See inside a rock that was formed over One Million Years Ago

Split a Geode

In the past to open a Geode you had to use a really big hammer.

The Captains crew has a new easy way to use Geode Splitter than almost any age can use.

We offer Choyas and Trancas Geodes

Split a Geode for as low as $5.99 Small Trancas Geode up to $24.99 Large 4" Choyas Geode

Trancas: Come from Chihuahua Mexico. They range from 2 to 4 inches in diameter. These geodes are guaranteed to be 95 % hollow and are great for cracking with a geode cracker shown above. They tend to have a few different types of crystals inside making it a surprise every time you open one.

Las Choyas: Las Choyas geodes, also known as the Coconut Geodes, come from Chihuahua Mexico. They range from 2 to 6 inches in diameter. These geodes are guaranteed to be at least 95 % hollow and are great for cracking with a geode cracker shown above. They tend to have many different types of crystals inside (Clear Quartz, Smokey Quartz, and sometimes amethyst) making it a surprise every time you open one.

What is a Geode

A geode is a rock formation that combines minerals to form a hollowed-out rock with crystals lining the inside. It can take a long time for geodes to form. Some geodes that have been found are thousands to millions of years old. When a geode is split in half, the different layers can be seen, which will include the hollowed out center, crystal deposits and mineral deposits. If a geode is completely filled up with crystals leaving no hollowed space, it is called a nodule.

 

Geodes are made or formed by starting out in a hollow bubble inside a rock layer. Geodes formed from volcanic rock give us the best idea of of how a geode is made. Volcanic rock is formed from molten lava that cools and sets. When an air bubble appears, like those in pumice rocks, and slowly gets covered by more volcanic rock, the opportunity for a geode to form presents itself. This all happens while the air bubble is hot. When rain pelts down onto the outer layer of the rock, chemicals from the rock are released into the water. The water gets absorbed and passed through the hard, rocky outside layer of the bubble and then gets trapped on the inside of the bubble. This lasts for only a moment to a few seconds, long enough for the mineral-rich water to have small particles cling to the inside of the air bubble. Over time these particles turn into crystals from water constantly moving through the bubble and the water depositing more and more minerals to the inside of the hollow air bubble. Crystals of varying shapes and sizes appear depending on how long the geode has been forming and by how the water was moving through the air bubble.

Why are Geodes different colors

Not all geodes are the same because of the different types of rocks that help them to form. The chemicals that the rocks release into the water that passes through the air bubbles is full of minerals. Different minerals that cling to the inside of the air bubble cause the different colors of crystal forming the geode. Most geodes have quartz or calcite that forms the interior because 90 percent of the Earth's crust is covered with silicates, which is exactly what quartz crystal is. Mix in some carbon and oxygen from the water passing through the air bubble and you have calcite. Colors appear when other minerals get mixed into the composition. Magnesium, iron and copper in a minute traces can change the colors in the crystals and also change the color variations in the crystal depending on whether they are mixed in with the quartz or with the calcite or both. Heat also plays a part in the colors that appear in a geode.