for statues, amphibolite is a tough rock often used in the construction industry as crushed stone for roads or as facing stone on buildings. However, geologists value it for a different reason: they study amphibolites to understand the history of Earth's crust. Think of them as time capsules holding clues about our planet's past! The name comes from the Greek word "amphibolos" meaning "doubtful," because the minerals inside were originally difficult for scientists to classify.
Amphibolite is a medium-to-coarse-grained metamorphic rock formed when pre-existing mafic igneous rocks (like basalt or gabbro) are subjected to high temperatures and pressures deep within the Earth's crust. It's not just any heated rock, though – amphibolites form under specific conditions (often called amphibolite-facies metamorphism) that favor the growth of amphibole minerals alongside plagioclase feldspar. These minerals, primarily hornblende, give the rock its characteristic dark green or black coloration, often contrasted against lighter feldspar.
You'll typically find amphibolite in regions that have experienced regional metamorphism, meaning large-scale changes due to tectonic activity. Think of places where continents collide – the Alps, Appalachians, and Himalayas are all likely spots to discover these rocks. They often appear as elongated bands or lenses within other metamorphic formations, marking the zones where the Earth was under significant stress.
While frequently used as construction aggregate (road metal) or marketed as "black granite" for countertops, amphibolites are also incredibly valuable to science. By studying their mineral composition and texture, scientists can reconstruct the temperature and pressure conditions under which they formed. This reveals details about ancient plate movements, mountain-building events, and the overall evolution of Earth's crust.
The name "amphibolite" has a bit of a history itself! It is derived from the mineral group "amphibole," which comes from the Greek word "amphibolos," meaning "doubtful" or "ambiguous." Early mineralogists gave the minerals this name because they were so variable in composition and appearance that they were difficult to categorize. So, next time you see a dark, hard rock with green flecks, remember it might be an amphibolite – a silent witness to Earth's dramatic past!
Examples
- 1
Trail geology
The trail cuts through a ridge of amphibolite near the lake.
Domain
amphibolite
a dark rock name used mainly in geology
- 2
Rock layers
Geologists found thin layers of quartz running through the amphibolite.
- 3
Rock formation
The report says the local amphibolite formed under high pressure and heat.
Forms and spellings
1 form open this card.
Main spelling
- amphibolitenoun