American Geophysical Union 2018

Rose here –

Last December I got a chance to do two things I have never done before: Visit Washington D.C. and attend the American Geophysical Union (AGU) fall meeting. The AGU fall meeting is one of the biggest geology conferences and is held every year in December. This year they broke records with 26,000+ attendees and 28,000+ abstracts submitted!

Here I am with my advisor, Dr. Wade Bishop from the UT School of Information Sciences, at the Data Help Desk in the exhibit hall, where we spent most of the conference.

My advisor was working on a project which required surveying attendees of the meeting and he was able to pay for me to come as well to help out with that. While I had to spend much of my time there at the Earth Science Information Partners (ESIP) Data Help Desk in the exhibit hall, I was able to get away and attend some talks and poster sessions. The project I was helping with was asking scientists who came for help at the Help Desk about their experiences, so we can figure out how to make the Help Desk more relevant and helpful for scientists at future meetings.

I flew in a whole day early so I could explore around D.C., because I knew once the conference started there would be so much going on it would be hard to get away. It was quite cold out so I bundled up in my jacket, hat, and scarf and headed out to see what I could find. I headed toward the National Mall, excited to finally visit the Smithsonian and all the memorials. I walked all the way to the far end of the mall first so I could see the various memorials. I visited the World War II, Korean War, Vietnam War, Lincoln, and Martin Luther King Jr. memorials. As a geologist, my favorite was the WWII memorial because of the variety of rocks used in cool ways. I also learned that besides the regular Vietnam War memorial wall, there is a memorial to the women who served the country and made great contributions during that time.

One of my favorite exhibits at the National Museum of Natural History. All of the minerals in this case are specimens of Corundum, also known as Ruby or Sapphire.

Next I visited the National Museum of Natural History. I had seen it in movies, but I was excited to see all the exhibits in person. This being AGU week, the most packed section was the rock and mineral exhibit. There was a line to even get in, and once in the excitement in the room was quite noticeable. It was so fun to see everyone excitedly discussing the different minerals, where they came from, and why they looked the way they did. These are the things we do for fun when you get a bunch of geologists together!

At the conference, while I did spend most of my time working in the exhibit hall, I had picked a few sessions of science talks to attend. The cool thing about conferences like these is that there are many simultaneous sessions in multiple fields of geology, so I could go see talks on anything I want. I often hop around to talks in fields other than what I work on, but since I had limited time to see talks this time I picked a few planetary science sessions to go see, and a few in areas that are important to me, like promoting equity and inclusion and dealing with sexual harassment in the geosciences. One of my favorite sessions was a lunchtime special session on the last day. AGU held a session celebrating the start of their 100th year, where they had speakers from many of their 25 sections give talks on how our scientific understanding has changed in the last 100 years in their field.

Visiting the map collection at the Library of Congress!

One of the coolest things I got to do was on the last day, right before we left D.C. My advisor knows someone who works at the Library of Congress (LOC) with the map collection, so we got to go and get a behind the scenes tour at the LOC. I loved seeing all the old and unusual maps they have there. The room where they store the maps is as long as 3 football fields! As a geologist it was especially exciting to see their collection of notes and maps from Marie Tharp, who used data from instruments on research ships to produce the first scientific map of the seafloor. This map was important because it showed us where the seafloor was spreading and gave us more evidence for plate tectonics.

I am so glad I was able to go to AGU in D.C. for the start of their Centennial celebrations, and I look forward to going again!

Information Sciences: What are they?

Rose here –

I study information sciences at the University of Tennessee. Why is it called information sciences and not information science? The information sciences are a very broad field, containing many other fields such as data management, knowledge management, librarianship (public, academic, and specialized), archiving, museum studies, and information-seeking behavior studies, among others. This is really true of most sciences, as biology, geology, physics, and chemistry all contain multitudinous specialized fields within the broad discipline.

