Newberry Volcano Caldera (Image with permission under creative commons, by Craig Elliot, Flickr user Tjflex2)

How is a volcano going to create electricity, you ask?  By pumping 24 million gallons of water deep into its side and capturing the hot water and steam generated, whereupon it will be sent through turbines at the surface to create electrical power.  This process is commonly known as geothermal energy, a renewable resource which developers hope – by adding this volcano element – will be made economically competitive with the cheap (and booming) natural gas industry.

The companies conducting the study will be pumping 24 million gallons of water over 10,000 feet below the surface on the side of the volcano.  Here, the cold water injected into the ground can be heated by the hot rock which, in turn, is heated by an underlying magma chamber (only 2-5 km deep).  When this water is heated, the steam is recovered to produce electricity (as explained above).

In order to efficiently heat the water, you can’t just drill a hole straight down and pump water into the ground.  This is where a process called hydroshearing comes in.  Hydroshearing is a technique in which water is injected into the boring under high pressure in order to induce and enhance fractures within the rock.  Once these fractures are in place, the cold water is injected into a newly created “reservoir” composed of this fracture network within the hot rocks.  Now, hot water and steam can quickly and easily be recovered.

Does this process sound familiar?  It should: it’s nearly identical to hydraulic fracturing.  You say po-ta-to, I say po-tah-to.  The name change is (in my opinion) a political thing.  There’s too much bad press floating around the term “fracking”, so they change the name to “shearing” and it’s automatically more environmentally friendly.  To be clear, hydroshearing is safer for the environment. The big difference here is that hydrofracking injects a large number of chemicals into the ground and hydroshearing doesn’t.

If you’re one of those worried about earthquakes induced by hydraulic fracturing, well then you should feel free to worry about these geothermal projects, too.  However, you can read a previous post on hydrofracking to hear my stance on that issue.

In the end, it seems odd to me that nobody thought of this before.  The exploitation of geothermal energy has been around for over a century, why wouldn’t we go to a location where a heat source exists much closer to the surface, thereby making it easier and cheaper to utilize.  Regardless, it seems the government and private sectors are interested in the project, investing over $40 million.    I’m looking forward to seeing the results!

I know some of you who read this live in this region of the country and therefore will be much more directly affected by this than myself.  What are your thoughts/concerns?

Thanks to my colleague, Jeff, for giving me a little inspiration for a new post by leaving this article on my desk this morning!  Please take the time to read it through a get some more details on the geothermal project at Newberry Volcano.

Today, Google has tipped its hat to geologists everywhere by dedicating its Google Doodle to Nicolas Steno on his 374th birthday.

Steno was one of the world’s earliest geologists and, by many accounts, very likely the first.  He was one of the first to theorize (correctly) that fossils may not have been naturally forming inclusions in rock, but remains of prehistoric animals.  Steno also helped to develop stratigraphic relationships, Original Horizontality and Superposition, which are included today as two of the six Fundamental Principles of Geology.

Today’s Doodle commemorates these achievements by forming the logo using horizontal rock layers representing different periods of geologic time (oldest on bottom, of course).  The layers of rock are also full of fossils to represent Steno’s accomplishments in paleontology.

Happy 374th Birthday Nicolas!  And thanks, Google, for honoring the father of geology!

Until next time, have a Merry Holiday-of-Your-Choosing and Happy New Year!!!

My reason for beginning this site was to advocate the study of geology and answer the age old question “Why should I care?“. To do this, I like to write about topics which demonstrate how much geology affects your every day life. Therefore, despite the overwhelming coverage of the topic and how well others have written about it, I’d be remiss if I did not devote a post to the oil and gas recovery technique known as hydro-fracking.

Much of what I’ve written here has been addressed in one way or another in articles all over the web. What I hope to accomplish here is to provide accurate information and to pull together different topics and concerns into one place where you can feel confident that you are being provided factual information with none of the fear mongering or cover up nonsense.

What is hydraulic-fracturing?

Hydraulic fracturing – aka “hydro-fracking” or simply “fracking” – is a technique most often used by oil and gas companies when they install a new recovery well into a gas/oil-bearing geologic unit. The hydro-fracking process is implemented after a well is installed, but before recovery begins. At this stage, a mixture of water, sand, and various other chemicals are injected into the well under pressure in order to spread open and propagate new and pre-existing joints and fractures in the geologic unit of interest.

