Thursday, March 19, 2026

Explore the Pacific Northwest and Northern Rocky Mountains with Geotripper! June 18-July 2, 2026

Grand Tetons National Park, Wyoming
Be forewarned. This post is a TRAP! It is designed to draw you in, weaken your defenses, and cause you to do something different than everyday life. Warning given...

Have you ever dreamed of hitting the open road and finally seeing those places you've dreamed about, but haven't acted on that dream yet? What if you found out about an excursion that doesn't just tour, but allows you to learn the geology and history of those wild places? A tour on which you can even earn college credit? AND, a tour that is affordable? Maybe this is the one...
Mt. Shasta, a Cascade volcano in northern California
From June 18-July 2, 2026, the geology and anthropology departments of Modesto Junior College will be conducting a field studies course (Geology 192/Anthropology 192) in the Pacific Northwest and Northern Rocky Mountains. It will be a six semester unit course designed for our community college clientele: first year geology/anthropology majors, potential majors, as well as community members (especially teachers) and life-long learners interested in geology, archaeology, and natural history. We will develop the necessary geological/anthropology background prior to and in the early days of the trip, so people of all backgrounds are encouraged to attend. The total cost is $850 which will include all food, camp fees, entrance fees, transportation costs for the trip. The tuition cost for the six units of semester credit will be around $380 (out of state tuition is higher). The only additional costs should be for showers, laundry, books and other souvenirs, and junk food (we provide healthy food for the most part; if you want Twinkies you are on your own!). We will be camping each night, and the school provides the transportation (vans). The excellent meals are planned by our professional volunteer staff, and cooked by the participants under their watchful eyes.
Lava Tube in Lava Beds National Monument
What will you see and experience? On the 18th we'll leave MJC and drive north through the Great Valley of California and arrive at the south end of the Cascades Range. The huge edifice of Mt. Shasta looms over the north state at 14,163 feet, and still is potentially active. It last erupted in 1786. Depending on snow conditions, we'll climb to the 8,000 feet level at the old ski bowl and have a close look at the rock and ash deposits. We'll continue north and end the day at Lava Beds National Monument near the Oregon border. There will be chance to explore some lava tubes while we are there.
The view from Smith Rock State Park in Oregon
We drive through Oregon the next day, with possible stops at Crater Lake National Park and Newberry Crater (depending, once again, on snow conditions). Camp will be at Tumalo State Park. The following day we will explore Smith Rock State Park (above), Mt. Hood, and the Columbia River Gorge (if there is time we will climb Beacon Rock in the gorge). The third camp will be at Seaquest State Park at the foot of Mt. St. Helens in southern Washington.
Mt. St. Helens in Washington. It erupted in 1980 and 2004
The following day will be devoted to the exploration of Mt. St. Helens (weather allowing!). We'll then move on to the Pacific Coast and the temperate rainforests of Olympic National Park. We'll visit some tribal lands near the westernmost point of the lower 48 states and explore Hurricane Ridge at Olympic's north side. 

We'll then descend the eastern flank of the Cascades (including a close look at Mt. Rainier) and drive onto the Columbia River Plateau, a vast basalt plain that covers much of eastern Washington and Oregon. Camp will be at Sportsman's State Park in Yakima.
Dry Falls State Park in Washington. The floodwaters covered this entire landscape to a depth of 300 feet during the Spokane floods.
The next day we will view the evidence for vast floods that swept across the plateau during the Pleistocene ice ages. The discovery of these floods by J Harlan Bretz in the 1920s and the long road to acceptance of the hypothesis by the geological community is one of the great stories in the history of geology as a science. We'll have a look at the Channeled Scablands, Soap Lake, and Dry Falls as we travel east through Washington. We'll spend the night at Riverside State Park in Spokane, Washington.

