Explore the Wonders of the Colorado Plateau: Join Geotripper and the AAPG on May 23-29, 2015!

Antelope Canyon, on the Navajo Reservation near Page, Arizona

The Colorado Plateau, the region encompassing large parts of Arizona, Utah, New Mexico and Colorado, is one of the great geologic showplaces on planet Earth. Within the region, one can see in vivid colorful detail nearly two billion years of Earth history, from the ancient Proterozoic crust exposed at the bottom of the Grand Canyon to the Cenozoic lake sediments that formed the strange hoodoos of Bryce Canyon. The plateau country has been central to many of my blogs over the last five years, including three major series: Time Beyond Imagining, Vagabonding Across the 39th Parallel, and The Abandoned Lands. In addition to being a bountiful source of information about the past, it is one of the most beautiful landscapes in the world.

The Great Unconformity, the erosional boundary between the Proterozoic rocks of the Yavapai Orogeny and the Cambrian Tonto Group exposed in Diamond Creek on the Hualapai Reservation.

On May 23-29, 2014, I will be conducting a tour through the heart of the Colorado Plateau under the auspices of the American Association of Petroleum Geologists. The trip will begin and end in Las Vegas, Nevada, and will be a 1,000 mile loop through Grand Canyon National Park, Glen Canyon National Recreational Area, Grand Staircase-Escalante National Monument, Bryce Canyon National Park, and Zion National Park. The purpose of the journey is to provide an introduction to this fascinating landscape to anyone with an interest in geology, including geologists, teachers, students, and their family members. One does not need to be a member of the AAPG to participate. We will travel in rental vehicles (friendly drivers provided!), and stay in hotels at or near the parks. The fee, including all transportation costs during the trip, accommodations, tour fees, park entrance fees, and the trip guidebook, is $3,100 ($3,300 after 4/24/14). The fee doesn't include food, or travel to and from Las Vegas, where the trip will originate.

The Colorado River at Diamond Creek on the Hualapai Reservation

What will you see and learn? Our route will begin in Las Vegas. As we leave town, we will have a first look at the Colorado River at Hoover Dam, and then drive southeast on Highway 93 to Kingman Arizona. We will have a close look at the Peach Springs Tuff, remnants of a vast explosive eruption that blanketed thousands of square miles, providing some evidence of the origin of Grand Canyon.

From Kingman, we will head northeast on the longest remaining stretch of Route 66 to Peach Springs. At this point we expect to make our way down Diamond Creek, the only place where one can drive to the bottom of the Grand Canyon. We will have a close look at the Proterozoic and lower Paleozoic rocks of the canyon, formations not easily accessed in most parts of the Grand Canyon. If we are lucky, we may run across a herd of bighorn sheep.

We will then drive to the south rim of Grand Canyon, and spend a day exploring one of the most spectacular gorges in existence. Some free time will be available for a hike into the canyon, or for an optional canyon overflight. Relatively short (but steep) hikes from the rim provide access to the upper Paleozoic rocks of the plateau country, such as the Coconino Sandstone, Toroweap Formation, and Kaibab Limestone.

The following day we will work our way east to the canyon of the Little Colorado River and the Navajo Reservation. We will be exploring the Mesozoic formations of the plateau, including the Moenkopi, Chinle, Kayenta, Wingate and Navajo formations. Along the way we will stroll out to Horseshoe Bend on the Colorado River (below) and the incredible Antelope Canyon (the top photo), one of the most dramatic slot canyons to be found anywhere. We will spend a night in Page, Arizona, next to Lake Powell.

Horseshoe Bend on the Colorado River below Glen Canyon Dam.

From Page, we expect (weather conditions permitting) to follow Cottonwood Canyon to Grosvenor Arch and Kodachrome Basin State Park in Utah. The road follows the Cockscomb monocline, one of the major Laramide folds on the plateau (the southern extension of the fold forms the eastern edge of the Grand Canyon) through the heart of Grand Staircase-Escalante National Monument. The spectacular road exposes much of the Mesozoic stratigraphy found in the region, including the Tropic Shale, the Entrada Sandstone, and the Dakota Sandstone. Kodachrome Basin is a small gem of a park containing unusual sedimentary "pipes" that formed in the Entrada Sandstone.

