Back from the Cascades!

The trip to the Cascades Volcanoes has come and gone, and I think it was thoroughly successful. The trip’s purpose was to provide insight into and first-hand experience with one of the world’s most famous and accessible volcanic arcs. Some of the highlights included hikes at Lassen Peak, Crater Lake, Lava Butte, Mt. Rainier, and Mt. St. Helens. I managed to take a plethora of pictures (~200, which for me is a very high number for 10 days) and I’ll be uploading the best ones as soon as I get my hands on a Nikon USB cable, since mine has gone missing. I’ll write more in detail about the various stops as I post the pictures. For now, here’s brief information about the stops I just mentioned.

Lassen Peak: Our visit included stops at active fumaroles and boiling mudpots as well as a hike to the 10,462-foot summit. Lassen is the southernmost active Cascade Volcano, and is located in northern California. We made use of the Lost Creek campsite, and here’s a non-geologic point of interest: we saw a bear! That may not be very exciting to some of you, but when you consider that the most exotic animals I typically see in L.A. are errant housecats, I bet you’ll understand the novelty.

Crater Lake: This area is the remnant of a much larger prehistoric stratovolcano known as Mount Mazama. Its last eruption created its present distinctive geologic appearance, and rain and snowmelt are responsible for its vibrantly blue waters. The lake is too interesting to encapsulate without accompanying photos, so I’ll wait to elaborate on its features until I post some images.

Lava Butte: This tourist-friendly cinder cone situated in the northwest rift zone of Newberry Volcano is an easy way to introduce people to the effects of volcanism on the landscape. The complex it is part of is very interesting, and the cinder cone’s a`a lava flows reminded me entirely too much of my vaunted Ainapo Trail hike from last summer’s Hawaiian adventures. The major differences are that during this encounter with a`a I was not carrying ~60lbs of equipment and the hike only lasted 15 minutes!

Mt. Rainier: I have to say unequivocally that the Mt. Rainier hike was my favorite time on the trip. Those 5 miles were some of the most ethereal and memorable I’ve covered in my life, and the rapidly changing weather cycled through the vagaries of all four seasons in the span of a few hours. The heavily-glaciated and snow-capped summit of Rainier was wrapped in wispy clouds, and the resulting vision is not one I will soon forget. At any rate, this volcano will definitely receive more discussion.

Mt. St. Helens: For some people, a hike to the summit of Mt. St. Helens would be the high point of such a trip. Unfortunately, I was unable to complete the hike due to a flare-up of my kidney stone pain. My sudden illness that first manifested on the Waikupanaha flow fields last year was eventually diagnosed as a kidney stone. As I did not have insurance at the time of diagnosis, I’ve been unable to afford the removal procedure. What this means for purposes of this site is that I didn’t make it all the way up St. Helens. 75% of the way just doesn’t cut it, but for once in my life I actually turned back when my physical health demanded it. Anyway, I’ll make certain to discuss the St. Helens experience in greater detail when I post the pictures.

So, there you have the trip’s highlights in brief! Rest assured that the full discussions will be replete with the usual science and commentary that you’ve come to expect from VolcanoSummer. See you in a few days!

VolcanoSummer, v2.0 is up and running (I think)!

Hey everyone! It’s been a while since I last wrote anything here, but I had to return to my (semi) regular life as a geology graduate student at California State University – Los Angeles. However, school is now officially out for the summer, so you know what that means…VolcanoSummer, back in a whole new way. This year I’m not undertaking a single long stint of duty (capped nicely by a surprise oceanographic research trip), but rather I’ll be doing a bit of volcano-hopping as my time in grad school draws to a close.

On Monday (June 15th), I’m heading north to the volcanoes of the Cascade Range in California, Oregon, and Washington. It’s the culmination of a volcanology course I took this spring, and it should be a blast. Since I won’t have internet access while camping my way across these excellent volcanoes, I set up a VolcanoSummer Twitter account to keep the updates coming. If you want to follow my escapades directly on Twitter, the URL is twitter.com/volcanosummer.