We'll head through the copper mining districts of Idaho and into Montana where we'll see more evidence of the ice age floods. We'll drive east to Lewis and Clark Caverns and stay near Bozeman, Montana. We'll check out the Museum of the Rockies and move on to explore Yellowstone, America's oldest national park. We'll spend two days exploring this incredible park.
Yellowstone Falls in the Grand Canyon of the Yellowstone River
There is the Grand Canyon of Yellowstone, and a menagerie of incredible animals, including elk, bison, moose, bighorn sheep, and if we get really lucky, wolves.
Wolf near Norris Geyser Basin, Yellowstone National Park
Then there are geothermal features for which Yellowstone is so famous. Grand Prismatic Spring, for instance, and 70% of the world's geysers (there's lots more besides just Old Faithful!).
Grand Prismatic Spring, Yellowstone National Park
We'll then head south and spend two days at Grand Tetons National Park with time for some spectacular hikes. Then we start the road home with a drive through northern Nevada.
Big Geyser (not Old Faithful!) in Lower Basin, Yellowstone National Park

It's hard to describe the wonders that exist across the Pacific Northwest and Northern Rocky Mountains without getting an overwhelming urge to get up and leave right away. If you are in the Modesto region, we are having our first information meeting on Monday, March 23 in the Science Community Center on the west campus of the Modesto Junior College at 7 PM in SCC 325 (attendance is not mandatory to go on the trip). We hope you will join us!


Tuesday, March 3, 2026

I Got Up at 3am So You Wouldn't Have To: The Last Lunar Eclipse Before 2029


I didn't really feel like it, but lunar eclipses are dramatic, and this was the last one to take place until 2029, so I got up a few times between 2am and 4am to snap a few shots of the event
Lunar eclipses happen when the Earth moves in-between the Sun and the Moon, and casts a shadow across the face of the Moon. The shadow is spherical, by the way, so flat-earthers can re-examine their belief system.
The darkened portion of the lunar disk is much darker than the lit portion, and was hard to focus on with my limited photographic equipment.
The red color is due to the red edge of the visible light spectrum being bent through the Earth's atmosphere. It could be kind of cool to see a lunar eclipse from the Moon itself. I assume the Earth would have a red ring around it.
I would have stayed up longer, but my camera (based on previous experience) probably wouldn't focus right, and I had to work today.
One cool aspect of lunar eclipses is that many more stars appear during totality. My phone couldn't focus so much on the Moon, but did show how many stars were visible near the Moon that wouldn't otherwise be visible.


 

Friday, December 26, 2025

Revisiting the Wrightwood Mudflows of Ages Past: That Slope Won't Be a Problem Will It?

Like many others, I've been astonished by the storms of the last few days and the effects across all of California and the Pacific Northwest. It's not quite over, and if you are in one of the danger zones, listen to the emergency workers. They know what they are doing. 

I've been especially attentive to the stories coming out of Wrightwood in Southern California. It's been a well-known trouble spot for many years. Back in 2013, I paid a visit and had a look at the geological conditions that have plagued the area. What follows was posted in March of 2013.

You learn something new everyday. At least I hope you do. I learned something astounding revealed by satellite imagery of the Mojave Desert.

We were headed home a week or two ago, and were taking a "short cut" along the San Andreas fault in Lone Pine Canyon and through the town of Wrightwood. That's right, "through" the town. The village is built on top of the San Andreas! But that's not what I learned. I've known of the close proximity of the fault and the town for years.

It had something to do with the town's other famous natural hazard: the Wrightwood mudflow. There is a slope south of the town heading at an elevation of more than 8,000 feet composed of deeply weathered and crushed Pelona Schist. As can be seen in the picture below, the slope is so steep that trees and shrubs can't gain a roothold, and failures are constant, especially during the spring snowmelt and during heavy rainstorms.
The Pelona schist formed in the accretionary wedge of the subduction zone that lay off the California coast during the Mesozoic Era, and as such may be similar to the Franciscan Complex farther to the north. It is an attractive muscovite mica quartz albite schist in hand samples, but it doesn't do well on steep slopes.
We passed several channels that were clearly designed to send the flows through town without causing further damage.
In May of 1941, just over a million cubic yards of mud and boulders flowed down Heath Canyon and into the town of Wrightwood, damaging and burying a number of structures. No deaths or injuries were reported. The immediate cause was the rapid melting and runoff of the heavy snowpack during a period of unseasonably warm temperatures. Surges of mud continued for a week. Other damaging mudflows occurred in 1969 and 2004.

