700 Months

How big is the number 700? Not very big in today's world (and certainly not for a geologist). But 700 months. How long do you think 700 months is?

Well I can tell you because on Nov. 1, I will turn 700 months old! It sounds like such a short time doesn't it? "Really? Only 700 months?" Yep, it's true.

So the first day of November I will turn 58.25 years old or

700 months;
3,045 weeks;
21,308 days;
511,400 hours;
About 30,683,500 minutes;
or 1,840,997,000 seconds.

If you'd like to know how old you are, check out this web site: http://www.paulsadowski.com/Birthday.asp. It's fun and a happy place to be.

Disclaimer! This photograph of me was taken in my 682nd month at one of my favorite places - the inner gorge of the Grand Canyon!

10,000th Copy of "Ancient Landscapes" Sold At GCNP

Late on the afternoon of September 22 (or thereabouts), someone at Grand Canyon National Park bought the 10,000 copy of the book, "Ancient Landscapes of the Colorado Plateau". I don't know who that lucky person was, or where they live. But if there was any way that i could know, I would inscribe a most appropriate notation on the inside title page.

"ALCP" made its debut on bookshelves in October, 2008 to robust reviews. The book's "back story" however, is quite interesting. For years prior to its publication, I had been admiring Ron Blakey's paleogeographic maps and using them in the geology classes I taught at Yavapai and Coconino Community Colleges. Being a former student of Ron's at Northern Arizona University, I became filled with his infectious enthusiasm for rock strata and the ancient landscapes they reveal. I occasionally heard from Ron (and others) that he was about to publish a book containing the maps and always made it a point to ask him about it when I saw him at a professional meeting. All too often, he would relate his most recent publishing "detour". (He had three prior publishers lined up at different times and on one occasion was close to a deal with Oxford University Press). The only person more disappointed than Ron in hearing the news was myself, as I knew that his maps provided an excellent avenue for people to learn about geology and earth history.

Then in 2005, while attending the Annual Meeting of the Geological Society of America (GSA) in Salt Lake City, I saw Ron in the exhibit area of the convention floor. I had not seen him for a few years but once again asked him how the book project was coming along. He gave what was becoming an all too familiar look of disappointment and shuffled his feet and shook his head with disgust. Obviously, there had been another setback. I was disappointed once again to get the news. But then an idea came to mind! I was at the meeting to attend the professional talks and to promote and sign my new book, "Carving Grand Canyon". The book had been recently published by the Grand Canyon Association (the non-profit partner for Grand Canyon National Park) and I was aware that they were willing to consider other geology titles for future books. Within about 15 minutes of talking to Ron about a possible collaboration, the idea for "ALCP" came to light that moment in Salt Lake City.

It took three years to write new text and to design the book (beautifully executed by Ron Short). But by the time GSA held its Annual Meeting in October, 2008 in Houston, Texas, Ron Blakey and I were doing our own book signing on the convention floor.

Book signing at the GSA Annual Meeting in Houston, Texas in October, 2008

"Ancient Landscapes of the Colorado Plateau" is selling as well or even better now as it was on the day it was published. Both Ron and I are appreciative of the support that the Grand Canyon Association gives us and remain gratified that so many professionals and lay persons alike are benefiting from the story it tells. It is an amazing work and I receive correspondence from readers all the time telling me how it has helped them "get over the hump" in learning geologic concepts. ALCP rocks!

Yellowstone Article Posted On US Route 89 Web Site

One of the joys of being a geologic interpreter is that you often get a chance to explain some earthly phenomena for a general audience. It may be a public lecture, a chance to ride along on a river trip, or to write an article. I welcome these opportunities to enlighten the general public about the magic and joys of geologic thinking.

The Grand Canyon of the Yellowstone River is carved in volcanic rocks erupted about 640,000 years ago

I was recently contacted by Jim and Barbara Cowlin, who have a passion for US Highway 89, also known as the Park to Park Highway since it connects seven different National Parks (as well as many more National Monuments) between the Mexican and Canadian borders. Jim is a professional photographer and this site is one you should bookmark if you love this art form or Western scenery. They both have traveled the highway from one end to the other and know it well. They offer tips on things to see, side excursions, and places to visit.