Why is it used?

The hydro-fracking process has been used since the late 1940′s for a variety of reasons, including groundwater, geothermal, and waste storage applications. One of the most notable uses of hydro-fracking is oil and natural gas recovery, where it is utilized to enhance recovery of these resources in the subsurface. The technique increases the permeability of a geologic unit, which allows liquid and/or gas to move more freely toward the recovery well and, therefore, significantly increases production at the wellhead.

In recent years, drilling technologies have advanced and oil/gas-bearing geologic units previously believed to be too cost-prohibitive to drill are now becoming the center of attention. Enter the shale gas.

Shale is a sedimentary rock which can have a high porosity (small voids within the rock which can store oil and/or natural gas), but has a very low permeability (stored fluids cannot move through the rock easily, if at all). Fractures already exist in the shale, but are typically very tight, hairline fractures which don’t permit much movement of fluids. This made recovery from these units uneconomical without the use of fracturing techniques which would increase secondary porosity (fractures and joints). By opening and extending these fractures and joints, the oil and gas is now easily recovered.

Even with hydro-fracking being used for decades, shale gas was considered too hard to recover because these fractures only propagate outward from the well so far…you wouldn’t reach much gas without putting a dense grid of wells over a large region. With the invention of horizontal drilling, this problem was solved. A company can now drill vertically down to the geologic unit of interest (the Marcellus Shale in Pennsylvania, for example), then change direction and begin drilling horizontally along the length of the unit. In addition, multiple wells can be drilled from a single location on the surface. Shale gas is now not only recoverable, but profitable.

How is it accomplished?

It’s all about stress. At depths sometimes reaching 20,000 feet below the surface, you can expect great amounts of confining pressure. This pressure tends to hold fractures tightly closed. By introducing an incompressible fluid (water) and putting it under enough pressure, these fractures may be spread open. This same process is also capable of creating new fractures. By pressurizing the water, you reduce the effective stress of the rock and cause the minimum principle stress to become tensile. When the minimum principle stress (now tensile) exceeds the tensile strength of the rock, fractures are induced parallel to the maximum principle stress direction (perpendicular to the minimum principal stress).

All open fractures are immediately filled with sand grains which were mixed in with the pressurized water. The main purpose of the sand is to prop open the fractures. Remember, once the pressure is removed from the water, the original confining pressure will return. Without the sand in place, that pressure would close all the new fractures. The sand not only prevents fractures from closing, but is a highly permeable medium for fluids to pass through, ensuring the fractures will continue to serve as efficient conduits for recovery.

Concerns with hydro-fracking

Hydraulic fracturing has been blamed for creating many hazards to humans and the environment. However, how credible are claims of fire-breathing faucets and earth-splitting quakes? To understand the possible threats, we must understand the geology of the location being “fracked”.

Earthquakes

Earthquakes seem to be on the rise this year and, according to many media outlets, the culprit is hydro-fracking. Rather than believing everything you hear on the television or internet, do yourself a favor and treat yourself to some light research before developing a strong feeling on the subject. If you did, you’d probably find out that we’re not experiencing any more earthquakes than usual. Statistically speaking, we’re right on track.

But when earthquakes happen in areas thought to be safely away from common sources, like fault zones and plate boundaries, folks are quick to blame hydraulic fracturing. Such was the case when the magnitude 5.8 earthquake hit near Washington, D.C. on August 23, 2011. One of the first fingers pointed was directly at hydro-fracking. Besides, what else could it be? There was no large fault zones in the region, and Virginia is about as far from a plate boundary as you can get. The hitch was that there were no fracking operations near the focus of the quake, either.

Many people don’t realize that you don’t need a plate boundary or large fault system to experience an earthquake. True, these definitely help and tend to be where you get the larger quakes, but small earthquakes happen all over. Ohio, for example, has experienced nearly 200 earthquakes of magnitude 2.0 or higher in its recorded history, with a 5.4 magnitude quake occurring in 1937, well before hydro-fracking techniques were ever used.

