GREAT
GRANITE!!
This earth cache
begins at the parking area for Segment 2 of the Colorado
Trail.
There is no hiking involved to log this cache, just gathering
information about the natural world and applying some scientific
theory at both Stages 1 and 2.
Both stages are along the same road, and it is a very short
drive (or long walk) between the two stages.
This earthcache is two stages.Both stages offer many parking
spots or pull-offs.
The road in this area once served as a stage and rail line.
There are many caches in the area commemorating settlers, pioneers,
miners, everyday heroes, and mother earth.
To log this earth cache, answer the questions to the best of
your ability.Feel free to post photos of your adventure.
Answers that contain little to no information about your visit
to this cache will be deleted.
STAGE 1:
Stage 1 provides an array of Granite, an intrusive,
coarse-grained igneous rock composed of primarily of quartz and
feldspars.
Igneous rock is formed when magma solidifies.
"Igneous"comes from the Latin word for fire, and all igneous
rocks began as hot, fluid material. This material may have been
lava erupted at the Earth's surface, or magma (unerupted lava) at
shallow depths, or magma in deep bodies (plutons).
Rock formed from lava is called extrusive, rock from shallow
magma is called intrusive and rock from deep magma is called
plutonic.
Igneous rocks formed in this area where continental crust was
pushed together, making it thicker and allowing it to heat to
melting.
Many people commonly think of lava and magma as a liquid, like
molten metal, but geologists find that magma is usually a mush - a
liquid carrying a load of mineral crystals.
Magma crystallizes into a collection of minerals, and some
crystallize sooner than others. When the minerals crystallize, they
leave the remaining liquid with a changed chemical composition.
Thus a body of magma, as it cools, evolves, and as it moves through
the crust, interacting with other rocks, it evolves further.
Questions for Stage 1:
A. Describe the granite just across the bridge. Include forms,
colors and texture. What are other features you noticed?
B. There is an old quartz quarry just west of this spot. With
this knowledge, how does quartz content affect the appearance of
the rock formations here?
C. Where and how does the South Platte River originate?
D. What mineral causes the color of the granite here at Stage
1?
STAGE 2
Now go to: N 39 22.796 W 105 10.194
This area is home to many impressive granite rocks and domes.
The rock is Pikes Peak Granite, approximately 1.09 billion years
old. This outcropping of granite is part of the Pikes Peak
batholith exposure.
Questions for Stage 2:
E. Describe the rock formations here. Include size, shapes, and
texture. How does this granite differ in appearance from Stage
1?
F. What might have caused the rock here to appear the way it
does?
G. Was the rock here formed by lava, shallow magma, or deep
magma ?
Email your answers to: isisfan1@yahoo.com