Here at UT, we have some undergraduate and doctoral students in the School of Information Sciences, but the majority of the students are in the master’s (MS) program. This is because in the library and information sciences, an MS is considered the terminal degree. It is a professional degree, meaning that rather than a focus on research and producing a thesis or dissertation like many grad school programs, there is a focus on learning theories and practical skills that librarians and information professionals need to do their jobs.

Standing in front of the library at Central Washington University, where I got my undergrad degree in geology. This library was one of my favorite places and I spent many hours there studying or just reading in a quiet corner.
Librarians at many colleges and universities have faculty status, even though they are not doing full-time teaching or research. This is important because the services they provide are integral to all of the research and teaching that occur on campus. Many information professionals and librarians, especially academic librarians, already have graduate or undergrad degrees in other fields, which gives them a good foundation for knowing the potential information needs of the patrons they serve. Many librarians spend some amount of time on their own research, either within the information sciences or in other areas they have expertise in.

I also have a previous graduate degree, an MS in planetary geology. I decided to continue and get another MS in information sciences rather than try to find a job as a geologist right away. I knew I did not want to get a PhD and be a professor doing full-time research or teaching. However, I did want to find a way to stay involved in the planetary research and teaching community in a support role. With a degree in information sciences, I could work as a GIS specialist (What is GIS?), a technical information or data management specialist, or as a librarian specializing in an area related to planetary science. These are all jobs that exist within organizations such as academic and specialized libraries, USGS/NASA/NOAA, and private planetary science institutes and industries.

One of my favorite holiday activities: sitting by the fire reading about awesome women in science!
Since joining the School of Information Sciences last fall, I have had several opportunities to explore career options in this field. I got a position this as a Community Fellow with the Earth Science Information Partners (ESIP). ESIP receives funding from NASA, NOAA, and USGS, and contains many member organizations who are working to improve all aspects of information and data management in the earth sciences. In my position as a fellow I get to attend their two annual meetings for free and to participate in any of their clusters (groups focused on a specific topic), as well as working more closely with one particular cluster. This gives me the opportunity to see what is going on in earth science data, as well as find new people to collaborate with. I have also been able to participate in a couple of research projects focused on Earth and planetary science data. I got the chance to travel to the American Geophysical Union meeting in Washington DC in December to collect data for one of these projects. I had never been to Washington DC before, so that was a cool experience. I will even get to travel to the 4th Planetary Data Workshop in Flagstaff in June to present some of my research, so stay tuned for a post about that!

Drumheller Channels

Rose here –

The Columbia National Wildlife Refuge was designated as a National Natural Landmark in 1986. The landscape here is amazing because while it is a desert or shrub-steppe environment, it has been amazingly eroded and carved by water from the giant Ice Age floods. This influx of water has allowed plant and animal life to flourish here, and also allowed humans to farm the land. For more, click here.
A couple of years ago my mom and I took a road trip to eastern Washington state to visit Drumheller Channels in the Columbia National Wildlife Refuge. This is an area containing giant basalt columns, part of the Columbia River Basalt flows, as well as some of the landscape known as the Channeled Scablands, remnants of the catastrophic Ice Age floods (check out the Ice Age Floods Institute for more info).

The Columbia River Basalt Group (CRBG) is a large igneous province in eastern Washington. Large igneous provinces are usually made of very low viscosity (runny) lava which has erupted from fissures in the ground and spread out to cover a large area. The CRBG is a series of lava flows (more than 350!) that cover an area of about 163,700 km2 (63,200 mi2). These lava flows altogether are more than 1.8 km (5,900 ft) thick. These flood basalt eruptions occurred from about 17 million years to about 5 million years ago

This is a view of the channeled scablands landscape, where you can see the tops of different coulees and lava flows in the distance. This land is crazy rugged to drive through!
As basalt cools, it forms a hexagonal pattern on the cooling surface exposed to the air, similar to the pattern you see in mud as it dries. From the side this pattern looks like rows of columns next to each other, and beautiful landscapes made up of several stacked flows of this “columnar basalt” are a common sight as you drive through eastern Washington. The other major component of the eastern Washington landscape, the Channeled Scablands, are the result of flooding that occurred toward the end of the last ice age. They are called Channeled Scablands because the landscape consists of many interconnected channels and coulees and appears very rugged. This landscape has turned out to be one of the most important pieces of evidence in shaping our current understanding of how geological processes have shaped the surface of the Earth.