The Cockscomb monocline near Kodachrome Basin State Park in Utah.

From Kodachrome Basin, we will climb through the Cretaceous sediments of the plateau country, including the Tropic Shale and Mesa Verde Group. We will arrive at Bryce Canyon National Park, which exposes one of the youngest formations on the Colorado Plateau, the Claron Formation. The hoodoos of Bryce are some of the most photogenic rocks to be seen anywhere. There will be time to hike below the rim for a completely different perspective on the unusual spires.

Wall Street Canyon in Bryce Canyon National Park

Leaving Bryce, we will head south along the Sevier fault and then turn west at Mt. Carmel Junction to drive into Zion National Park. Zion Canyon provides the best possible look at the incredible Navajo Sandstone, a Jurassic deposit that preserves the evidence of a vast sand sea that once covered a large part of the western United States.

Our route will take us on a little-traveled road through the western and northern part of the park to Lava Point. Along the way we will traverse a unique inverted stream, and pass through some rarely seen lava flows and cinder cones.

Leaving Zion, we will head southwest back to Las Vegas.

The guidebook for the trip was written by myself and my son Andrew, an anthropology professor at Modesto Junior College. It includes a great deal of information on the natural and human history of the plateau, as well as the geology.

There are a host of other wonders along the route! I've been writing about this country for a long time, introducing you, my readers, to one of the most beautiful and geologically rich corners of our planet. We've traveled together in words and pictures, and I would love the opportunity to travel with some of you in person this summer. Join us!

Detailed information and registration forms can be accessed at on the AAPG site (click here)  I would be pleased to answer any questions you might have by emailing me at hayesg (at) mjc.edu.

A Land of Strange Standing Stones, and an Odd Connection to the Grand Canyon

There are a lot of strange landscapes on the Colorado Plateau and otherworldly scenes. Some are famous enough as to not surprise first time visitors, such as the spires and hoodoos at Bryce Canyon National Park. But others are hidden, strung along gravel roads far off the beaten track. Seeing them for the first time comes as a shock. These rocks just aren't "normal". 

The largest single park in the Colorado Plateau region is also one of the least familiar. Really, how many of you have heard of Grand Staircase-Escalante National Monument? It covers a huge swath of land north of Grand Canyon and Glen Canyon National Recreational Area, west of Capitol Reef National Park, and south of Bryce Canyon. It was controversial in its birth, as have been most of our National Monuments, but it is indeed worthy of protection. We are only just beginning to discover the treasures that lie within its borders.

Our journey on this day would take us from Glen Canyon Dam to Bryce Canyon National Park via Cottonwood Wash Road, a gravel track that runs for thirty miles along the East Kaibab Monocline, known here as the Cockscomb.

Part of the Cockscomb (East Kaibab Monocline) courtesy of Google Earth

A monocline is a step-like fold, flat on either side and flexing in the middle. Such folds often develop where fault moves beneath horizontal sedimentary layers. The Cockscomb is an extraordinary example of one of these features, with a vertical separation of nearly a mile (erosion has leveled off much of the uplifted rock, so the actual elevation change across the fold is much less). The fold is also very long. It extends for 150 miles and actually forms the eastern edge of the Kaibab Plateau where the Colorado River turns west to form the deepest part of the Grand Canyon. It formed during the Laramide Orogeny in Late Cretaceous-Early Paleogene time.

From Wikipedia

The rocks within the monocline have been twisted so much that the layers are vertical. They have also been attenuated (stretched) so that some of the layers are thinned out. The rocks have been brecciated (crushed) to some extent, which provides a probable explanation for the strange towers and pinnacles found here and there along Cottonwood Wash Road. Groundwater following the fractures would have left mineral deposits that had the effect of reinforcing and cementing some of the most deformed rocks. Erosion removed the surrounding softer rocks leaving behind the towers and spires.