So, what will I be doing up there? The answer is mostly just taking in the scenery and exploring some of the world’s most beautiful stratovolcanoes. Along the way I’ll be visiting Lassen Peak, Mount Shasta, Lava Beds National Monument/Medicine Lake Volcano, Crater Lake, Newberry, the Three Sisters, Mount Jefferson, Mt. Hood, Mt. Adams, and of course, Mount St. Helens. Unfortunately, Mount Rainier isn’t on the agenda, but that just means I’ll have to go back! Also, I’ll be hiking up Mt. St. Helens and providing you, my excellent readers, with pictures and some awesome scientific facts about the whole ordeal. Huzzah!

Ok, so now you might be wondering what will happen after this Cascades trip concludes. Well, I have a few potential research opportunities in the works, including a return trip to Hawai`i. Regardless, I will also be working on my thesis. I know, I know. You’re thinking that thesis work could be monumentally boring to read about. Fear not! My thesis is creating a map of the rift zone of the Loihi Seamount, the undersea volcano I helped research last October. I’ll be travelling to the Woods Hole Oceanographic Institute in Woods Hole, Massachusetts to work on creating the map. Time permitting, I’ll also be performing geochemical analyses on some of the rocks we collected last year. I’ll be sure to finally post those pics I took on the research cruise, too!

At any rate, the updates from the Cascade trip will be brief (thanks for the 140 characters, Twitter) but pithy. I’ll throw in phone camera pics for good measure, and I’ll upload the real pictures upon my return. Anyway, I just wanted to let everyone know I’m back in business stalking volcanoes around the world! Welcome back, everyone.

Ocean bound!

Sorry guys, no pictures today. However, I am happy to report that I’m now officially done with my time at HVO and onboard the R/V Thomas G. Thompson. It is AMAZING. I’m even happier to report that the ship has full (yet slow) internet. I won’t update with anything tonight, but expect some amazing pictures and information in the next day or so. I’m going to keep the blog going through the end of the cruise, so for all of you who are interested in my continued adventures in volcanology…you’re in luck!

(I will begin practicing my pirate-talk ASAP.) AHOY!

Neverending summer.

Well, I have some excellent news that I’ve been keeping under wraps for quite some time since I didn’t want to jinx it. A few weeks ago my boss at HVO mentioned that a scientist friend of his from Woods Hole asked him to join a scientific research cruise to the Loihi Seamount. Since Loihi is definitely something I’d like to research in the future, I promptly freaked out. I demanded to know what his reply was, and he told me that he’d been there, done that. I informed him that he was nuts. To that, he asked if I wanted to go. Cue another freak out.

My amazing boss then put in a good word for me with the scientist, and after an interview and much airline and school wrangling…I’m going on a research cruise! That means that instead of leaving here tomorrow to return to California, next Sunday I fly to Oahu. I’ll meet up with the boat and we’ll depart on Monday, 9/22. We’ll return to port on October 12, and I’ll fly back to California the next day. That’s about three weeks at sea! Since marine geology is what really butters my bread, this is one of my strongest dreams come true. Now, here are the details.

The cruise is actually going out under the auspices of the FeMO Iron Microbial Observatory at Loihi Volcano. The boat is the R/V Thomas G. Thompson, a NOAA-owned and University of Washington-operated vessel. If you click the ship’s link you can see all of the details, including the berthing setup. I’ll be in berth #35! Excitement. If you read the FeMO link, you know that they primarily study biology. I will most likely help out with that, but I’m there for an experiment in sampling volcanic glasses. My boss on the ship is from WHOI, as I mentioned before. That’s not all of the awesomeness, oh no. It gets better.

I assume most of the people who read this blog have watched the Discovery Channel at some point. Many of you may have heard of the ROV Jason. I certainly had, and using ROV and submersibles to do research was another of my life’s goals. You can guess where I’m going with this, can’t you? Jason will be on board, and we’re using him to collect the samples. Absolutely incredible. Words just can’t do justice to how amazing this whole summer has been (and continues to be).