Here I am hiking over to some of the columns so you can get a measure of scale of these features.
Before J Harlen Bretz started studying this landscape in the 1920s, geologists thought all Earth processes were extremely slow and gradual in making any changes in the landscape. This was a reaction to the suggestion by young earth creationists that the earth was formed rapidly by catastrophic events. The response of geologists to this idea was to immediately dismiss any hypothesis that the landscape had formed rapidly and insist that everything had happened very slowly and gradually. J Harlen Bretz became interested in some interesting erosional features he saw in eastern Washington and began doing intensive fieldwork in the area in 1922. As he continued to map and record his observations of the features he saw there, he became more and more convinced that this landscape had not been formed gradually but had been shaped by giant floods from further east. There are giant ripples here, giant channels and coulees, and giant “potholes” where rock has been plucked up by water rushing past. These features could not be explained by very slow and gradual erosion. Today, geologists understand that while many features are formed slowly, the landscape has also been formed in places by catastrophic events, some of which we can see today in volcanic eruptions, earthquakes, and tsunamis.

Here I am standing next to some of the best-shaped columns, which have been carefully separated from the rest of the basalt flow and stood up on their own so you can see the hexagonal shape.

If you want to know more, here are a couple of good books to start with. Check with your local public library!

More References:

We knew we had made it when we saw the giant basalt columns in the distance. Check out the pictures of me next to them to see how big they really are!
Close-up view of the basalt columns from the side.
Close-up view of the basalt columns from the top.
Standing next to the column wall so you can see how large they really are!
The sun was in my eyes, but this place was so pretty I had to get a picture with it. Thanks to my mom for all the awesome photos from this trip!

Can you dig it?

Rose here –

In the geology gallery at the museum, scientists explore their own research and help visitors better understand the process of fossilization. Photo from @EPS_UTK on Twitter.

At the University of Tennessee in Knoxville, we have a natural history museum on campus called the McClung Museum of Natural History and Culture. Every year they do a family fun day event called Can You Dig It? where scientists from different departments on campus come and set up various activities to engage families. The Earth and Planetary Sciences department always shows up with several fun activities for families and kids of all ages. This year we had quite a few things going on.

Outside we had two tables of planetary activities. One table was talking about volcanoes and how to tell the difference between rocks formed by volcanic eruptions and rocks formed by meteorite impacts. We had real meteorites and impact deposits, as well as some volcanic rocks, so the kids could hold them all and really see the difference.

Other graduate students outside with experiments dealing with impact craters for visitors to explore!

I was at the other planetary table, where we had some more meteorites and 3D-printed models of actual impact craters on the moon and Mars. We used these to explain how the shape of impact craters change depending on the size of a meteorite and the speed at which it impacts. We also had a tub of flour with a thin layer of cocoa powder on top. There were several marbles and small balls, and kids could hold one above the tub and drop it to make their very own impact crater. The layering using cocoa powder allowed us to show them how ejecta blankets work at real impact craters. An ejecta blanket is made of rocks from the impact site being blown up and out of the crater and landing to form a “blanket” surrounding the crater. In the tub, you could see flour on top of the cocoa powder after the impact, showing how buried layers get exposed at the surface surrounding impact craters.

Graduate students have a STEAM (Science, Technology, Engineering, Arts, and Mathematics) for students and visitors to get more information about a variety of topics. Photo from @EPS_UTK on Twitter.

Inside the museum, we had a table where people could bring in rocks or fossils they had collected and geologists or paleontologists would help identify them. This is a really popular thing, and some people bring loads of rocks they’ve been collecting all year.
If you have a local museum, make sure to go check them out. Local museums are often cheap or free and also host fun events like this one!