They asked me to write a short post on volcanism near Yellowstone. I was fortunate to spend much time there about ten years ago, becoming familiar with many of the geologic features there. You can read my posting on Yellowstone volcanism here.  The introductory article for the US Highway 89 web site can be read here. I have also written geologic summaries of the three geographic provinces that US Highway 89 traverses. The Basin and Range article can be read here. The Colorado Plateau article is found at this link. And the article describing the geology of the Rocky Mountain Province is here. The Cowlin's are to be commended for celebrating the beauty and heritage of this incredible western highway.

Happy traveling!

"Game Changing" Images From The Mars Rover Curiosity

I thought for sure that the national airwaves would be buzzing endlessly about the discovery of river-worn pebbles by the Mars rover Curiosity on September 27. The announcement was made to the usual temporary fanfare and faded away predictably in unceremonious fashion. I guess that is the price we pay to live in this info-charged, "what-have-you-done-for-me-lately" world. If our attention spans get any shorter there will be nothing in the solar system that amazes us.

Well not for this old rock-hound, who remains duly impressed a full two weeks after the announcement was publicized. This truly is the smoking gun for the former presence of running water on Mars. Previous studies have shown that minute amounts of water still reside near the Martian poles and perhaps beneath the Martian surface elsewhere. But this is verifiable and visible evidence that rivers once ran on Mars! (A River Ran On It).

In this posting, I include images released by NASA with their own captions beautifully describing each one (I modified the captions slightly to reduce redundancy). The full story as posted on the NASA web site can be read and accessed here. Wow! This is really impressive. Stay tuned to NASA and this blog for more fantastic discoveries from Mars.

Where Water Flowed Downslope

This image shows the topography, with shading added, around the area where the rover Curiosity landed on Aug. 5 PDT (Aug. 6 EDT). Higher elevations are colored in red, with cooler colors indicating transitions downslope to lower elevations. The black oval indicates the targeted landing area for the rover known as the "landing ellipse," and the cross shows where the rover actually landed.

An alluvial fan, or fan-shaped deposit where debris spreads out downslope, has been highlighted in lighter colors for better viewing. On Earth, alluvial fans often are formed by water flowing downslope. New observations from Curiosity of rounded pebbles embedded with rocky outcrops provide concrete evidence that water did flow in this region on Mars, creating the alluvial fan. Water carrying the pebbly material is thought to have streamed downslope extending the alluvial fan, at least occasionally, to where the rover now sits studying its ancient history.

Remnants of Ancient Streambed on Mars

NASA's Curiosity rover found evidence for an ancient, flowing stream on Mars at a few sites, including the rock outcrop pictured here, which the science team has named "Hottah" after Hottah Lake in Canada’s Northwest Territories. It may look like a broken sidewalk, but this geological feature on Mars is actually exposed bedrock made up of smaller fragments cemented together, or what geologists call a sedimentary conglomerate. Scientists theorize that the bedrock was disrupted in the past, giving it the titled angle, most likely via impacts from meteorites.

The key evidence for the ancient stream comes from the size and rounded shape of the gravel in and around the bedrock. Hottah has pieces of gravel embedded in it, called clasts, up to a couple inches (few centimeters) in size and located within a matrix of sand-sized material. Some of the clasts are round in shape, leading the science team to conclude they were transported by a vigorous flow of water. The grains are too large to have been moved by wind. This image mosaic was taken by Curiosity's 100-millimeter Mastcam telephoto lens on its 39th Martian day, or sol, of the mission (Sept. 14, 2012 PDT/Sept. 15 GMT).

Close-up view of Hottah

A close-up view of Hottah reveals more details in the outcrop. Broken surfaces of the outcrop have rounded, gravel clasts, such as the one circled in white, which is about 1.2 inches (3 centimeters) across. Erosion of the outcrop results in gravel clasts that protrude from the outcrop and ultimately fall onto the ground, creating the gravel pile at left.

Link to a Watery Past

In this image a rock outcrop called Link pops out from a Martian surface that is elsewhere blanketed by reddish-brown dust. The fractured Link outcrop has blocks of exposed, clean surfaces. Rounded gravel fragments, or clasts, up to a couple inches in size are in a matrix of white material. Many gravel-sized rocks have eroded out of the outcrop onto the surface, particularly in the left portion of the frame. The outcrop characteristics are consistent with a sedimentary conglomerate, or a rock that was formed by the deposition of water and is composed of many smaller rounded rocks cemented together. Water transport is the only process capable of producing the rounded shape of clasts of this size. The name Link is derived from a significant rock formation in the Northwest Territories of Canada, where there is also a lake with the same name.

