41st Anniversary of the Eruption of Mt. St. Helens: It Still Matters and So Does Science

It is the 41st anniversary of the eruption of the St. Helens volcano and as I think of those days, I realize that even though a majority of the population wasn't even alive at the time, the volcano still matters. Not because of the potential for future eruptions (although that remains a distinct possibility), but because of the way we process and deal with the natural hazards that we all face, no matter where we live. This is kind of a recurring post that I've modified over the years.


When the volcano began rumbling and sending ash into the atmosphere, we had only a few avenues to get information, mainly television news, radio, and newspapers. I think now how limiting these sources were compared to the nearly instantaneous delivery of news over the internet in the present day. We can look up earthquakes just moments after they happen, and webcams allow us to monitor volcanoes around the world in real time. There is both good and bad in this profound change. There were terrible sources of news in those olden days, like the Weekly World News or the National Enquirer, but they pale in comparison to the sewage found on the internet today. Back then, national news outlets and newspapers practiced careful journalism in most instances, but it often seems today that the only reward for excellence and honesty in reporting is decreased ratings and falling revenues. To get attention in a crowded internet environment media outlets have to dress their stories as shiny objects and provide them with the worst possible clickbait titles. In the olden days we often had to wait impatiently for information about natural disasters, but the information that came through the media was more likely to be vetted and checked for accuracy. The journalistic filters today are completely gone in many media sources, and it can be difficult to distinguish between the trash and the truth.

There are so many conspiracy theories floating around today about natural disasters and potential disasters. The eruptions of Steamboat Geyser in Yellowstone National Park numerous times after years of quiescence caused a blizzard of posts on the internet pondering whether Yellowstone has been disturbed and may blow as a "supervolcano" eruption soon (and we'll all die). The same has happened after a number of recent small earthquakes. But a reading of the reality-based data says that Yellowstone caldera has not had a lava flow or eruption of any kind in 70,000 years, and no knowledgeable geologist sees any evidence of precursors to any new eruptions. A few years back, an earthquake and an internet video of a group of bison running "away" from Yellowstone caused the same kind of internet speculation (it turns out the bison were running towards the caldera).




Of course it is true that the Yellowstone caldera was born in one of the most colossal eruptions ever recorded. Learning the story of the eruption of the Huckleberry Tuff is fascinating. It brings an entirely new appreciation of the incredible scenery to be observed in a place that contains 70% of all the world's geysers. It should be enough. But there are so many individuals out there who would like to make a buck by scaring people needlessly. And there are too many gullible and ignorant people out there who can't pick rational accounts out of the confusing mix of conspiracy theories that exist on the internet.




And then there is the Big Island of Hawai'i. There were some serious and tragic things going on in 2018 when the longest eruption in recorded history reached a climax. The activity endangered lives and destroyed homes as Kilauea underwent major changes from the "norm" of the eruptions that had been ongoing for the last 35 years. One of the truly awesome sights I have ever seen was the collapse of a portion of the Kilauea Caldera into a gigantic pit that reached a depth of 1,800 feet. It stabilized for a year or so, even forming a lake (of water) at the bottom, but then a few months ago the eruptions started again, filling the pit with 700 feet of roiling molten basalt. 

The U.S. Geological Survey and Hawaiian civil defense authorities did a pretty good job of providing up-to-date information about the latest activity, but that didn't stop all kinds of stories from popping up on the internet about the "Ring of Fire" which has nothing at all to do with Hawai'i. It was just too easy to pick up stories of eruptions in Alaska and Indonesia and think there was a pattern of increasing volcanism or earthquake activity (OMG, a magnitude 6 quake in the Kermadec Islands and an eruption at Mt. Cleveland in Alaska! It's a pattern and therefore Seattle will fall into the sea very soon!). The problem is one of perspective: if you had signed up for earthquake notifications and volcano advisories from the USGS or other geologic research institutions, you would have realized that these things happen all the time, and that a cluster of events is not unusual.