Pareidolia is the tendency of humans to build patterns out of randomness, seeing things that aren't really there: faces in clouds, and human or animal figures in rocks. Who does the rock below bring to mind?

The final rock in our little mini-tour of the Grand Staircase is Grosvenor Arch, which is really two arches, and which once was called Butler Arch until people on an expedition with the National Geographical Society decided to name it after their boss. They apparently had more pull with the Board of Geographic Names. It's not part of the monocline, but is instead at the boundary between two layers of different erosional resistance. The upper rock is a conglomerate equivalent to the early Cretaceous Cedar Mountain Formation, while the lower layer is the Henrieville Sandstone of Jurassic age. The largest opening is 152 feet high and 100 feet wide.

Lastly I have pictures of flowers. Despite the ongoing drought, there were some beautiful wildflowers blooming in one of the side canyons we explored. There were Evening Primroses...

...and some beautiful Sego Lilies, the state flower of Utah.

Vagabonding Across the Colorado Plateau: Join Geotripper and the AAPG on May 31-June 6, 2014!

Antelope Canyon, on the Navajo Reservation near Page, Arizona

The Colorado Plateau, the region encompassing large parts of Arizona, Utah, New Mexico and Colorado, is one of the great geologic showplaces on planet Earth. Within the region, one can see in vivid colorful detail nearly two billion years of Earth history, from the ancient Proterozoic crust exposed at the bottom of the Grand Canyon to the Cenozoic lake sediments that formed the strange hoodoos of Bryce Canyon. The plateau country has been central to many of my blogs over the last five years, including three major series: Time Beyond Imagining, Vagabonding Across the 39th Parallel, and The Abandoned Lands (I'm also slowly working on the latest, America's Never-Never). In addition to being a bountiful source of information about the past, it is one of the most beautiful landscapes in the world.

The Great Unconformity, the erosional boundary between the Proterozoic rocks of the Yavapai Orogeny and the Cambrian Tonto Group exposed in Diamond Creek on the Hualapai Reservation.

On May 31-June 6, 2014, I will be conducting a tour through the heart of the Colorado Plateau under the auspices of the American Association of Petroleum Geologists. The trip will begin and end in Las Vegas, Nevada, and will be a 1,000 mile loop through Grand Canyon National Park, Glen Canyon National Recreational Area, Grand Staircase-Escalante National Monument, Bryce Canyon National Park, and Zion National Park. The purpose of the journey is to provide an introduction to this fascinating landscape to anyone with an interest in geology, including geologists, teachers, students, and their family members. One does not need to be a member of the AAPG to participate. We will travel in rental vehicles (friendly drivers provided!), and stay in hotels at or near the parks. The fee, including all transportation costs during the trip, accommodations, tour fees, park entrance fees, and the trip guidebook, is $2,900 ($3,100 after 5/1/14). The fee doesn't include food, or travel to and from Las Vegas, where the trip will originate.

The Colorado River at Diamond Creek on the Hualapai Reservation

What will you see and learn? Our route will begin in Las Vegas. As we leave town, we will have a first look at the Colorado River at Hoover Dam, and then drive southeast on Highway 93 to Kingman Arizona. We will have a close look at the Peach Springs Tuff, remnants of a vast explosive eruption that blanketed thousands of square miles, providing some evidence of the origin of Grand Canyon.

From Kingman, we will head northeast on the longest remaining stretch of Route 66 to Peach Springs. At this point we expect to make our way down Diamond Creek, the only place where one can drive to the bottom of the Grand Canyon. We will have a close look at the Proterozoic and lower Paleozoic rocks of the canyon, formations not easily accessed in most parts of the Grand Canyon. If we are lucky, we may run across a herd of bighorn sheep.