Skype a Scientist

Rose here –

I recently got to participate in a different kind of outreach activity. Instead of going to a classroom or museum and talking to students in person, I got to share my research with students in a classroom all the way across the country via Skype! I had signed up with an organization called Skype a Scientist earlier this past fall.

I didn’t take any pictures during the session, but here are the rocks I used to answer their question “what are your favorite rocks that you’ve collected?” Clockwise from top left: a conglomerate a friend sent me from California, a jar of Mount St. Helens ash my gramma collected off her car the morning after the eruption, a piece of Columbia River Basalt I collected in undergrad, a gypsum rose from Morocco (my parents bought it in a shop in Oregon), a large quartz crystal my gramma collected in the Mojave desert, a piece of rose quartz I collected in the Sierra Nevada, and a piece of amethyst my roommate brought back from Uruguay.

This organization matches scientists with teachers who would like to have a scientist talk to their classrooms about their research, maybe related to something they’ve studied in class. Because it’s all conducted via Skype, the scientists and classrooms could be anywhere. I live in Knoxville, TN and the 7th grade classroom I connected with is in Seattle, WA. This was fun because I grew up in the greater Seattle area, so I could talk about the local geology. I got to share with them how growing up in the shadow of volcanoes, experiencing earthquakes as a kid, and learning about the glacial ice sheets that used to cover the land where my family now lives all inspired me to love and learn about geology.

My thesis research here in Knoxville has been on the geomorphology of Mars, which was perfect because this class was just finishing up a unit on Mars geomorphology. The teacher contacted me a couple of weeks before we met via Skype. I sent them some info on my research and the students sent back a list of questions they had for me. The topics of these questions ranged from undergrad vs. grad school to questions about Mars to questions about my favorite rocks or field areas. I was really impressed by the thought they put into these questions and the range of things they were interested in. During the Skype session, I started by answering as many of these questions as I could. This took about half the class time, so the teacher and students then had a chance to ask follow-up questions. The students were very engaged and interested in what I was saying. I was a little nervous beforehand that I wouldn’t be able to answer their questions or the technology would fail on us, but it went really well and we all agreed it would be fun to do again. If you are a teacher or scientist I would totally recommend checking it out!

If you are interested in signing your class up, or a researcher interested in talking to a classroom, you can sign up for Skype a Scientist here!

Grand Canyon Trip

Rose here –

Standing on a rock at Ooh Aah Point, about a mile down the South Kaibab Rim Trail.
A year ago I got the chance to visit the Grand Canyon National Park. I had been there once as a toddler, but of course I didn’t remember it, so I was very excited to have the opportunity to go again now, especially since I’ve been studying geology for a few years. The Grand Canyon is like Disneyland for geologists. There are SO many cool geologic processes and so much geologic time represented there (click here for a fun read on the geology).

Hiking down the South Kaibab Rim Trail and looking back up at the South Rim.
We were staying in Flagstaff, AZ for a conference, but my colleague and I had a free day before it started and since the Grand Canyon is only an hour and a half away we decided to just hop in the car and go. We started off early in the morning so we could try and beat the heat. When we arrived we headed straight to the rim.
It was one of the most exciting moments of my life. I had seen pictures of the canyon, but nothing prepared me for what it was actually like to stand there in person. We walked up to the rim with our eyes on the ground so we would see it all at once. When we got close enough we looked up and were utterly speechless for at least a minute. It was so worth it. The Grand Canyon is so big. Like, SO BIG. Apart from all the cool geology, it is a really amazing view.

Sitting near the edge by the Geology Museum (I was further back than it looks!).
One of the coolest things about the Grand Canyon (besides the size) is how you can really see textbook examples of geologic concepts displayed in a way that anyone can see. For example, the Great Unconformity is a famous example of an unconformity – a place where rocks were deposited or uplifted and then some time passed and/or erosion occurred before more rocks were deposited. The Great Unconformity is the place where the beautiful sedimentary rock layers that make up most of the Grand Canyon are deposited on top of older metamorphic and igneous rocks. The distinct sedimentary rocks layers we see exposed in the canyon help geologists understand what the environment was like at different times in the past. After all these rocks were deposited, the canyon itself was carved out by the Colorado River starting at least 6 million years ago (click here for more information), resulting in the Grand Canyon we see today.