It's one thing to make up stories about normal volcanic activity to scare people. One can argue that they are ultimately harmless because the eruptions aren't actually taking place or hurting anyone. But there are real-world consequences of ignoring journalistic standards. Many of those who make their money with false headlines about such things will also traffic in climate change denial. When science becomes a matter of believing whatever one wishes, the very real problem of global warming becomes just another "scare" story, and the alarm bells being sounded by climate scientists become just more noise in an internet full of noise. But the predicted real-world consequences are happening now, and action is needed to counteract the changes or to stop them. But it has become too easy to ignore the problem because it is so incremental and slow-acting. It just can't compete with the shiny baubles and clickbait on the web.

People in Hawai'i mostly trusted the geologists who studied the volcanoes all their lives and thus made the correct decisions about evacuating homes and businesses. In the same way they trusted the seismologists when a tsunami threatened the islands in 2011 after the massive earthquake in Japan. No lives were lost when the tsunami hit because people had evacuated the low-lying areas. The wave surge was 8 feet deep in places and caused millions of dollars of damage. Many people could have been killed, but they accepted the authority of the scientists who predicted the timing and magnitude of the seismically induced waves.

There has been one characteristic about the natural disasters that I've described above. They were local events that profoundly changed lives, but in large and yet limited regions. When earthquakes and volcanic eruptions strike, survivors can turn to other regional state and national governments for support, since those entities were not so badly affected. Now we face a different set of natural disasters: those that affect the entire planet. Pandemics and climate change affect all of us. Witness the spread of the COVID-19 virus last year to literally every corner and every country of the planet in a matter of weeks.

Scientific experts have long predicted the emergence of dangerous new strains of viruses, and previous administrations used the best scientific minds to prepare for their inevitable arrival. But those administrations were replaced by one that denigrated scientific expertise and fired the experts who could have crafted an appropriate national response to the COVID-19 virus. And last year we saw the result: nearly 600,000 deaths in the U.S. with more to come, lack of critical medical supplies in the critical early months, and no coordinated federal response, even once vaccines became available. Even worse was a propaganda campaign that convinced people that the disease was not as bad as it clearly was, and worse still, that the vaccines were some kind of insidious plot. Other countries listened to their scientists and saved countless lives. I thank the heavens that the country ultimately elected an administration that is being guided for the most part by science in their decision-making processes.

And that's why the Mt. St. Helens eruption of 1980 matters today. Scientific expertise matters. The pandemic (and others to come) will be a continuing problem in our interconnected world. Climate change is proving to be an even more profound danger to society than any virus, earthquake or volcanic eruption. We need people to give climate scientists the same kind of respect they give geologists when volcanoes are rumbling and smoking. They are the ones to listen to, not the hucksters on the internet who are out to make a buck, or trying to protect those industries that make their profits off of producing greenhouse gases. We seem to talk little these days about integrity and striving for excellence, but scientific researchers are among those who still have those traits. There are always exceptions, but I would trust a scientist over a politician every time (unless it is clear that the politician knows how to listen to a scientist).




There is a sign seen at some of the March For Science protests that have been happening around the country: "At the start of every disaster movie there's a scientist being ignored". Unfortunately, it is too true in real life as well.

This has been an abridged and updated version of my St. Helen eruption anniversary reflection.

Driving Through the Most Dangerous Plate Boundary in the World: Exploring the Underside of the Volcano

Quick, name the nation's oldest national park. I'll even give you a clue, it starts with 'y'. Did you guess Yellowstone? You are right. Did you guess Yosemite? You are also right, in a sense. Have you ever said "Yosemite" when you meant "Yellowstone"? I've done that plenty of times.

Castle and Beehive Geysers at Yellowstone National Park, Wyoming

Yellowstone technically is the nation's oldest national park, having been established in 1876 by an act of Congress, but Yosemite gains credit as the first "idea" of a permanently protected area when the valley was ceded to the state of California in 1864 by Abraham Lincoln.

Yosemite Falls from Swinging Bridge in Yosemite Valley

It's hard to think of two parks more different from each other. Yellowstone, with geysers, hot springs, bison, and moose. Yosemite, with huge vertical cliffs of granite and high alpine peaks. In Yosemite, the bears break into your car. In Yellowstone, the bears occasionally eat you.

