The Enchanted Rock
The Enchanted Rock
Located a few miles North of Fredericksburg, Texas, the Enchanted Rock is a popular destination for hikers, naturalists, spelunkers, and geologists alike. From the summit there are breathtaking views of the surrounding Hill Country. From Native Americans, to U.S. Cavalry, to tourists from New York, this geologic feature has been viewed by millions.
Satellite View of the Enchanted Rock
What is the Enchanted Rock?
In geologic terms the Enchanted Rock is a large igneous pluton. Igneous means this rock is a product of cooled magma. Pluton is the term given to a magma chamber that was never erupted. Over millions of years the magma cooled inside the crust of the earth creating a giant piece of rock.
By now you may be wondering, "If it cooled inside the earth, why does it stick out so much now?" To answer that question it is necessary to look at the other rocks in this area. Originally, the Enchanted Rock was underneath a layer of limestone, which is prevalent all across the state of Texas. The overlying limestone, which is a sedimentary rock, is much softer than the granite that composes the Enchanted Rock. In short, millions of years of wind, rain, ice etc… eroded away all the soft limestone and left approximately 400 feet of the Enchanted Rock exposed. Today, much of the Enchanted Rock is still buried and it is estimated the total size of this pluton is roughly the same as Manhattan. That's a lot of magma!
Enchanted Rock Granite
Minerology of the Enchanted Rock
Anyone could tell you the Enchanted Rock is granite, the same thing your kitchen countertop is made of, but what exactly does that mean? The color and texture of granite varies depending on what minerals get thrown into the mix when it is being formed. The particular granite that composes the Enchanted Rock contains a few very common minerals.
As you can see in the adjacent picture, it is possible to discern these minerals simply by observation. Orthoclase, the pink mineral is one of the most abundant minerals in the earth, and makes up most of the Enchanted Rock pluton. Quartz is the clear to grey looking mineral in the Enchanted Rock it is also very common and resistant to weathering. Plagioclase is the white mineral. Plagioclase is a cousin to orthoclase with only a slightly different composition.The black spots are most likely a dark mineral called hornblende. Each of these minerals contributes to the makeup of the Enchanted Rock.The slow cooling process can allow for minerals to grow quite large in plutons such as the Enchanted Rock. Adjacent is a picture of one of the many massive quartz veins that runs through this pluton.
Modern Day Processes at the Enchanted Rock
Thankfully, there is currently no volcanic activity at the Enchanted Rock. However, some other major geologic process are still happening. These processes are the weathering and erosion of this granite. As previously mentioned, granite is hard and does resist weathering better than limestone, however this does not mean it does not weather at all.
The picture to the right shows a weathering process called foliation. In the picture you can clearly see the large sheets of granite that look as if they're being broken off the main rock, which they are! Fluctuations in temperature cause the rocks to expand and contract. This eventually causes the brittle (yes brittle) rocks to crack and fracture. Water can then seep into these fractures, and if it freezes (like it did when I visited) the rocks can literally be wedged apart, as water expands when it freezes.
Fractures in the rocks can also play host to a different kind of weathering known as biogenic weathering. This is a weathering process where the breakup of rocks is aided by plants and or animals. Roots can forcibly crack rocks, while chemical changes due to plant life, or animal feces breakdown rocks further.
The main erosional force at the Enchanted Rock is gravity. Once the rocks are weathered from the protolith- or parent rock, gravity pulls them down to the bottom of this pluton. The smaller pieces can also be blown away by strong winds.
Erik Mion (author) on March 21, 2015:
Thank you all for the kind comments!
Mel Carriere from Snowbound and down in Northern Colorado on March 20, 2015:
This was a fascinating geological study. I was born in El Paso, Texas and have driven across the state, but have never swooped down south to see the hill country. Great hub!
Garrett Benham on March 20, 2015:
Well written piece with sweet images, thoroughly enjoyed.
ScarlettHenson from Charleston, South Carolina on March 19, 2015: