Sunday, September 27, 2009

Pictures From My 2009 "Geology and Hiking River Trip" in Grand Canyon

This years trip was another wonderful success! We had a very special group of people who were interested in learning more about the geology of the Grand Canyon from a river perspective. Our guides were accommodating, the weather was splendid, and the muddy river subtly revealed her secrets through time. This is not a complete review of our trip but merely some snapshots of portions of our trip that lasted for 10 days.

September 13 at Lees Ferry had a wondrous sky to the southwest. We received our only significant rain of the whole trip (1/2 hour) later on this evening. The Vermilion Cliffs rise in the background.

Shortly after leaving Lees Ferry, we passed slightly upturned strata that signal the very start of the Grand Canyon. Here is the cream-colored Kaibab Formation just beginning to rise from below the river. Incredible to think that millions of tourists stand on this same stratigraphic horizon 88 miles downstream from here on both the north and south rims. While the river drops an average of 8 feet per mile, the rocks rise out of the ground an average of 70 feet per mile and that is how the high elevations of the tourist areas are achieved. It all starts here.

At about Mile 13, a narrow gorge is cut through the Supai Group rocks.

Our first hike of the trip was up the drainage of North Canyon. This is a very special place with many features of geologic interest.

Rains from the previous evening delivered fresh mud in the stream bed. It looked like chocolate milk.

Another intriguing feature we observed was exfoliation in sandstone. Note how the sandstone spalls parallel to all of the drainages - as the confining pressure is released by the erosion and removal of overlying rock, the sandstone pops out to create these lines of weakness.

Other interesting features observed in the Supai Group are the many root cast from plants that were anchored in the ancient sandy soils. Here is one with the trunk and underlying roots exposed in cross-section.

Alternating beds of cliff-forming sandstone (above) and slope-forming mudstone (below) suggest intervals of climate change during deposition of the Supai Group in the Pennsylvanian Period. The sands may have been deposited in eolian dunes, while the mud may have derived on the muddy floodplain of a river. Here Mark checks out the deposits.

The Grand Canyon and Colorado River always seem to attract unique sporting endeavors. On numerous occasions we passed a world-class surfer who was attempting to paddle the entire length of the canyon on a surfing paddle board. Amazing.

Early morning reflections in the large President Harding loop in the river.

Near the southern end of Marble Canyon, the Bright Angel Shale is beautifully exposed.

I have never seen as many Big Horn sheep as we saw on this trip. A retired BLM biologist, Terry Ruzzi, gladly shared his knowledge of the species with the group. I estimate that we saw over 75 big horn in nine days. Perhaps they were along the river because of unusually dry conditions elsewhere in the canyon.

Not many camps exist in the Inner Gorge of the canyon but we found a nice one at Grapevine Camp across from Vishnu Creek. Everyone enjoyed this ample sandy camp within this beautiful gorge.

Here Gail and Peggy reflect on a days worth of exploration in camp.

Many rapids line the channel of the Colorado and here our group is enjoying the ride in one of the more moderate drops. Most rapids are formed when side canyons deliver boulders to the main channel in big side canyon floods.

In Stephen Aisle, we camped beneath some wonderful Tapeats Sandstone towers. Groundwater most likely weakened the cement of this part of the sandstone but the harder horizons stick out in relief.

Steve, John, and Jim enjoy a quiet moment in camp. These sandy beaches are clean and provide an unbelievably comfortable place from which to watch the sunset in the Grand Canyon.

Peggy relaxing on a boulder in camp.

Here is a view of The Great Unconformity in Blacktail Canyon. The schist below is 1,200 million years older that the sandstone that overlies it. This is more than 1/4th of all earth history.

A rare shot of Bill while not taking a picture on the river. A child-like enthusiasm often overcomes people as they travel down the river.

Within the Middle Granite Gorge are a series of pink dikes that here seem to overwhelm the preexisting black schist. Their patterns are curiosities that beg for photographs.

Islands of rock once stood above a Cambrian sea. I inserted a red line that distinguishes the sea sand (top) from the older rocks that formed high-standing islands (below line). This all happened 525 million years ago.

The temperature of the Colorado River is a cold 48 degrees but many of the side canyons harbor warm, clear water streams. This one is Stone Creek located at about Mile 130.

While returning to Stone Creek beach Mike spotted a Chuckwalla (Sauromalus obesis) sunning on a rock. When alarmed these large lizards will slip into a narrow crack and inflate their lungs with air to wedge inside for protection. Paiute Indians would travel through Northern Arizona with sharp sticks to deflate them and then enjoy a hearty meal.

At only one location in Grand Canyon does a waterfall enter directly into the Colorado River - Deer Creek. This curious setting is the result of a large rock slide that blocked an ancestral Deer Creek, causing it to carve a new route to the river. The new canyon has not yet had time to cut down the grade.

Upper Deer Creek above the falls.

Spectacular view to the east along the Middle Granite Gorge.

This is much the same view as the previous picture but was taken the following morning when smoke from a fire had filled the canyon. We could smell the thick smoke but it lifted later in the day.

The blue water of Cataract Creek in Havasu Canyon. This was a welcome stop away from the muddy river.

As we approached Lava Falls on the river, we spotted a thin black volcanic dike rising up through the stack of sedimentary layers. See if you spot the dike as it rises through the rocks.

A fantastic lava cascade filling a north side canyon.