However, anthropogenic sources for earthquakes have been well documented. Many of these involve injection of fluids into the ground (especially along fault lines) for waste storage or enhanced recovery techniques. Additional induced seismicity has been documented after large volumes of fluid like groundwater have been removed from the ground (large-scale ground subsidence), or when new reservoirs are filled (increased overburden pressures). The U.S. Department of Energy touches on this subject, as well.

It is important to note that hydro-fracking does cause earthquakes! If you think about it, the process is creating fractures in rock which is buried miles beneath the surface. This is obviously going to result in seismic events recordable on a seismograph. The distinction is the magnitude of these events. In most cases (and by most, I mean nearly all) the conditions present at a project site result in “micro-quakes”, or those that can only be detected by extremely sensitive instruments. It should go without saying that these “earthquakes” cannot be felt and definitely won’t cause damage at the surface.

In certain cases, like in the UK this past month, the site’s geology may make it more susceptible to earthquakes. In this example, multiple minor earthquakes of magnitudes up to 2.3 (in April 2011) occurred in the vicinity of a hydraulic-fracturing operation being conducted by Cuadrilla Resources. An investigation into the cause of the quakes led Cuadrilla to the conclusion that the waste water injection wells (associated with hydro-fracking operations) most likely triggered these earthquakes. However, the unique geologic conditions at the site – namely, the presence of a fault zone – made the site more at-risk than most. Even so, the largest of the possibly induced quakes was barely enough to be felt at the surface, and led to no damage.

Even with the knowledge that fracking-induced earthquakes are possible with the right geologic setting, it’s not something to start blaming for every earthquake which we don’t expect. Such was the case above as well as other locations, such as the November earthquakes in Oklahoma. A look at the geology of this are showed that the Magnitude 5.6 earthquake occurred on an existing fault line which had been building stress for millions of years.

As far as fracking-induced earthquakes, the UK example is pretty well worst-case scenario. Meaning, this is one concern we shouldn’t be wasting our time worrying about.

Groundwater Contamination

If you do want something to worry about, here’s where I’d start. Hydro-fracking gets its name from the vast amount of water (“hydro”) it uses to fracture (“fracking”) the geologic unit. However, water is not the only thing being pumped into the ground. As we already discussed, sand is mixed with the water in order to prop open induced fractures and maintain a high permeability. But water and sand are just the main ingredients, multiple other chemicals are added to the mix and make up about 1-2% (by weight) of the fluids being injected into the well.

Why all the chemicals? They all have their uses: biocides keep algae and other organisms from growing in the well network, acids polish the metal well casings to keep metal shavings from damaging the pumps, other chemicals adjust fluid viscosity and act as emulsifiers. While some of these chemicals are perfectly safe (even for consumption), many can be toxic or carcinogenic.

According to the U.S. House of Representatives Committee on Energy and Commerce, over 2,500 hydraulic fracturing products containing 750 chemicals and other components have been used between 2005 and 2009. In the same report, the committee has compiled a list of all 750 chemicals known to be used in hydraulic fracturing applications.

Hydro-fracking fluid is the “secret sauce” of the gas and oil world. While we may know what chemicals could be in the mixture, the concentrations of these chemicals are “trade secrets” and, therefore, companies do not have to reveal how much of any chemical is in use. In other words, any concentration of products could be used, and the company is OK to use it as long as they tell the customer (permitting agency) that they used some combination of milk, eggs, and peanut (BTEX components, methanol, and boric acid).

The main concern here is groundwater contamination. Millions of people get their water from groundwater resources. When you’re pumping unknown concentrations of multiple (sometimes tens or hundreds) of chemicals into the ground, you want to carefully monitor where those chemicals go. Until recently, no such monitoring was taking place. In fact, oil/gas companies claimed that their process recovers most (~99%) of these chemicals once fracturing was completed, and that was good enough for them.

This year (FINALLY) the U.S. Environmental Protection Agency began one of the first large-scale studies on the effects of hydraulic fracturing on groundwater resources. The study will monitor wells at varying distances from hydro-fracking operations in seven different study locations across the United States. The idea being, if high concentrations of chemical X are detected around fracking sites, and diminish as you move farther away, there is a high likelihood (if not certainty) that fracking operations are the source of chemical X in groundwater. According to the U.S. EPA website, preliminary results will be available by the end of 2012, with the final report completed in 2014.