A note from the editor (Jen): I wholeheartedly agree with this description, the view is beyond breathtaking. It takes a while to soak in the awe inspiring beauty. Time is so often taken for granted but when you can see so much time in the rocks, it gives you a new perspective.

A view of the Grand Canyon from near the visitor’s center, looking north from the South Rim.
Me standing at the South Rim, with Bright Angel canyon behind me.

Freedom Schools Program

Rose here –

A picture of my teammate Katie and I with our Freedom School scholars. I am sitting second from the left in the back row.

This summer I got the chance to hang out with local elementary school students and do cool science experiments. I was one of several volunteers from 500 Women Scientists KnoxPod, an organization dedicated to science outreach and opportunities for fellowship for women scientists, and we partnered with the local Freedom Schools Program, a national summer literacy program for at-risk and minority youth. As part of our partnership, we came up with some fun experiments and demonstrations of various scientific topics to get our students engaged and interested in science.

Our main goals were to show the students that anyone can do science and that the ideas of science affect our daily lives in many ways. Since we had never done this before, it involved a lot of Google searching and trying to find ways to do experiments that were fun and doable for a range of ages and abilities of students. It was helpful that the students we worked with were divided into upper and lower elementary age groups, so we could have some activities involving more reading for the older kids. But both groups were very impressive with their understanding and retention of the ideas, even remembering things we had talked about much earlier in the summer!

One of the most rewarding moments was when one of the girls who had seemed kind of shy and reserved during the earlier sessions came up to me one day and told me that she wants to be a scientist when she grows up! By the end of the summer there were other kids too who would cheer when I walked in, declare that science was their favorite subject, and try to sit as close to me as possible. This made me feel like all the hours spent preparing lessons were totally worth it. I had never done any sort of K-12 classroom presentation before so it was also a really great opportunity to get more practice explaining the concepts of science in an accessible way.

Below are pictures from when we made a pendulum and added paint to make some art and show patterns of pendulum swinging and their causes.

Planetary Geologic Mapper’s Meeting

Rose here –

The meeting room with several posters of maps that were presented.

One of my favorite events every year is called the Planetary Geologic Mappers Meeting. This is a meeting held annually at which all scientists with a NASA grant to do geologic mapping come and present updates on their maps. It’s really cool because there are maps not just of well-known or major planetary bodies (Mars, Mercury, Venus, the Moon) but also of smaller or less well-known bodies, including asteroids, dwarf planets, and several moons of planets in the solar system. Earth is of course a planet too, but to distinguish science done on and about earth from that done about any other place in the solar system or universe, everything not on Earth is called “planetary” and Earth-specific research is termed “terrestrial”. The main point of this meeting is to update NASA, although it has also become a place to get feedback and support from the USGS Astrogeology mapping support team and fellow mapping scientists, but it’s also a great opportunity for students to network and learn more about planetary geologic mapping.

This meeting is very small, generally less than 50 attendees, unlike the big geology conferences like GSA (Geological Society of America) and AGU (American Geophysical Union). This means that even though this was only my third time attending, I was familiar with many of the people there and what they were doing. There were a number of new faces this time, which is very exciting. It’s always fun when people start doing planetary mapping for the first time, and the community is very welcoming of new-comers and willing to help.

Several members of Dr. Burr’s research group discussing a map of fluvial features on Titan (a moon of Saturn).

This year it was held in our department at the University of Tennessee, Knoxville. My advisor, Dr. Devon Burr, was the local organizer this year, so I got a chance to see everything that goes into hosting a conference like this. It was great fun to welcome all the mappers to Knoxville. I’ve made a few friends at this meeting over the years and I loved the chance to show them around my city.