I think this is an appropriate time to thank the people who’ve made it all possible. Thank you to my parents, for obvious reasons, and because they’re the best parents anyone could ever have. They gave me chemistry sets and helped me with science fair projects since as early as I can remember. Thank you to my professors at California State University – Los Angeles, and in particular Dr. Kim Bishop. They are magnanimous enough to allow me to make up the coursework I’ll miss while on the cruise, and Dr. Bishop is taking over my teaching duties while I am gone. Thank you to everyone who reads this journal, whether I know you in real life or not. You have made documenting this journey of a lifetime a true pleasure. If you have specific questions you’d like answered, please leave them in the comments of this post. It’s often hard for me to go back and pick the questions out from the comments, so let me know what you’d like answered!

Last but certainly not least, I have to thank my incredible husband of almost 7 months. His support is the linchpin that holds both of us together. Without his unfailing encouragement there is no way I’d have come to Hawai`i in the first place, let alone gone on this cruise. He is in Los Angeles, working hard and taking care of our dog and cat. He even moved our home to a new apartment last month. If there was a Husband of the Year Award, I’d nominate him in a heartbeat. So thank you, Benji. I appreciate this more than I could ever tell you.

Ok, just so this post isn’t all texts n’ links, here’s a picture of the R/V Thompson!

From lava to the stars.

We made a pretty stunning discovery in Halema`uma`u on Friday. Many months after the explosion that first opened the vent, we finally had visual confirmation of a roiling, active lava lake inside. Some of the scientists were over the vent in a helicopter, and they were able to get pictures and video of the lava. The best estimate is that it’s about 100 meters below the top of the vent. A few hours after the helicopter overflight, I went out with the gas geochemistry team to do Fourier transform infrared spectroscopy, or FTIR since the lava was visible.

The round part on top of the tripod is a telescope, and the box on top is the spectrometer. Anyway, since we were on the rim and right over the vent, I think perhaps a picture of the lava’s incandescence is in order.

Yep, that’s lava down there. That sort of glow just doesn’t normally happen during daylight hours. It was truly impressive to stand right above a lava lake. The noises were loud, tremendous, and unrelenting. If it wasn’t clanging with rock falls, it was making gas-rushing noises that sounded like jet engines. The earth is alive!

I have a special treat for all of you. My colleague Brian White was down on the other side of the vent from where I was, and he recorded video. You can finally hear the noises I keep writing about! Make sure your sound is turned on. It’s possible to see some of the incandescence as well.

Thanks Brian!

Saturday brought more impressive sights. I ventured up Mauna Kea with some colleagues to check out the view and do some stargazing. The name Mauna Kea means White Mountain, and that’s because it frequently has snow on its peak during winter. It stands 13,796 feet above the ocean, and is older than Mauna Loa and Kilauea. Mauna Kea is considered dormant, but not extinct. It’s also home to some of the world’s best telescopes and astronomical observatories.

Those are the Keck Twins, formally known as the W.M. Keck Observatory. They sit 85 meters apart at Mauna Kea’s summit and they each have a 10 meter primary mirror.

Those are cinder cones on the north flank of Mauna Kea. Since the volcano is in its “post-shield building” stage, it is literally pockmarked with cones like these.

This is the NASA Infrared Telescope Facility. It was posing nicely for me. It was built to support the Voyager missions.

This is the Caltech Submillimeter Observatory with its dome open.

I don’t think that one needs much explanation.

Here we have the moon, some stars, and the Subaru Telescope.

Last but certainly not least, I give you this:

Yes, that’s a laser issuing from one of the Keck Twins. It actually creates an artificial star that astronomers use to establish a relative location in the sky. I’m sure it does some other neat things, too, but I’m not aware of what they are, exactly. ***EDIT*** Check out Andrew Cooper’s comment at the end of this post for the actual use of the artificial star. He knows what he’s talking about!

If you’re ever in Hawai`i, sunset on Mauna Kea is definitely in order. Oh yeah…you might want to check out any available lava lakes, too.

Volcanic eruptions and fumes, oh my!