This basic information was something I was made aware of during my first geology class at Chaffey College many years ago. One thing I didn't know is that the mud passed beyond Wrightwood and continued for 15 miles into the adjacent Mojave Desert. The flow traveled a vertical mile, from 8,000 feet to 3,000 feet.
Source: http://www.wrightwoodcalif.com/mudflows/53SharpRptMud.pdf
The other thing I didn't know is that Wrightwood mudflow has been active for at least five centuries, and that the results of the slide are clearly visible from space! Check out the Google earth image below and note the dark gray alluvial fan just right of center. The gray colored fan is composed of the Pelona schist, which is much darker than the sediments in adjacent fans which contain more granitic rock.
Source: http://epod.usra.edu/blog/2009/06/heath-canyon-landslide.html

The town of Wrightwood is easy to visit. It is just off of Highway 138 west of Cajon Pass on the Angeles Crest Highway. As noted previously, the town sits on the San Andreas fault, so the locality is a good spot to visit and reflect on the many hazards that must be dealt with when one decides to take up residence in the state. For more information on the mudflow, check out this state report: http://www.wrightwoodcalif.com/mudflows/79MortonMudRpt.pdf

The Other California is my on again-off again blog series on the geologically interesting places in our fair state that don't show up on the tourist guides.

Monday, October 13, 2025

Why did the Road Cross the San Andreas Fault? 23 Years of Geologic Change (a new Update)

2002
I've been leading geology field studies trips to lots of places in the American West for 37 years and started to take digital pictures in 2001. I sometimes struggle to find new things to photograph when I visit a place for the 37th time, but in some cases it is not a problem. There are geologic changes that happen on a yearly basis, and with twenty-three years of photos (minus two due to Covid), the changes become obvious. This is a continuing update from a post in 2013, and I'll probably continue updating for the foreseeable future.
2004
Highway 25 in the California Coast Ranges connects the town of Hollister with the access road to Pinnacles National Park (formerly Pinnacles National Monument). Along the way the highway crosses the San Andreas fault in a section where the fault creeps an inch or so each year (36°35'54.27"N, 121°11'40.19"W). Most years we've stopped to have a look at the effect the movement has on the pavement. In 2002 and 2004, the damage was obvious.
2008
By 2008 someone had patched the road, and no fault motion was evident.
2009
Little damage was evident in 2009 either. But by 2010 cracks had begun to appear as the fault stressed the pavement.
2010
The fact that the fault creeps in this region is a good thing. It means that stress is not building along the fault surface, but instead is being released gradually. The sections of the fault to the north and south of the creeping section are locked by friction, and are building up the ominous stress that will eventually produce quakes with magnitudes in the range of 7.5 to 8.0. The quakes are coming and we need to be as prepared as possible.
2012
By 2012, the road had been completely repaved, and  yet the shearing was already evident.
2013
It became even more pronounced by 2013 and in 2014. Just by chance, the person working as a scale was the same individual as in 2004.
2014

In 2015 the fractures were moderately larger. They'll need to start thinking of road repairs before long.
2015
In 2016 Laura once again provided scale, as she did in 2014 and 2004.
2016
Here in 2017, long-time trip volunteer Mary provides scale. The cracks in the road are just a bit larger, but they didn't look appreciably different than the previous year except for a twist (pun intended).

2017
On Dec. 2, 2018, the break to my eye seems more continuous. It's now been six years since the road was completely repaved.
2018

Last year the paint was deformed (twisted), but not split (below).
2017
The offset paint strip reminds me of illustrations of elastic rebound theory, the idea that stress builds up on a fault line over time. In that model, the land on either side of the fault is distorted over time until the frictional resistance is overcome and the rock snaps back to its original shape. That won't be happening with the paint. Last year in 2017 I said "if they don't repair the road (as they often do; see above), it will probably show a clear break by next year." Here's what transpired:

First, a close-up on 2017's center stripe...
2017
And here's how it looked on Sunday, Dec. 2, 2018:
2018
As predicted, the break in the paint is complete...