The first two days are poster and oral presentations. One person from each mapping team gives an oral presentation on their project, with some time for questions they have for other mappers or thoughts and questions from the mappers and USGS mapping staff. Most mapping teams also have posters of their maps. There is lots of time built into the schedule for poster presentations and networking. There are teams of mappers from different universities or institutions who use this time to meet and discuss their work in person rather than phone or e-mail as they usually have to do during the school year. It’s also a good time for student mappers to ask more experienced mappers or those with expertise in a particular field for advice and feedback on their projects.

This photo shows members of the Earth and Planetary Sciences department who participated in the Planetary Mapper’s Meeting this year. On the far right is Dr. Devon Burr, who led the local organizing committee for the meeting.

The first night we had a social and all went out for dinner at a local restaurant. It was a great break from all the science we’d been discussing. We got a chance to catch up and talk about where we’re all living and working, show off pictures of our pets and families, etc. It’s good as scientists to take time to appreciate each other as humans too with lives outside of our jobs each day. While this meeting is short and sweet, it’s always great fun and I look forward to the next one!

Geologic Mapping on Mars

Rose here –

One of the famous first stories of modern geology involves the publishing of a geologic map of England by William Smith in 1815. This was one of the first geologic maps made by a geologist doing fieldwork, which often involves camping out in an area for a few days, weeks, or months to find out as much as possible about the area to be mapped. Geologists walk around the area to be mapped and take measurements of what types of rocks are there, how thick each layer is, whether they are tilted or faulted, etc. They may also take samples of the rocks to do chemical tests or look at them under a microscope. Field geologists look at the morphology (shape) of the landscape in order to map the locations of ridges, depressions, and other features and determine the processes that formed them.

Several students (I am on the far right) mapping the “Banana Canyon” area in southern Idaho at senior field camp, summer 2014. We spent a couple days roaming around this area, taking measurements and notes and figuring out what kind of rocks were here. Then we would go back to camp and use our measurements to make a cross-section showing the different layers of rocks and where faults or folds might have occurred. Our long sleeves, pants, and hats were so we didn’t get sunburned – it was actually pretty hot that day (and every day)!
My experiences in geology as an undergraduate major were largely field-based, going on many field trips to various places and taking notes and measurements at different locations. But how do you make a map when your field area is on average 140 million miles (225 million km) away from Earth? I had never considered studying geology in a field area anywhere other than Earth, but shortly after starting my master’s degree I had the opportunity to work with a team of collaborators to create a geologic map of a small region on Mars. Geologists can now create maps of planets, moons, and asteroids using high-resolution images from spacecraft orbiting Mars, Mercury, the Moon, and many other bodies in our solar system. I was excited to begin this project, but first I had to learn a whole new set of skills than what I had used in field camp as an undergrad.

There are several software programs scientists can use to make maps using images and other types of geospatial data. These software programs are collectively called Geographic Information Systems (GIS). GIS software is used in many different fields for different kinds of projects and analyses. For example, biologists might use GIS to make maps of where certain species of animals live in relation to cities, lakes, highways, etc. Geologists might use GIS to produce maps showing the location of certain types of rocks or geologic features.

For my master’s project, I used a mosaic (several images digitally “stitched” together) of images from the Mars Reconnaissance Orbiter’s (MRO) Context Camera (CTX). To identify a feature in these spacecraft images, it needs to be big enough to have at least two pixels across it each way (so a minimum 2×2 grid). CTX images of Mars have a resolution of 6 meters (m) per pixel, which means they can be used to find features about the size of a large room. When I upload these images into my GIS program, I can zoom in and out to see features better. When I find a feature that looks interesting, I can mark its location and shape by making a new “layer” and drawing on the image. I use different layers for different types of features, and each layer can be turned on and off so I can see where different features are in relation to each other.