The night after I helped set up the time-lapse camera to record any collapses of the vent rim, there were two magmatic explosive events. The rim area beneath and to the east of the plume is littered with spatter material. The explosions happened about an hour after I visited the visitor overlook. If only I’d been an hour later! At any rate, I was able to go down into the caldera again yesterday to assist with sampling gases from fumaroles. These are holes in the ground near volcanoes that emit gases and steam. We decided to see the spatter material before venturing in on foot.

Let’s just say it’s a good thing that this road is closed to the public. Some of the ejected material was incandescent at the time of eruption, which signifies fairly high temperatures.

We left that area and journeyed to the less-travelled southern end of Halema`uma`u crater. Here’s a view of the crater wall that you can’t see from the Observatory or Jaggar Museum.

We continued hiking around to the western edge of the crater and stopped for a bit to watch the plume. The vent was making banging noises like it had all day on Tuesday, and after a while it switched to gas rushing sounds. It’s akin to the noise a 747 jet makes as it lands. At one point the plume almost died out, and then it resumed more vigorous puffing and turned brown.

Our resident gas geochemist was nice enough to model for me.

He’s standing in an area of the crater known as the Postal Rift. When Halema`uma`u was filled entirely with lava back in 1919, visitors could walk right up to the rift and dip their postcards into the lava. The edges would become a nicely singed, unique souvenir of their visit to Kilauea. Try to imagine that whole crater and the rift where the scientist is standing as a lava lake. Pretty amazing.

So, I’m sure you’re all curious about what sulfur dioxide does to the areas surrounding it.

It makes sulfur crystals! When sulfur-rich gas seeps out of the earth and the area remains relatively undisturbed, it gives sulfur crystals the chance to grow. They’re beautiful.

Here’s a fumarole up close and personal. The crystals are about 1/2-3/4 inch at their longest. They also smell like rotten eggs. Hey, perfection is hard!

This is what we do with fumaroles…we sample the gas they emit! I’m using a technique called evacuated-bottle fumarole gas sampling. First we measure the temperature of the fumarole using a probe. The temperature around the crater is right near the boiling temperature at this altitude = 94.8 degrees Celsius. After that we insert a teflon tube into the fumarole, and connect the tube to a specially-made vacuum-sealed Pyrex bottle. We then pump the gas into the bottle slowly, and make sure that it cools and condenses enough to close the bottle off.

Once we get back to the lab we run the samples through a manometer (pressure-reading device) to compare the gas pressure in the bottles to the ambient room pressure. After that we stick it on a gas chromatograph and measure the bottle’s levels of air, water, CO2, and SO2. Fumaroles from different areas have different gas concentrations, and this helps us to understand the magma and gas beneath the crater’s surface.

Not a day goes by without me learning something incredibly interesting!

At The Edge Of Oblivion

Today I did another amazing thing. I suppose if I keep calling everything I do amazing people won’t know how to distinguish daily stuff from special stuff. Either that or you’ll all become geologists! My evil plan will finally come to fruition!

Ok, in all seriousness I did something incredible. So you know the vent in Halema`uma`u I keep writing about? Today I helped install a time-lapse camera where the red dot in this photo is located. Keep in mind that the dot is about the size of 3 adults standing right next to each other, and make sure you click to see the full view of the image.

We also walked all along the rim on either side of that dot to perform maintenance on the ash-catching stations we have set up. I was directly over the vent and it was thrilling.

Here you can see the initial setup phase with the monster sulfur dioxide plume in the background. That’s the tripod.

Here’s the conversation I had with the geologist in that photo just seconds after I snapped the pic.

Him: “Hey, do you hear those loud banging noises from the vent?”
Me: “Yeah! They’re so loud! It’s amazing.”
Him: “If you hear a particularly loud one, get ready to run.”
Me: “Oh, right. Rocks can be ejected.”
Him: “You do realize that we could die, right?”
Me: “Yep!”
Him: “Ok, can you hand me those pliers over there?”

Not your average conversation at the office, was it? Let’s just say I pondered my time on this mortal coil for a minute whilst gazing into the swirling maw of Hell.