In 2019 (those last few halcyon days before Covid) long-time volunteer Paul provided scale (he has been assisting MJC with field trips for 25 years!). The crack continues to grow, and I wouldn't have been surprised if it was patched by next year.
 The paint on the center strip is split even more.
November 2019
And then Covid happened and for a few years we were not able to conduct our field studies classes. In 2022 we made a return visit with our students and here is the then-current condition of the highway. It didn't appear that any repairs have been conducted yet. Our host is once again Laura, who was with us back in 2004 and subsequent years!
November 2022
Fault creep is not a constant. I didn't see a whole lot of change over the last three years, although I didn't get as many close-up shots. Here's a closer look with Paul, our other long-time volunteer. What do you see that is different?
November 2022
In 2023 the road continued to become more deformed, and the passing traffic produced an audible thump as it passed over the fault. Our host since 2004, Laura, was not able to join us, so her husband Ryan stood in her place.
Oct. 28, 2023
And then it was 2024, October 12 to be specific. Once again our guide is Laura, who has assisted on these trips since at least 2004. The crack continues with minor changes, and it may be overdue for another repaving job.
October 12, 2024
They may not have repaved the highway, but they did in fact repaint the center line, which obscures about two inches of right lateral offset.
And that brings us to 2025 (October 11). Our long-time volunteers weren't on the trip this year, so River and Makayla jumped in to provide scale. 

Oct. 11, 2025
The road hasn't been repaved since 2012, and the crack is continuing to slip and fracture. The pavement at the road median has fragmented, and completely repainted which hides the offset a bit.
These little changes that happen at a rate visible in human lifetimes add up to huge changes when multiplied by thousands or millions of years. The nearby eroded volcano of Pinnacles National Park has been displaced 195 miles (315 kilometers) in the last 20 million years or so by movement along the San Andreas.

How will it look next year?



Thursday, October 9, 2025

The Things We Don't Think About: The Aftermath of a Major Earthquake from a Great Valley Perspective

The Great Shakeout is planned for Oct. 16, 2025, at 10:16 AM. 

Source: U.S. Geological Survey

We Californians live in earthquake country. The state is riddled with fault zones, and many of them are more than capable of producing damaging quakes. Some of the state's biggest cities are built on or adjacent to active faults, and much attention has been devoted to the probabilities and outcomes of major quakes in those cities, with predictions of possibly thousands of fatalities and hundreds of thousands of injuries. The dystopian models predict legions of newly homeless people, and badly disrupted services and ruptured transportation lines. It's grim reading. Government organizations are cognizant of the danger, and billions of dollars have been spent on preparing for such quakes, including reinforcement of vulnerable infrastructure, and educating the population about the dangers.

But what about the outlying regions of the state, somewhat removed from the most damaging aspects of the coming quakes? What is life going to be like after the fabled "BIG ONE" strikes? That's what I want to write about, since that's where I and many of my friends and acquaintances live. What's going to happen to us here in the Great Valley, in towns like Modesto and Turlock?

Source: Earthquake Country Alliance
First, the good news: the threat of severe shaking is considerably less in much of the Great Valley, with certain important exceptions (see the map above). Much of the valley floor is located tens of miles east of the most dangerous faults like the Hayward or San Andreas. The expected shaking will lead to some damage, but for the most part, buildings and infrastructure (roads, rails, pipelines) should fare reasonably well.

Liquefaction damage in San Francisco, 1906. Source: USGS
The sediments of the Great Valley can have a tendency towards liquefaction, the phenomenon of turning into "quicksand" during shaking, causing buildings to partially sink and severing buried pipelines and cables. This is especially true along river floodplains, including the San Joaquin River and within the Sacramento Delta (citizens of Tracy and Patterson need to take special note). This is the result of a shallow groundwater table. Luckily, much of middle and eastern parts of the valley have a deep water table, and liquefaction is less likely in the dry sediments.

Here's what happened last time in 1906. Source: Wikipedia open domain
So...let's imagine the worst has happened. A 7.8 magnitude earthquake has struck in the Bay Area, and devastation is widespread throughout the region. Hundreds, perhaps even several thousand people have died, and many tens of thousands have been injured. There are widespread power outages, and pipelines have been broken in many places, leaving many without water. Streets and freeways are blocked by debris and collapsed bridges, and emergency services are overwhelmed. Several hundred thousand homes have been rendered uninhabitable. Fires are burning in many areas. Dozens of aftershocks, some as great as magnitude 6, cause additional damage and panic. Life has taken a catastrophic turn, and millions are affected in profound ways. There's much uncertainty now as the population faces concerns of water, food, shelter, and danger from further seismic activity. It's the time that we find out if years of planning and preparation have been effective. Emergency services swing into action.