Sunset in Yosemite from the Gateway View

The parks in one sense are very similar, and the similarity can be summed up in one word: "felsic". The word combines the mineral "feldspar", and the chemical "silica". These are the principle components of the plutonic rock granite, and the volcanic rock rhyolite. The rocks are identical in chemistry, but differ in origin: granite is silica-rich magma that cooled slowly deep in the crust, while rhyolite is a volcanic rock that often forms during extremely violent eruptions. The rocks of Yellowstone are mainly rhyolite and related rocks that formed in caldera eruptions, while those of Yosemite are principally granitic.

El Capitan in Yosemite Valley

We've reached the culmination of our journey across the most dangerous plate boundary in the world. As I've said before, it's not as dangerous today as it was in the Cretaceous period, but we can use these rocks to better understand subduction zones elsewhere in the world (it's a lot easier to study rocks at the surface than it is to drill miles into the crust, after all). We started the journey on the coast at Point Reyes National Seashore, worked our way along the Marin Peninsula, crossed into the Coast Ranges at Lick Observatory and Del Puerto Canyon, crossed the Great Valley, and worked our way up into the Sierra Nevada. And now we stand in Yosemite Valley, one of the most spectacular exposures of granitic rock on the planet.

Lassen Peak and Brokeoff Mountain, an active volcanic center in the southern Cascades Range

The subducting slab of oceanic crust in Cretaceous time was heated, and water that was released changed the melting point of the rocks at the base of the continental crust. The masses of molten rock worked their way up into the upper crust. Some of the rocks erupted at the surface as large Andean-style volcanoes, or as rhyolitic caldera eruptions. The chain of volcanic features is called a magmatic or volcanic arc. The surface may at times have even resembled Yellowstone, although present day Lassen Volcanic National Park or Mt. Shasta provides the best analog. But deep in the crust the rock was cooling slowly, developing into large crystals of quartz, feldspar and mica, then principle minerals of granite and related plutonic rocks.

El Capitan Granite, with gray-looking quartz crystals, white feldspar, and black biotite mica

Yosemite Valley provides a 3-D view of seven or eight different intrusions of granitic rock (for the purists, these include granite, granodiorite, tonalite, and diorite). Some of the rocks, principally the granite, stand out as bold cliffs like El Capitan and Cathedral Rocks. Other rocks were more easily eroded and formed recesses. The combination gives Yosemite the unique appearance that sets it apart from so many other glacially carved canyons.

When you visit Yosemite, take a moment to realize you are exploring the underside of massive volcanoes, quite literally Yellowstone or Lassen or Shasta from the inside out. It never ceases to amaze me that while the 3,000 foot cliffs are spectacular, they once were buried 4 or 5 miles deep in the crust, and that erosion has removed the missing rock (and filled our Great Valley in the process).

Half Dome from Washburn Point above Yosemite Valley

We've completed our exploration across the most dangerous boundary, and we are still alive! It's been several months with lots of interruptions, so you can expect a compilation of all the posts soon so you can get the whole story in one place. I hope you've enjoyed the journey!

A Convergence of Wonders: A Compilation

The trip I called the Convergence of Wonders was a combined geology and archaeology course that we conducted on June 15-30, 2011, in which we explored the Pacific Northwest and Northern Rocky Mountains. Our students and volunteers traveled more than 4,500 miles through regions that have been influenced by convergence along the Cascadia and related subduction zones, as well as a hot spot and continental divergence. Each day revealed stunning geological features and insights into the human occupation of the region over the last 13,000 years or more. This is a compilation of all of the blog entries I posted about the trip.



"Journeys in the Pacific Northwest" was the introductory post about the series, and provided some background about why we did the trip we did, and what our goals were. 





"Journeys in the Pacific Northwest, Day 1" was the story of the trip from home to our first camp at Lava Beds National Monument on the night of the full moon. En route, we explored the flanks of Mt. Shasta, the largest stratovolcano in the Cascades, and found out that a record snowpack and late spring was going to be a problem on this trip.

"Day 2, Lava Beds and Newberry Caldera" includes our exploration of Lava Beds National Monument, including the extensive lava tube system, an incredible panel of petroglyphs, and the site of the last war between the federal government and Native Americans in California. Late in the day, we visited an obsidian dome in Newberry caldera.