Maybe I should take up modelling hard hats? Anyway, here’s the end product of our efforts:

In the foreground you can see the solar panel that is responsible for powering the camera. The grey case on the ground is the battery, and the camera is in the open case on the tripod. The camera case lid is shut once we’re done adjusting it. The reason we installed it is that the vent has been growing. The lip and side walls have been collapsing quite a bit lately, so that first picture in this post actually shows the vent even smaller than it is now.

The noises issuing from the vent were otherworldly. I now understand perfectly why ancient Greeks and Romans believed that Hephaestus or Vulcan, respectively, was hammering away inside of the volcanoes. It honestly sounds like someone is forging things in the traditional hammer-and-anvil way. The booms are loud, metallic, and frequent. Sometimes it sounds like metallic popcorn, and other times it sounds like the resonating, drawn out intonation of a gong. It’s not always noisy like this. In fact, everyone is remarking on how unusual the noises actually are. I feel privileged to have heard them.

For those who are curious, I threw several rocks into the vent. I stopped after it belched out a massive plume that immediately blew in our direction. Making Pele, the Hawaiian volcano goddess, angry while perched on the lip of the vent was not on my To Do List for today.

Also of note: Both my photography and my person are present on the official HVO website! Visit the Kilauea Eruption Update page on HVO’s site to take a look. August 28th is the magic date. Those of you keeping up with the blog will recognize some of the images! The Quicktime video from August 31 is definitely worth a watch, too.

Helicopter fun!

On Thursday I went on a geology overflight to Kupaianaha and Pu`u O`o. This area of Kilauea is in its 24th year of eruption. Pu`u O`o is a parasitic cinder cone on the flank of Kilauea, and Kupaianaha is a shield that has formed 3km down from Pu`u` O`o.

The first part of the flight consisted of travelling down the path of the flows towards the current ocean entry.

This is a view to the northeast. The older flows are darker, and the younger flows are silvery.

This is the ocean entry plume shot from above. The lava is pouring into the ocean from a lava tube that is just under the hardened surface flows. The plume is poisonous sulfur dioxide gas (SO2).

Here’s a shot of the plume as we were flying away. Helicopters can induce some funky camera angles.

The helicopter dropped us off further up the flow field so that we could take some measurements. Two of my colleagues are performing Total station measurements with Pu`u O`o in the background. These measurements help us to determine how the ground around the active lava flows and lava tubes is deforming. We can measure elevation change and distances, among other things.

After we finished with the Total station, we hiked towards Pu`u O`o to map a new seep of “toothpaste” lava. This texture of lava is considered to be a transitional stage between smooth pahoehoe and rough a`a flows. We use GPS tracklogging and walk along the boundary of the seep to create the map. That’s what I’m doing here.

The lava seep is from just a few months ago, so the lava itself has an interesting array of colors and textures. There are many small vents of hot SO2 that waft up from beneath where we were standing. I was examining some of the textures and enjoying the warmth of my own volcanic sauna.

After we mapped the boundaries of the seep, we measured the thickness of the seep itself. I was holding the base of the tape measure and recording the data.

The helicopter met us after a few hours and flew us over Pu`u O`o for a look at the current eruption. For those of you waiting anxiously for the smoking cone, here you go!

Of course, this doesn’t provide a good perspective of how large Pu`u O`o really is. That’s why I’m including this image as well.

Those very small, silver dots near the rim in the foreground? Those are our measurement stations. They’re about the size of an average adult. Yes, Pu`u O`o is large. Flying over it was incredible.

I hope everyone is having a wonderfully restful long weekend!

It’s work time…field work, that is.

It’s high time that I posted about the field work I’ve been doing lately. Before I became sick last week, I was out mapping the newest lava flows at Waikupanaha. Well, it was a gorgeous day and I did manage to snap a few pictures before the hospital called.

While hiking to where we were to begin our mapping, we heard and saw some lava bubble bursts to the left of the ocean entry plume. Unfortunately, a watched pot never boils and neither does a watched ocean entry. As soon as I pulled my camera out, the bursts stopped. Ah well, at least the ocean entry plume still looked good.