We will then drive to the south rim of Grand Canyon, and spend a day exploring one of the most spectacular gorges in existence. Some free time will be available for a hike into the canyon, or for an optional canyon overflight. Relatively short (but steep) hikes from the rim provide access to the upper Paleozoic rocks of the plateau country, such as the Coconino Sandstone, Toroweap Formation, and Kaibab Limestone.

The following day we will work our way east to the canyon of the Little Colorado River and the Navajo Reservation. We will be exploring the Mesozoic formations of the plateau, including the Moenkopi, Chinle, Kayenta, Wingate and Navajo formations. Along the way we will stroll out to Horseshoe Bend on the Colorado River (below) and the incredible Antelope Canyon (the top photo), one of the most dramatic slot canyons to be found anywhere. We will spend a night in Page, Arizona, next to Lake Powell.

Horseshoe Bend on the Colorado River below Glen Canyon Dam.

From Page, we expect (weather conditions permitting) to follow Cottonwood Canyon to Grosvenor Arch and Kodachrome Basin State Park in Utah. The road follows the Cockscomb monocline, one of the major Laramide folds on the plateau (the southern extension of the fold forms the eastern edge of the Grand Canyon) through the heart of Grand Staircase-Escalante National Monument. The spectacular road exposes much of the Mesozoic stratigraphy found in the region, including the Tropic Shale, the Entrada Sandstone, and the Dakota Sandstone. Kodachrome Basin is a small gem of a park containing unusual sedimentary "pipes" that formed in the Entrada Sandstone.

The Cockscomb monocline near Kodachrome Basin State Park in Utah.

From Kodachrome Basin, we will climb through the Cretaceous sediments of the plateau country, including the Tropic Shale and Mesa Verde Group. We will arrive at Bryce Canyon National Park, which exposes one of the youngest formations on the Colorado Plateau, the Claron Formation. The hoodoos of Bryce are some of the most photogenic rocks to be seen anywhere. There will be time to hike below the rim for a completely different perspective on the unusual spires.

Wall Street Canyon in Bryce Canyon National Park

Leaving Bryce, we will head south along the Sevier fault and then turn west at Mt. Carmel Junction to drive into Zion National Park. Zion Canyon provides the best possible look at the incredible Navajo Sandstone, a Jurassic deposit that preserves the evidence of a vast sand sea that once covered a large part of the western United States.

Our route will take us on a little-traveled road through the western and northern part of the park to Lava Point. Along the way we will traverse a unique inverted stream, and pass through some rarely seen lava flows and cinder cones.

Leaving Zion, we will head southwest back to Las Vegas.

The guidebook for the trip was written by myself and my son Andrew, an anthropology professor at Modesto Junior College. It includes a great deal of information on the natural and human history of the plateau, as well as the geology.

This is the second time we are making this journey, and we had a great time last year, with a marvelous group of geologists and their families, some of whom traveled from as far away as Australia and Canada. This year's crew looks to be equally international.

There are a host of other wonders along the route! I've been writing about this country for a long time, introducing you, my readers, to one of the most beautiful and geologically rich corners of our planet. We've traveled together in words and pictures, and I would love the opportunity to travel with some of you in person this summer. Join us!

Detailed information and registration forms can be accessed at on the AAPG site (click here)  I would be pleased to answer any questions you might have by emailing me at hayesg (at) mjc.edu.

Time Beyond Imagining on the Colorado Plateau: You can imagine it too, on June 1-7, 2013

Antelope Canyon, on the Navajo Reservation near Page, Arizona

The Colorado Plateau, the region encompassing large parts of Arizona, Utah, New Mexico and Colorado, is one of the great geologic showplaces on planet Earth. Within the region, one can see in vivid colorful detail nearly two billion years of Earth history, from the ancient Proterozoic crust exposed at the bottom of the Grand Canyon to the Cenozoic lake sediments that formed the strange hoodoos of Bryce Canyon. The plateau country has been central to many of my blogs over the last five years, including three major series: Time Beyond Imagining, Vagabonding Across the 39th Parallel, and The Abandoned Lands. In addition to being a bountiful source of information about the past, it is one of the most beautiful landscapes in the world.