"Day 3, Crossing the Subduction Zone" chronicled our passage across the Cascades to the Washington coast at the mouth of the Columbia River at Cape Disappointment State Park. Smith Rock State Park in Oregon was an incredibly scenic view into the heart of a rhyolite caldera eruption, and our day ended looking pillow basalts from the floor of the Pacific Ocean floor. In between, we checked out an excavation taking place at Fort Vancouver.

"Day 4: Cape Disappointment and Real Disappointments" was the story of weather-related disappointments. The skies opened up throughout the day, including along the flanks of Mt. St. Helens, which was to be the centerpiece of our exploration. The mountain remained invisible in the clouds. The sun emerged, of course, but not until we were far beyond the crest of the Cascades and almost to our camp in Yakima.

"Day 5: In the Land of the Great Flood" was a narrative of our passage across the wastelands produced by a series of catastrophic floods that defy human imagination. At Dry Falls, we looked at canyons (the coulees) that were carved in a few days or weeks of remarkable "river" flows hundreds of feet deep. We also had a chance to see the Wenas Creek Mammoth at Central Washington University.

"Day 6: In the Land of the Great Draining" was an exploration of the lands where the floodwaters originated: glacial Lake Missoula. We traversed a barren valley (the Camas Prairie) where ripplemarks thirty feet high convinced many geologists of the occurrence of the Spokane Floods. We arrived in beautiful Glacier National Park at the end of the day, and were greeted with an incredible rainbow.

"Day 7: Of Time and Pressure in Glacier National Park" found us at the Canadian border where we started an exploration of Glacier National Park, at least the parts that were not still snowbound. We checked out the Lewis Overthrust, and examined the Proterozoic sedimentary rocks that make up much of the park.

"Day 8: Of Time, Pressure, and the Plain Truth" found us out on the Great Plains east of Glacier. We toured the Museum of the Plains Indians in Browning, and worked our way past numerous thrust sheets in Sun Canyon, where convergence pushed numerous fault slices over one another. We also checked out some exhibits on some of the most famous discoveries concerning dinosaurs at Choteau, Montana.

"Day 9: Into the Depths of the Crust, and of Time" discusses one of the most spectacular roads in America, the Beartooth Highway from Red Lodge to Yellowstone National Park. We also checked out the Stillwater Mine, where platinum and other rare minerals are produced. The outcrops we were traversing including some of the most ancient rocks on the continent.

"Day 10: Explorations of a Real Hot Spot" was just that...a tour of Yellowstone National Park, one of the crown jewels of the National Park System. We explored Yellowstone Falls, the Grand Canyon of the Yellowstone, Mammoth Hot Springs, and Norris Geyser Basin. The highlight for many of us was the witnessing of a wolf competing with a raven at a kill site.

"Day 11: The Orange Steam is OK, but the Blue Stuff Will Kill You" was a further exploration of Yellowstone, with visits to Grand Prismatic Hot Spring, and the famous geysers in Upper Basin (yeah, Old Faithful was spouting off, but I was watching Beehive). We ended the day in Grand Teton National Park.

"Day 12: A Richness of Geological Drama at Grand Teton (and Pelicans)" was a beautiful day of exploration in the Grand Tetons. We also checked out the Gros Ventre Slide, one of the most famous slope failures in the United States.

"Day 13: Hidden Treasures and Hazards on the Road in Western Wyoming" saw us beginning the long journey home. We checked out the Game Creek Archaeological Site and Fossil Butte National Monument, and saw a lot of sagebrush as we made our way south into Utah...

"Day 14: Treasures Discovered and Lost in Nine Mile Canyon" chronicles an expedition through seventy-mile long Nine Mile Canyon, a showcase of Fremont Culture artwork and archaeological sites. The canyon is also a site of controversy, as heavy industry is mining natural gas in the area, with profound effects in the canyon itself. Later in the day, we saw the Dinosaur Museum in Price, and ended the day searching for Topaz crystals in the western Utah desert.