This is a view to the south, and you can see the pali (or cliff) at the right of the frame. The lava flows toward the ocean from very far up the pali, sometimes aboveground and mostly underground through lava tubes.

The way we map new lava breakouts is by putting handheld GPS units on Tracking mode and then walking along the boundaries of the fresh lava. It’s a good way to map, since you can set the GPS to record your position at intervals of three seconds. The level of accuracy is enough for our purposes. After all, the flow field changes fairly often.

Moving on to the field work I did on Friday (it wasn’t too strenuous, don’t worry)! We met up with a cultural resources guy from Pohakuloa Training Area, a massive area between Mauna Loa and Mauna Kea where the Army and Marines practice bombing and combat. The samples we needed to obtain were on the military’s land, so we have to go through the proper channels to collect them.

There’s a bit of archaeology in what we were doing there.

That is a pit dug by the ancient Hawaiians. No one is sure why they dug these pits, which happen to be about 9,000 feet up the slope of Mauna Loa. We collected samples of the displaced rocks to perform the same Chlorine-36 cosmogenic isotope dating that we did on Mauna Loa’s summit. The reddish lava flow that the pits are situated in is of unknown age, so we’re also going to date that as well. It should give us an idea of how long ago the Hawaiians made the pits.

I suppose it can’t hurt to throw in a picture of the other massive volcano on this island. If you can make out a small whitish blob in the left foreground, past the plants…that’s our truck. This might give some sense of how gentle this particular slope of Mauna Loa is. Trust me, they’re not all like that!

Tonight is my last night housesitting, so my internet access (and consequently posting) should pick up a bit this week.

Sorry for the interruption!

So dear readers, I must beg your apologies. Last week I was out in the field almost every day, and then I had a trip to the hospital. The diagnosis was inconclusive, somewhere between a kidney infection and appendicitis. After a night in the Hilo hospital I was itching to get back up to HVO. I am now full of antibiotics and slightly worse for the wear, but I’m going back out in the field tomorrow! It’s a light field day, so I won’t have much chance to strain myself. It is pretty cool to go into an emergency room right after you’ve been mapping lava flows. The ER staff is a bit more impressed than they would be otherwise. Still, I don’t recommend spending your time in Hawai`i surrounded my medical professionals (unless you’re here for a conference, of course).

Ok, so here’s the amazing truck I drive for work. It’s my boss’ truck, and it has rock-crawling tires for jaunts up Mauna Loa. The front bumper has been sawed off for better clearance, too. It’s a beast.

I planned and am about one third of the way through conducting a survey of the gravity of the Ninole Hills in Kahuku Ranch on Mauna Loa’s Southwest Rift Zone. There is a gravity anomaly there that could indicate the presence of an older, proto-Mauna Loa that has since been overtaken by the new Mauna Loa. It was my boss’ idea of course, but it’s really amazing to be conducting the survey with very minimal supervision.

Over the weekend one of my entomologist friends was able to get the two of us into the Keauhou Bird Conservation Center, a normally off-limits endangered bird conservation facility. Our goal was to see the Alala, or Hawaiian Crow. There are only 60 of these birds left alive in the entire world, and they are all in captivity. Breeding them is exceptionally difficult as their genetic diversity is very limited. The females have notoriously poor egg quality, and they just don’t have the survival wherewithal to make it in the wild any longer. This is probably the most rare creature I’ve ever laid eyes on, and I won’t forget the experience any time soon.

The Conservation Center has two Alalas together in the educational aviary, and they’re not a breeding pair. The male has cataracts and the female has a degenerative ovary disease. They were still beautiful and obviously intelligent birds. The female has her left leg banded and the male’s right leg is banded.

She was enjoying a thawed mouse snack, and from the way she ripped into it her wild heritage was clearly evident.

This is the male, and he barely stayed still long enough for me to snap this picture.

At any rate, there will be more geology this weekend! It’s good to be back. A special note to Sherry and Randy from FL: I hope you didn’t miss the entries too much!