Scientists enhanced the color in this version to show the Martian scene as it would appear under the lighting conditions we have on Earth, which helps in analyzing the terrain. Image credit: NASA/JPL-Caltech/MSSS

Rock Outcrops on Mars and Earth

This set of images compares the Link outcrop of rocks on Mars (left) with similar rocks seen on Earth (right). The image of Link, obtained by NASA's Curiosity rover, shows rounded gravel fragments, or clasts, up to a couple inches (few centimeters), within the rock outcrop. Erosion of the outcrop results in gravel clasts that fall onto the ground, creating the gravel pile at left. The outcrop characteristics are consistent with a sedimentary conglomerate, or a rock that was formed by the deposition of water and is composed of many smaller rounded rocks cemented together. A typical Earth example of sedimentary conglomerate formed of gravel fragments in a stream is shown on the right.

An annotated version of the image highlights a piece of gravel that is about 0.4 inches (1 centimeter) across. It was selected as an example of coarse size and rounded shape. Rounded grains (of any size) occur by abrasion in sediment transport, by wind or water, when the grains bounce against each other. Gravel fragments are too large to be transported by wind. At this size, scientists know the rounding occurred in water transport in a stream.

Scientists enhanced the color in the Mars image to show the scene as it would appear under the lighting conditions we have on Earth, which helps in analyzing the terrain. The Link outcrop was imaged with the 100-millimeter Mast Camera on Sept. 2, 2012, which was the 27th sol, or Martian day of operations. Image credit: NASA/JPL-Caltech/MSSS and PSI

Flash Flood Videos from the 2012 Grand Canyon Monsoon

The monsoon season of 2012 will go down as one of the most active in recent memory. It seems that here in Flagstaff we were constantly under rain showers from July 4th to September 12th. There were many fantastic floods that also occurred in the Grand Canyon and I include some phenomenal links to videos of these events in this posting. Before that however, you may want to refer back to some pictures I posted of two debris piles that were deposited catastrophically at the mouths of Red Canyon and National Canyon. These were taken on my 10-Day Geology Rafting trip from September 12 to 21. You can refer to that posting and view the pictures here.

Some video was captured of the big National Canyon flood, which occurred on July 14, 2012. It is courtesy of Joe Clark, a boatman for Western River Expeditions. That video can be viewed here. And there is a second video here that shows how the floodwater entered the Colorado as a foamy mess. These are amazing images. I have heard estimates that National Canyon had a peak flow of about 15,000 cubic feet per second, making it almost as large as the Colorado River on that day.

 Another flood occurred very close to National Canyon but on the other side of the river at Fern Glen Canyon on August 20th, 2012. A river trip apparently had stopped to hike at Fern Glen but on the way up into the canyon, the extreme runoff filled the canyon bottom. That video can be watched here. I have heard no estimates of the discharge on this flood but it is quite a bit smaller that what came down National. Anyone who would have been caught in the narrows in Fern Glen Canyon however, would not have cared one bit if this flood was somewhat smaller - the amount of runoff is impressive and deadly.

 Finally, there is this footage from some monsoon waterfalls that developed quite rapidly in a downpour that occurred in Marble Canyon in July, specifically at Redwall Cavern. A party of rafters had stopped in the large cavern when the skies let loose and they watched the rain fall in sheets which produced significant waterfalls of brown water into the river. Watch the footage here. Be sure to watch it through to the end - the rain gets stronger and the amount of water pouring into the river gets extreme. (You can also look at waterfall footage from Redwall Cavern from 2008 here).

Flash floods are common in landscapes that contain widespread bare rock exposures with few soils. They are the mechanism by which the canyons are created and facilitate the deep dissection that makes the Colorado Plateau and Grand Canyon so wonderful. With the advent of cheap but high quality electronics, more of these events are now visible to us. Watching the majesty and power of these events stirs the soul.

Addendum - 12/12/12: I became aware of this footage of the Red Canyon flood at Hance Rapid today! Here it is.

How The Earth Was Made

See a clip of my part in the History Channel's production, "How The Earth Was Made" here at this link.

