Amygdule
± 1971. Found: Gomera, Spain (JN0690-3)
Filled Cavities with Minerals in Igneous Rock
Chemical Formula: Variable
Crystal System: Variable
Crystal Habit: Variable
Mohs Scale: Variable
Tenacity: Variable
Fracture: Variable
Color: Usually white
Streak: Usually white
Luster: Pearly or waxy
Diaphaneity: Transparent to translucent
Amygdule: A Hidden Treasure Within Volcanic Rocks
Imagine a world where molten rock erupts from the Earth's depths, spewing fiery lava and creating a breathtaking spectacle of nature's power. As the lava cools and hardens, it leaves behind tiny pockets of air called vesicles. Over time, these vesicles can become filled with beautiful minerals, transforming into hidden treasures known as amygdules. In this article, we'll dive into the world of amygdules, exploring their definition, history, and the fascinating process of their formation.
What in the World is an Amygdule?
You know how some pancakes or bread have little holes in them? Rocks can have something similar. If you find an igneous rock (which is a rock formed from molten material like lava or magma) and see an oval or almond-shaped blob in it, you might be looking at an amygdule (pronounced uh-MIG-dyool). These fascinating features tell us a story about how the rock formed.
Let's break down the word
The word "amygdule" comes from the Greek word "amygdalē" which means "almond." You can see why – amygdules are often almond-shaped!
Bubbles, Blobs, and Minerals
Here's a quick science lesson explaining how amygdules form:
Volcanic Bubbles: When hot lava or magma erupts from a volcano, it often contains dissolved gases, just like a fizzy soda. As the lava cools, these gases escape, leaving behind tiny, round holes called vesicles.
Mineral Filling: Over time, groundwater seeps through the porous rock. This water carries dissolved minerals. When these mineral-rich waters reach the vesicles (those little holes), the minerals start to crystallize and grow within the empty spaces.
Amygdule Creation: Eventually, the minerals completely fill the vesicle, forming a solid structure – the amygdule.
What Do Amygdules Look Like?
Amygdules come in many colors and patterns depending on the minerals that fill them. Here are some common ones:
Quartz and Chalcedony: This creates a whitish or pale-colored amygdule. Chalcedony (kal-SED-uh-nee) is a type of quartz but has much smaller crystals that you can't see with your eyes.
Zeolites: These are a family of minerals with amazing crystal structures, often making amygdules that look fluffy or sparkly.
Calcite: A common mineral that makes whitish or transparent amygdules.
Chlorite: This gives amygdules a greenish color.
Sometimes you can find amygdules that have colorful, layered rings. Think of how tree rings look – the different layers come from different mineral deposits happening over a long period.
A Geologist's Treasure
Amygdules aren't just pretty to look at; they give geologists interesting information:
Volcanic History: Amygdules are common in volcanic rocks, so finding them helps geologists recognize ancient lava flows or volcanic eruptions.
Ancient Water: The minerals inside an amygdule can give clues about the type of water that flowed through the rock in the past and the temperatures they formed at.
Rock Types: Sometimes the shape and size of amygdules help geologists identify different types of volcanic rocks.
A Brief History of Amygdules
Geologists have been studying amygdules for centuries. Here are a few highlights:
Ancient Times: Amygdales were sometimes described in ancient mineralogy texts, although people didn't understand their formation back then.
18th Century: Scientific descriptions of amygdules and their connection to volcanic rocks started to appear.
19th Century: Geologists like Joseph LeConte made detailed studies of amygdules and how the minerals inside form.
Today (2022): Modern geologists use advanced methods to analyze the minerals in amygdules, unlocking even more secrets about Earth's history.
Where to Find Amygdules
If you want to see amygdules for yourself, the best places to look are areas with a history of volcanic activity. Rocks like basalt, which is common in lava flows, will often have these cool features. Gem and mineral shows or rock shops might also have samples available.
The Takeaway
Amygdules are more than just pretty spots in rocks. They're little capsules of geological history, telling us about ancient volcanoes and the hidden movement of water through the Earth. Next time you see an almond-shaped blob in a rock, remember, it's a tiny reminder of the amazing forces that shape our planet!