Walter and Sara On the road to who knows where
The Trail of Time begins not far from the Geology Museum near Yavapai Point at the Grand Canyon. Here they have done a great job trying to help you wrap you mind around the age of the rock layers that can be found in the Canyon. They have placed brass rounds in the walkway with years marked on them. They start with having you find your age (funny how they’re already working up to 10 year intervals by the time you hit 60) and then quickly time telescopes so that a stride is a million years and then 10 million years!

Believe it or not the canyon itself is pretty young. The Colorado River only began to carve the canyon 5 or 6 million years ago. It has made a lot of progress in such a short time!

As you walk along the the trail they show you samples of the rocks in the layers corresponding to the time period you’re walking through. It starts with Banded spring deposits which you find at the top of the canyon. It relatively new rock.

Banded spring deposit Grand Canyon

Then you pass a sample of basalt since there was volcanic activity 1,000 to 100,000 years ago along the canyon.

Basalt

Kaibab limestone is usually considered the top layer of most of the Grand Canyon. The rock in this layer is 270 mile years old. They are rocks formed from a time when shallow seas covered the area.

Kaibab Limestone

Toroweap sandstone is the next layer down. It is made up of river and sea deposits from 273 million years ago.

Toroweap sandstone

Coconino sandstone is 275 million years old. It was formed from sand dune deposits.

Coconino sandstone

If you look across the canyon in this photo you can see the top 4 layers pretty clearly. The top layer is the Kaibab Formation at 270 million years old. The next layer is the Toroweap Formation at 273 million years old. The 3rd layer down (the wide white band) is Coconino Sandstone at 275 million years old. The 4th layer (the sloping darker layer) is the Hermit Formation which is 280 million years old.

Top 4 layers of rock at Grand Canyon

Below that you can see the beginnings of the Supai Group which covers 285 to 315 million years ago. This group is comprised of layered Paleozoic Rocks that comprise the upper two thirds of the canyon's walls.

These rocks formed near sea level at the edge of the continent.

It includes Esplanade sandstone which is 285 million years old.

Esplanade Sandstone

After the Supai Group comes Redwall Limestone at 340 million years old and Temple Butte Formation which is 385 million years old. There is then a gap where the rock layers were eroded away before new layers were deposited. So we lose 120 million years of record!

And then we come to the Tonto Group which includes Muav limestone which is 505 million years old.


Muav limestone

And Bright Angel Shale which is 515 million years old.

Bright Angel shale

And Tapeats sandstone at 525 million years old.

Tapeats sandstone

Next we come to the Grand Canyon Supergroup which is are only visible in a few places in the canyon. The strata of the Supergroup accumulated in basins formed as the land mass pulled apart (going back over a billion years ago). The expansion caused the blocks of the layers to tilt, inclining the layers. The youngest of the visible tilted layers is Sixtymile conglomerate at 650 million years old.

Sixtymile conglomerate

Followed by Awatubi limestone at 750 million years old.

Awatubi limestone

And Carbon Butte sandstone at 760 million years old.

Carbon Butte sandstone

Duppa sandstone at 770 million years old

Duppa sandstone

Carbon Canyon limestone at 780 million years old

Carbon Canyon limestone

Jupiter limestone at 790 million years old

Jupiter limestone

Tanner limestone is 800 million years old

Tanner limestone

Nanloweap sandstone is 900 million years old

Nankoweap sandstone

Shinumo sandstone is 1,170 million years old or 1 billion 170 million years.

Shinumo sandstone

Hakatai sandstone is 1,180 million years old

Hakatai sandstone

Bass limestone is 1,190 million years old

Bass limestone

And the last of the Supergroup is Hotauta conglomerate which is 1,200 million years old.

Hotauta conglomerate

They gave us a sample of Cremation pegmatite at 1,698 milion years old but it doesn't show up in any of the literature I've found so I would guess it is very hard to find in the canyon.

Cremation pegmatite

The same is true for Horn Creek granite at 1,713 million years old.

Horn Creek granite

And Ruby gabbro at 1716 million years old.

Ruby grabbro

Finally we come to what is known as the Vishnu Basement Rocks. These were all formed nearly 2 billion years ago when a tectonic plate carrying an island chain and the plate that became North America collided. The heat and pressure from this collision changed the existing rock layers into dark metmorphic rock--the basement of the canyon. Molten rock squeezed into cracks and hardened as light bands of granite.

This is a sample of Folded Vishnu basement rock.

Folded Vishnu basement rock

Trinity granite has the same distinctive dark color. It is 1,730 million years old.

Trinity granite

Diamond Creek granite has intrusions of lighter granite. It is 1736 million years old.

Diamond Creek granite

Zoraster granite is 1740 million years old.

Zoroaster granite

Vishnu schist is 1745 million years old.

Vishnu schist

Brahma schist is 1750 million years old.

Brahma schist

Rama schist has red intrusions and is 1755 million years old.

Rama schist

And finally we hit bottom as it were, with Elves Canyon gneiss which is the oldest rock visible in the canyon at 1840 million years old. While it was formed 1840 million years ago it was transformed into gneiss only 1700 million years ago.

While nearly 2 billion years sounds incredibly old it is only 2/5ths the age of the earth itself.

Elves Chasm gneiss

When you arrive at the end of the trail the last of the markers indicates that we've covered 1999 million years in our Trail of Time.
 
1999 million years ago

Here is a sign showing how the layers in the canyon work. The tilted layers in the middle are the Grand Canyon Supergroup. And the old fossil standing next to the sign is of course, wonderful Walter.

Trail of Time rock layer sign