Arizona Daily Sun Article on the New Edition of Carving Grand Canyon

To read an article on the new edition of my book "Carving Grand Canyon" in the local Flagstaff newspaper, see the link here.

Images From My 2012 10-Day Geology Rafting Trip

Wow! I just concluded another great 10-day geology rafting trip in Grand Canyon. The trips just keep getting better and better. I'm off on another Grand Canyon adventure soon, this time on a Rim to Rim hike with the Grand Canyon Field Institute. But I thought I would at least post some of the pictures from the rafting trip. Highlights include seeing some brand new deposits from the intense runoff events that occurred during the summer monsoon. Look at these below!

I didn't take any pictures on the trip until river mile 76 at Hance Rapid, where a large debris flow entered the Colorado River in August.

The rock in the middle of the picture used to sit out in the channel of the river. But the new debris flow constructed a rocky pathway so that it is now part of the left bank.

New debris near the river's edge.

Looking upstream in Red Canyon where the debris flow originated.

While standing on the new debris fan, we got an excellent view of the Hance Rapid dike cutting across beds of the Hakatai Shale, a Precambrian red bed deposit of the Grand Canyon Supergroup.This is likely the unit that failed in the monsoon rain causing a cliff of overlying Shinumo Quartzite to collapse.

The vast majority of the boulders are Shinumo Quartzite suggesting that the debris was let loose close to the river and not within Paleozoic rocks up higher in the canyon walls.

Cruising through the Upper Granite Gorge above Phantom Ranch.

We talked a lot about metamorphic foliation, displayed vividly here.

Pt. Sublime on the North Rim of the canyon. Helen and I visited this viewpoint just three weeks previous to the river trip and I include a view from the point below, that looks back to this point on the river.

Looking back at the river from Pt. Sublime on August 12, 2012

A bighorn ram wanted to check us out at one lunch stop near Elves Chasm.

Evening on the river....

A time to reflect on the days sights....

A typical river camp. I did not set up a tent even once.

Barbara getting close to the Great Unconformity in Blacktail Canyon at river mile 121.

This years flooding left a large pool of clear water at the base of the chockstone cliff

A view downstream near Stone Creek of the angular unconformity that exists between the Tapeats Sandstone and the Grand Canyon Supergroup rocks. Can you see it?

If not, here is a close-up with all of the layers labeled. The yellow line represents the angular unconformity where more than half a billion years of earth history is missing in the rocks.

Near Tapeats Creek, there are huge landslide deposits that have filled former channels of the Colorado River. Can you spot the one here?

If not, here is the same photo with all of the labels.

Sunrise on the 6th morning below Deer Creek.

A quiet camp scene.

A huge fan of debris came down National Canyon at river mile 166 in July. The new material extends all the way to the rivers edge.

Wow! This view is of the upstream portion of the fan.

Here is a view of the downstream portion of the fan. The entire beach was inundated with rocky debris and rumors of 15,000 cfs coming down National Canyon are floating around.

No place to be in a flood.

The Grand Canyon

Alan and Carol

Cynthia and Tim

A volcanic dike cuts through the Bright Angel Shale just upstream from Lava Falls at river mile 179

Lava Falls as it looked on the morning of September 19 at just over 8,000 cfs.

Ready for the run of the Falls. Brandon did a great job getting us through.

I've never stopped at river mile 214 where the Bundy jars are located. The Bundy's are a local ranching family up on the Shivwits Plateau.

The jars are in an overhang of Tapeats Sandstone in front of numerous mescal pits. Here the group surrounds one of the pits.

Ripple marks in the sandtone

The summer rains really watered the desert in western Grand Canyon and I have rarely seen it so lush.

Green, green, green!

A lava remnant stands tall along a desert trail.

Mojave Desert vegetation in the western Grand Canyon.

Boatmen call this place "alien eggs."

Joe examines one close up. They appeared to be limestone blocks that were rounded and polished, then stained red by iron oxide.

This lava remnant is part of the Black Ledge flow that extends 84 miles down the channel of the Colorado River.

From the mouth of Three Springs Canyon at river mile 215.

Ocotillo

Looking downstream along the Colorado River at Three Springs Canyon.

Aliona or rounded pinwheel carpeting the desert floor.

Our final attraction stop was at Travertine Canyon at river mile 229.

The grotto is spectacular.

Final shot of our group.

Brandon and Tom, our crew for the trip.