Agricultural fields in the western part of the Great Valley near Patterson (my photo)
Meanwhile in Modesto the situation is quite different. Although heavy shaking is felt by literally everyone, the sensation is more of a rolling motion, not the fierce movements that brought down bridges and unreinforced buildings in the Bay Area. Some chimneys are shaken loose, cracks occur in some older buildings, and items fall from shelves throughout the city. Some people are hurt by falling debris, but deaths are probably few in number. Electricity goes out due to the disruption statewide to the state power grid. The outages mean that water pressure can't be maintained, so faucets are dry throughout the city. Cell phone towers may have been damaged, and those that aren't are soon overwhelmed by phone traffic (it has been said that social media spreads earthquake news faster than the seismic waves themselves).

In the immediate aftermath, life has become inconvenient. The power is out, the water is off, sirens are blaring all over the city, but for the most part it's a time of waiting. Waiting for the power to come back on, the water to flow, and the phones to start ringing again. It could take days, maybe even a week or two. All things considered, for most of us it is an interruption.

But there are larger consequences with this incredible earthquake in places like Modesto. 

Emergency services will be largely unavailable in town. Ambulance and EMT crews will pressed into service in the Bay Area, and local hospitals will be filled to overflowing with the injured (many Bay Area hospitals will be overwhelmed and maybe even unusable). The same will be true of firefighters and perhaps law enforcement personnel as well.

Many Bay Area freeways will be impassable, but emergency supplies must still reach the region. Interstate 5 may still be open, but Highway 99 will become a more critical lifeline than it is today. Traffic will increase. With refinery production in the Bay Area interrupted, gasoline will become scarce. Expect huge price increases and severe shortages at filling stations across the state.

As much as I don't like to think about it, most people will not have prepared for the eventuality of earthquakes. They won't have supplies of water and food and other materials on hand, so local store shelves will quickly empty out, and with a severely disrupted supply chain, those shelves will not quickly refill. There will be shortages. Restaurants and fast-food outlets will likely be closed for extended periods.

It's a given that our local community, our officials and authorities and our relatively undamaged infrastructure will be an important part of recovery efforts in Central California. My own institution, Modesto Junior College, has plans in place for sheltering and supporting thousands of people made homeless by the quake. They will likely be our guests for weeks or months. Many other schools and institutions have similar plans. The influx of hurting and anxious people will no doubt place a huge strain on our infrastructure, and I fervently hope we can rise to the occasion, just as I would hope that others will look upon us with compassion in case of catastrophic flooding in our valley (that's an entirely different subject for a future blog).

It's going to be a challenging time, and we can respond to it in two ways:

We can ignore the entire possibility of large earthquakes, and go on living our lives as if nothing will ever happen. That is frankly what most of us are doing now. It's seemingly worked well so far. We are of course living among fault zones that have been building up stress for a century or two, and they are all capable of producing damaging earthquakes right now. I don't think of this as a good choice. Not at all.

An aerial view of a devastated San Francisco shortly after the earthquake in 1906 (USGS)
Or...we could prepare. Take the possibility of a major quake with the intensity you would give it if you knew it was happening a few days. Gather supplies of food, water, and first aid supplies right now, before the shelves emptied by desperate quake refugees and victims. To the extent possible, keep your gas tank closer to full than empty. Have emergency go-bags ready in case you have to evacuate your home or community. Develop an emergency plan for your family, and maybe your neighborhood. Learn about the known seismic hazards in the place where you live. Check out my previous blog for more links and ideas. There is a great resource centered on Central California published by the California Earthquake Authority, the Earthquake Country Alliance, and the California Governor's Office of Emergency Services, that can be reached by clicking here.

It would be nice if we could know in advance that a quake is about to hit, but we don't. Since that's the case, we should be as ready as possible.

Source: USGS