Here I am doing a totally different kind of mapping! I am using the GIS software ArcMap from ESRI to map the locations of wrinkle ridges in my study area, a place called Aeolis Dorsa in the eastern hemisphere of Mars near the equator.
My first step in mapping was actually not mapping, but reading lots of previously published papers about the geology of my study area and about the particular type of feature I wanted to map. I am mapping a type of ridge on Mars called a wrinkle ridge. This ridge is formed by tectonic contraction and is found in layered igneous or sedimentary rock units. Once I had read as many papers as I could find on wrinkle ridges and made several tables summarizing the various types of information on them, I could finally start mapping. It took quite a while for my eyes to get used to looking at these images and to pick out the features I was looking for. However, wrinkle ridges have several common distinguishing characteristics, mentioned in many published papers, that I used to double-check my visual identification. When I had gone over my whole study area several times and marked any feature I thought could possibly be what I was looking for, I went over it again and narrowed down the number of features using my list of common characteristics. Learning to identify wrinkle ridges and other features visually is a good skill and I spent a great deal of time trying to do so. However, it is also important to make my results understandable and reproducible by other scientists. Thus I need to be able to clearly show how I identified a feature as either a wrinkle ridge or not. With my list of common characteristics, I decided how many of them would be required to determine if a feature is a wrinkle ridge, and within those determined to be wrinkle ridges I further divided them by how many characteristics they had into certainty levels: Certain, Probable, and Possible. This process allows my work to be reproduced or at least easily followed by any future scientists studying the same type of features.

I’ve been working on this project for about two years now and while it’s been a lot of hard work and tired eyes, it so rewarding to see my map finally coming together. While I’ve been mapping one type of feature, other scientists in my research group have been mapping different types of features and we are about to put them all together and make one complete map. When we have all our mapping together on one map, it will be published as an official United States Geological Survey (USGS) geologic map. Stay tuned!

A journey into geology

Rose here –

Howdy! Today I want to share with you some of my journey to get to where I am in grad school. I am currently finishing up a master’s degree in geology, but I didn’t always plan on going to grad school, or even going into science.

Growing up in the Pacific Northwest, some of my favorite books were the ones on earthquakes and volcanoes, which were both very real geologic hazards in the area I lived. Someone gave me a book on identifying rocks and minerals and I started a rock collection with rocks I found down by the river or in my parent’s driveway. My grandpa loved rocks and geology and taught me how to identify various rocks and minerals and even pan for gold with sand and gravel he brought back from the Mojave desert in California.

However, by the time I got to high school I was struggling with algebra and higher level science classes and didn’t think I had what it takes to be a scientist. There were no high school level geology classes offered at that time and I didn’t even know that “geologist” was an actual job title. I discovered that I was really passionate about education and helping folks with special needs so I decided to go into special education.

This is the group photo from the 2012 GEOL 210 course at CWU, an introductory field methods course. We took this photo standing in the White Mountains near Bishop, CA with the Sierra Nevada range in the background.

After high school, I started at nearby Green River Community College (GRCC) so I could save money by still living at home. In the spring of my second year I had to take a science elective and ended up in Geology 101. I could write a whole post on how important geology classes at community colleges are, but I’ll save that for next time. This class quickly became my favorite class from my time at GRCC. The professor focused on how geology can be useful in our daily lives by framing each unit in terms of local geologic hazards to consider when buying a house or how to know what geologic processes have occurred when looking at a landscape. This made geology seem very interesting and relevant.

Now that I knew what geology was all about and what geologists do, I started seriously considering a career as a geologist. I loved the idea of studying the earth and the processes that formed it and are still shaping the landscape today. I especially loved learning about different hazards that affect people’s lives in different places in the world and how geologists can help prepare for and mitigate after disasters. The accelerated pace of college classes seemed to be what I needed to finally figure out higher level math, and I was actually enjoying my algebra and chemistry classes. I started paying attention to geology stories in the news and was in my professor’s office almost every day to talk about a recent earthquake or a cool rock I had found, etc. I decided to pursue a BS degree in geology after finishing at community college and looked into quite a few undergrad programs from Alaska to Ohio. I settled on Central Washington University, about an hour and a half from my childhood home, but on the other side of the Cascade Mountains so I got to experience a totally different type of climate and landscape. In the CWU geology department, every class that could had at least one field trip, and often more. There were good examples of almost every type of geologic process within a couple of hours of our university. I loved every class I took there and it seemed like every day was constantly reaffirming that this was where I was supposed to be. Even the informally dubbed “weed-out classes” I loved, which I was assured was the whole point: if you loved even the classes with 4 hour labs and 25+ hours of work outside of class time, slogging through all kinds of geology problems, then you were in the right spot.