The Great Unconformity, the erosional boundary between the Proterozoic rocks of the Yavapai Orogeny and the Cambrian Tonto Group exposed in Diamond Creek on the Hualapai Reservation.

On June 1-7, 2013, I will be conducting a tour through the heart of the Colorado Plateau under the auspices of the American Association of Petroleum Geologists. The trip will begin and end in Las Vegas, Nevada, and will be a 1,000 mile loop through Grand Canyon National Park, Glen Canyon National Recreational Area, Grand Staircase-Escalante National Monument, Bryce Canyon National Park, and Zion National Park. The purpose of the journey is to provide an introduction to this fascinating landscape to anyone with an interest in geology, including geologists, teachers, students, and their family members. One does not need to be a member of the AAPG to participate. We will travel in rental vehicles (friendly drivers provided!), and stay in hotels at or near the parks. The fee, including all transportation costs during the trip, accommodations, tour fees, park entrance fees, and the trip guidebook, is $2,850 ($3,050 after 5/3/13). The fee doesn't include food, or travel to and from Las Vegas, where the trip will originate.

The Colorado River at Diamond Creek on the Hualapai Reservation

What will you see and learn? Our route will begin in Las Vegas. As we leave town, we will have a first look at the Colorado River at Hoover Dam, and then drive southeast on Highway 93 to Kingman Arizona. We will have a close look at the Peach Springs Tuff, remnants of a vast explosive eruption that blanketed thousands of square miles, providing some evidence of the origin of Grand Canyon.

From Kingman, we will head northeast on the longest remaining stretch of Route 66 to Peach Springs. At this point we expect to make our way down Diamond Creek, the only place where one can drive to the bottom of the Grand Canyon. We will have a close look at the Proterozoic and lower Paleozoic rocks of the canyon, formations not easily accessed in most parts of the Grand Canyon. If we are lucky, we may run across a herd of bighorn sheep.

We will then drive to the south rim of Grand Canyon, and spend a day exploring one of the most spectacular gorges in existence. Some free time will be available for a hike into the canyon, or for an optional canyon overflight. Relatively short (but steep) hikes from the rim provide access to the upper Paleozoic rocks of the plateau country, such as the Coconino Sandstone, Toroweap Formation, and Kaibab Limestone.

The following day we will work our way east to the canyon of the Little Colorado River and the Navajo Reservation. We will be exploring the Mesozoic formations of the plateau, including the Moenkopi, Chinle, Kayenta, Wingate and Navajo formations. Along the way we will stroll out to Horseshoe Bend on the Colorado River (below) and the incredible Antelope Canyon (the top photo), one of the most dramatic slot canyons to be found anywhere. We will spend a night in Page, Arizona, next to Lake Powell.

Horseshoe Bend on the Colorado River below Glen Canyon Dam.

From Page, we expect (weather conditions permitting) to follow Cottonwood Canyon to Grosvenor Arch and Kodachrome Basin State Park in Utah. The road follows the Cockscomb monocline, one of the major Laramide folds on the plateau (the southern extension of the fold forms the eastern edge of the Grand Canyon) through the heart of Grand Staircase-Escalante National Monument. The spectacular road exposes much of the Mesozoic stratigraphy found in the region, including the Tropic Shale, the Entrada Sandstone, and the Dakota Sandstone. Kodachrome Basin is a small gem of a park containing unusual sedimentary "pipes" that formed in the Entrada Sandstone.

The Cockscomb monocline near Kodachrome Basin State Park in Utah.

From Kodachrome Basin, we will climb through the Cretaceous sediments of the plateau country, including the Tropic Shale and Mesa Verde Group. We will arrive at Bryce Canyon National Park, which exposes one of the youngest formations on the Colorado Plateau, the Claron Formation. The hoodoos of Bryce are some of the most photogenic rocks to be seen anywhere. There will be time to hike below the rim for a completely different perspective on the unusual spires.