Look at these beautiful radiating columns within a lava flow. As this lava was cooling, water (either from rain or the river) infiltrated the flow and caused the unique pattern to form.

View of a lava flow remnant along the river.

View south towards Diamond Peak and the Hurricane Fault. The peak is on the downthrown side of the fault - I have inserted a red line to show the approximate trace of the fault. Here as much as 2,000 feet of offset is displayed as the much older Vishnu Schist (left) is placed next to the Muav Limestone (in Diamond Peak).

In the Lower Granite Gorge spectacular fluting in the crystalline rocks is seen. These form when a pebble spins in floods in a small depression, chiseling its way deeper into the bedrock.

A view of the Lower Gorge strata.

The water of Lake Mead is very low right now and deposits of the young "Lake Mead formation" are now being incised by the rejuvenated Colorado River. I once rowed boats on top of these deposits when the lake was much higher.

Here is the new Pearce Ferry Rapid, formed as the river has established a new course across a spur of the consolidated Muddy Creek Formation. This is a nasty rapid that swamped our boat.

After exiting the Grand Wash Cliffs and the western end of the Grand Canyon, all of the previously flat-lying strata are turned up on end. These are most likely deposits of the Supai Group.

I hope you enjoyed this recollection of my last geologic exploration in the canyon. Thanks to the 19 people who took this trip and our three wonderful boatmen from Canyoneers who were so professional in the execution of their craft.

Saturday, September 12, 2009

The Grand Canyon Skywalk - Hualapai Dreamland

I do not know anyone, not a river runner, Grand Canyon resident, or friend who has gone out on the Hualapai tribe's new glass Skywalk. So when I had a chance to visit this attraction at half price, I jumped - let me rephrase that - I took advantage of the opportunity. I was helping out on a Hollywood scout of the Grand Canyon in a pre-production locations search for an upcoming movie called "Due Date" starring Robert Downey Jr. No stars we present - just the director and producer who weighed the pro's and con's of filming here at Grand Canyon West (GCW) or the traditional view at Grand Canyon National Park.

The approach to the Skywalk is off of the Pierce Ferry/Meadview Road. Joshua Trees greet travelers on this dirt track which is currently being paved by Mojave County. The Grand Wash Cliffs, edge of the Colorado Plateau, is the background.

The empty entrance booth. Fees to enter Hualapai land total $42.00 per person. This includes a $29.00 entrance fee, $3.00 fuel charge (for the bus rides), $8.00 Impact Fee, and a Hualapai Tribal tax.

The gift shop has loads of plastic tomahawk's and stuffed Indian dolls.


After a short 3 mile bus ride, this was my first view of the Skywalk* There is no other angle from which to take a picture of it and camera's are not allowed on the "bridge." There are photographers wandering the glass plus photo radar type cameras to take your picture. Starting price $30.00 for one picture.

* I have seen the Skywalk from the river looking up.

Here you see the full drop to the Colorado River. Pre-trip information states that "it is 4,000 ft. straight down to the river." Actually it is about 800 feet down to a ledge of Redwall Limestone and about 2,700 feet above the river. Many exaggerations in statistics were noted. To go onto the Skywalk is an additional $32.05 on top of the previous fees.

I stayed out on the bridge for about an hour - long enough to listen to three different sets of people come through. Some were very scared and did not wander out onto the glass. Others were in awe of the Skywalk. But most folks seemed to be taken by the majesty of the Grand Canyon.

This is the backside of the Skywalk building. It is beautifully constructed but unfinished at this time.

There are some nice shade structures constructed away from the rim of the canyon. This one houses a dance floor where women of the tribe dance during the day.

Here are two members of the tribe doing a dance. No one was watching when I was here.

Numerous wikiups are constructed around a cultural trail. They also have Plains Indian tipis, Hopi pueblos, and Navajo hogans. The added benefit of these wikiups is that have full electricity (foreground).

This is Don, another Hualapi tribal member, I just loved his red feather headress.

I wonder if the name of this restaurant is lost on people? The Bat Shit Cafe!

A gorgeous view of the Colorado River from Guano Point. Note that the river here is perched on at least 50 feet of sediment deposited when Lake Mead was much higher. Thus, the river is not "natural" here.

Guano Point was named because this is where a cableway was built to extract guano from Bat Cave down near the river. After constructing this cableway, it was determined that there was very little guano to be mined and the effort died.

The seal of the Hualapai tribe. I have mixed feelings about this development. I wish the tribe well, but there is certainly a sense of "retribution" that I feel from the tribe. It is much more expensive to visit GCW vs. the national park. Many things seem hokey, trite, and ill-advised. But perhaps the greatest threat from this type of "entertainment tourism" is that it may only be the tip of the proverbial iceberg for what the tribe has in store here in the future. Right now there is a "Vietnam-type" atmosphere at GCW with zillions of helicopters and planes in the air. It is not a peaceful place. These helicopters bring tourists to boats that ply the river - with a total disregard for the Grand Canyon River Management Plan. A Las Vegas entrepreneur put up the money for the Skywalk and takes half of the receipts. What future deals will the tribe make with Las Vegas personalities? Hotels in the canyon? Casinos? Are tribes immune to rules, decorum, or even common sense in places like the Grand Canyon. Or is it "their land" with a right to do "whatever we want?" It all harbors a very chilling thought.

Old Route 66 west of Seligman, Arizona.