Here we are setting up a geodetic survey station during a geodesy field course at CWU. We were down near Three Sisters, OR and used the GPS data we gathered to study how the earth is deforming (moving up, down, or sideways) near these active volcanoes.

When I was finishing up my bachelor’s degree and pondering what was next, I thought that I wanted to go to grad school, but not just yet. I had been in college for 5 years at that point and felt like I needed a little break. But then I attended a national Geological Society of America meeting in Vancouver, BC during the fall of my senior year. This is one of the biggest conferences for geologists every year, and there were scientists from all over the US and the world and from every branch of geology. I saw so many cool projects and was so inspired by all the interesting geology that I decided I wanted to be a part of that as soon as possible. When I got back I did some research and started sending e-mails to professors I was interested in working with. I didn’t get a single response to my first round of e-mails and was kind of discouraged. But I still really wanted to get in on some cool geology research so I sent out a second round of e-mails to completely different professors and heard back from all of them within a couple days! I was so excited to begin this journey and immediately started the application process, took the Graduate Record Exam (GRE), and waited eagerly for acceptance letters. I got in to two of the four schools I ended up applying to. I had a choice between living in Tennessee or Alabama, but decided I wanted to be closer to the Great Smoky Mountains (a dream destination since my childhood) so I went with Tennessee.

Here we are sitting next to the Borah Peak fault scarp in Idaho. This was during senior field camp and we had to map out the extent of the scarp and measure how much deformation had occurred.

I moved to Knoxville and started my master’s in the Department of Earth and Planetary Sciences at The University of Tennessee, Knoxville. I was prepared for an adventure, but even this one didn’t go the way I thought it would. My first project didn’t quite pan out the way I thought and I ended up switching projects and advisors toward the end of my first semester. This is way more common than you hear about…I have several other friends who switched advisors or projects as well. Sometimes it’s a personality or advising style issue, or sometimes the project itself is just not a good fit. The thing I had to keep reminding myself during this time was that it wasn’t a failure to change projects and not do what I thought I was going to, it just meant it wasn’t a good fit for me.

So I was on to my new project: contributing to a geologic map of a local area on Mars. Before starting this project, I didn’t know scientists even had the data to do geology on Mars! I was a little disappointed to not be doing field geology on Earth, but I thought this was a great opportunity to learn something new and expand my skills in geology and mapping. I discovered in undergrad that I loved mapping and structural geology (faults and earthquakes and how rocks move and deform). This project combined both by allowing me to map structural features on Mars and try to figure out a little about how they formed and contributed to the landscape in my study area. Throughout my time on this project I have come to appreciate the

I’ve been on this project for two and a half years now and I’m nearly done and thus began pondering again: what’s next? I applied to lots of jobs in geology or related fields and got only one phone interview. This is fairly common, but it’s still difficult not knowing what’s next. Then over Christmas break I remembered that in undergrad I had considered someday being a librarian. I am really passionate about reading and writing, about the community spaces libraries provide, about making information available and accessible to all. I had sort of pushed this idea to the side while pursuing my master’s in geology, as a “someday dream”. Now that I was almost done with my geology studies, I decided maybe “someday” was actually “now”. I did some research, talked to friends who were librarians, and sent more e-mails to professors. I ended up applying and being accepted to the Information Sciences program at UT to start in Fall 2018. I am so excited to explore the possibilities of combining my passion for geology and information: some potential jobs include positions at state geology libraries, the United States Geological Survey (USGS) library, national labs, or as a subject librarian at academic libraries.