"Day 15: We Go Underground in Great Basin" saw us making a 500 mile journey across the Basin and Range Province, with a stop at Great Basin National Park for a tour of Lehman Cave, and a stop at Garnet Hill, for, eh, garnets. A motorcycle accident caused us to arrive in a spooky camp at 11:00 PM.

"Day 16: Our Home Mountains, Giant Swimming Reptiles, and a Bunny" was our last day on the road. We checked out the bizarre Mesozoic creatures at Berlin-Ichthyosaur State Park in Nevada, Mono Lake in eastern California, and Yosemite National Park in our backyard before arriving at the end our journey.

See Glacier Before the Glaciers are Gone; See Yellowstone Before the Supervolcano Blows: Take a Geology Field Course This Summer

There was a time when the our national parks seemed like unchangeable icons and symbols. They were protected from development, they were reservoirs of intact ecosystems and clean water and air, and a family might have told stories of camping in the olden days of the 30's and 40's, and until recently one could reasonably expect to have a similar experience in the current era. Times are changing, however. Glaciers are disappearing from Glacier National Park, forests and wildlife are transforming in parks like Yellowstone and Yosemite as the climate warms, and some parks are becoming isolated islands in seas of urban development. Views in parks like Grand Canyon, Bryce Canyon and Sequoia are increasingly obscured by air pollution. Our orphaned parks, the state parks, are being being closed for lack of funding. Others face privatization. It's a shame that the best idea our country ever had is being in some ways abandoned. I would love to think that we are coming up with better ways of caring for our national and state treasures, but I am not optimistic. When budget cuts come, the parks get cut first.
I guess this is an odd way to extend an invitation! But if you live in the Modesto region (or are willing to make some major travel arrangements), we would like to invite you to travel with us on an exploration of some of our country's most precious places: the Pacific Northwest and the Northern Rocky Mountains. I'm working with our anthropology professor to offer a dyad class on the archaeology and geology of nine national parks and monuments (Lava Beds, Crater Lake, Newberry Crater, Mt. Rainier, Glacier, Yellowstone, Grand Tetons, Great Basin, Yosemite) as well as a multitude of state parks and other sites. And you can get three units of semester credit doing something interesting!
That's not to say there will be no work...you have to learn stuff, and demonstrate it too us! And it is a camping excursion, with all the possibilities of rain, snow, sun, wind and critters. On the other hand, there will be plenty of opportunities to hike, to see starlight skies and wonderful sunsets, and to have a multitude of unforgettable and unique experiences. If you are interested, see the press release below for more information. We are having an informational meeting on Monday if you live nearby. We can provide info by e-mail if you can't come to the meeting.

MJC offers new Geology and Archaeology summer field studies class

(Modesto, CA) — Modesto Junior College is offering a unique summer field studies course entitled Geology and Archaeology of the Pacific Northwest and Northern Rocky Mountains held June 15 to June 30, 2011. Anyone interested in enrolling in this special learning opportunity is invited to attend the orientation meeting on Monday, May 23 at 7 p.m. in Science 132 on East Campus.

The course will provide an exploration of Yellowstone, Crater Lake, Grand Tetons and Glacier National Parks, and Mount St. Helens and Lava Beds National Monuments. Participants will also have the chance to visit and discover some less familiar spots that provide evidence of the geological and human history of the region, including Great Basin National Park, Berlin-Ichthyosaur State Park, Fossil Butte National Monument, and Newberry Crater.

The new joint class is being taught by Professor of Anthropology Susan Kerr and Professor of Geology Garry Hayes and students will earn 3 semester units in either Geology 174 or Anthropology 174. A background is not required in either of these subjects. Basic principles will be developed prior to and during the course, and participation will benefit anyone interested in a career in teaching, park management and rangering, or science.

The group will camp in the parks and monuments and the $650 class fee includes all transportation, camping fees, park admission fees, and food. A registration fee of $26 per unit is additional, as are other applicable fees for those not already enrolled as an MJC student. Anyone wishing to register for the class who is not already enrolled as an MJC student must submit an application online at www.mjc.edu.

For additional information email Susan Kerr at kerrs@mjc.edu or Garry Hayes hayesg@mjc.edu or visit http://virtual.yosemite.cc.ca.us/ghayes/serv06.htm for a complete itinerary.