Wall Street Canyon in Bryce Canyon National Park

Leaving Bryce, we will head south along the Sevier fault and then turn west at Mt. Carmel Junction to drive into Zion National Park. Zion Canyon provides the best possible look at the incredible Navajo Sandstone, a Jurassic deposit that preserves the evidence of a vast sand sea that once covered a large part of the western United States.

Our route will take us on a little-traveled road through the western and northern part of the park to Lava Point. Along the way we will traverse a unique inverted stream, and pass through some rarely seen lava flows and cinder cones.

Leaving Zion, we will head southwest back to Las Vegas.

There are a host of other wonders along the route! I've been writing about this country for a long time, introducing you, my readers, to one of the most beautiful and geologically rich corners of our planet. We've traveled together in words and pictures, and I would love the opportunity to travel with some of you in person this summer. Join us!

Detailed information and registration forms can be accessed at http://www.aapg.org/education/fieldseminars/details.cfm?ID=76. I would be pleased to answer any questions you might have by emailing me at hayesg (at) mjc.edu.

Time Beyond Imagining - A not-so-brief History of the Colorado Plateau

I'm almost embarrassed to come back to this subject, but I have always had an unfortunate propensity to leave big projects unfinished and I would like to overcome it. I was also inspired by the reemergence of the Accretionary Wedge after a brief absence, and some of the final posts in this series will involve the newest theme of the Wedge for June. The subject of my blog is the geologic history of the Colorado Plateau, and it has been a theme of my blogs since last July, although posts have been sporadic of late. Check here to get caught up. My last post concerned the disaster that met the animals of the region at the end of the Mesozoic era. This post will seem similar, but now we are looking forward to the new world that was left to the survivors at the end of the age.

The Colorado Plateau of the early Cenozoic was a new and unique landscape, unlike anything that had passed before. Somewhat like the last post, it brings to mind another poetic passage in the Bible, from Isaiah: "For behold, I create new heavens and a new earth; And the former things will not be remembered or come to mind." The oceans, which for many eons had washed over the region in a series of transgressions and regressions, had receded far to the west and south, and never again would lay down sediments on the Plateau. The crust had been buckled by regional compression which reactivated ancient faults in the deep crust and forced the rocks into a series of structural domes and basins. This event, the Laramide Orogeny, is what raised the Rocky Mountains, and formed the broad outlines of sub-provinces of the Colorado Plateau that we see today. The edge of one of the uplifted domes is seen as the Cockscomb Monocline in Grand Staircase/Escalante National Monument. Farther north, the buckled rocks form the eastern edge of the Kaibab Plateau that is bisected by the Grand Canyon.

Rivers were established across the landscape, and some ended up with nowhere to go, forming vast lakes in what is now Utah, and Wyoming. Volcanism swept across the region as well. But more than anything else, the region was now far above sea level, so in most areas it was eroding, and rocks that had been laid down over the previous 2 billion years were now being stripped away and being carried to the sea. For the geologists of today, it meant that the evidence of the past was disappearing, and in many respects, the Cenozoic Era is one of the most cryptic time periods for us to decipher. Compared to Paleozoic and Mesozoic time, Cenozoic rocks are fairly rare on the Plateau, and thus little evidence remains to tell us what happened, or who was living here.

And that is the other part of the story...the ecosystem of the region, and indeed the entire planet had been decimated by...something. The iconic dinosaurs were gone, and many large denizens of the oceans had disappeared as well. The land-based ecosystems in the earliest part of the Cenozoic were depleted, especially of larger animals. The mammals, who for whatever reason had survived the extinction event, vied with the birds for dominance. The birds almost won! Some species of the avian clan were large flightless predators that would have done their dinosaurian ancestors proud. But by and by, the birds retreated to the environmental niche they were best adapted for, the trees and skies, and mammal-based ecosystems were established in forests and grasslands throughout the world.

Posts coming soon on the Cenozoic's unique national park on the plateau, and the evidence of volcanism in the region. And...where the heck did the Grand Canyon come from?