Another study conducted by the University of Texas at Austin, Jackson School of Geoscience (JSG) has already yielded preliminary results, which shows no direct link between hydro-fracking and groundwater contamination at any of the sites they studied. I believe the EPA study will show the same. Why is this? Most drinking water aquifers (porous, permeable geologic units which act as reservoirs for groundwater) are within several hundred feet of the surface while most hydro-fracking operations take place many thousands of feet lower. The chances that existing or induced fractures create hydraulically conductive pathways vertically between thousands of feet of rock is very slim, even with the induced pressures caused by hydro-fracking.

The JSG study did identify more likely sources of contamination. The first is surface spills of waste water associated with hydro-fracking operations. Any fluid used to “frack” the shale is recovered and either recycled for use in the next well, or disposed of. If this fluid is spilled on the ground, the same chemicals may seep down through the surface sediments and rock, eventually making its way into an unconfined aquifer.

However, if you’re going to look at surface spills for a reason to shut down hydro-fracking, you should also shut down sources of surface spills which can exceed those done by fracking operations. Dry cleaning facilities (perchloroethylene) and at least 80% of gas stations (BTEX compounds, methyl tertiary butyl ether, polynuclear aromatic hydrocarbons, and a host of other chemicals) have leaks all the time. I’ve worked full-time for years dealing with environmental remediation for these sites. If the leaks weren’t there, I’d be out of a job. Scary statistic: over 2,000 confirmed underground storage tank system releases are currently in corrective actions in the state of Ohio alone. I’m not justifying spills of any kind, just pointing out that they’re not exclusive to hydro-fracking.

Speaking of leaks, the second indirect source which JSG noted was leaking of fracking fluids from the well itself. If the well casing was not installed properly, there’s the possibility that some fluid could leak through a seam in the casing as it passes through the aquifer (remember, in order to get to the shale to frack it, you have to first drill vertically down through the overburden rock, including any aquifer). If this happens, you’re putting chemicals directly into the groundwater. Again, the hydro-fracking itself isn’t actually causing this contamination. Of course, the chemicals used for fracking wouldn’t be there to contaminate anything if hydro-fracking wasn’t taking place. The issue here, however, is competency in the well installation process. Well installation needs to be conducted the right way every time in order to avoid any leakage. If there’s fracking fluid leaking from the well casing, their product (oil or gas) will leak, too…meaning lost profits. It’s in the company’s best interest, to make sure this doesn’t happen.

Another concern with groundwater contamination isn’t due to the fracking fluids, but the release of naturally occurring methane gas. This is thought to happen when induced fractures create pathways for the gas to “leak” out of a fracked geologic unit, and make their way into overlying aquifers and into our drinking water. There was a famous case, demonstrated in the documentary “GasLand“, where a homeowner turned on a faucet in their home and was able to light it on fire due to the amount of methane gas present. A number of homeowners have reported this problem following the commencement of nearby hydraulic-fracturing operations.

Two things to note. One: these are all properties where the residents have private water wells supplying their home, usually in deeper aquifers. So if you receive municipal water, you shouldn’t worry. Two: geology, geology, geology. Methane, as I mentioned, is naturally occurring (it is natural gas). In fact, it occurs all throughout the stratigraphic column in the areas of Pennsylvania, New York, and West Virginia where these claims are common. A study by Penn State explains that sources of methane in water wells can range from gas wells, coal mines, landfills, and simply natural deposits.

Does this mean that hydro-fracking was not the cause of methane in drinking water supplies? No. But it also means it’s not definitely the source, either. In Pennsylvania, where the “fire faucet” was documented in “GasLand”, a number of the residents jumped on the bandwagon of blaming hydro-fracking for methane in their wells. However, in the same area, multiple residents reported that they’ve always had methane in their water, as long as they’ve lived there and well before hydro-fracking began. In the same area, methane deposits are naturally occurring in geologic units where it can easily be recovered by water wells.

Of course, the EPA recently published results from a study in Pavillion, Wyoming where methane in water wells had a similar isotopic signature as methane from deep sources – near the depth of fracking operations – and did not match that of shallower deposits of methane usually associated with “natural contamination”. So, it’s a definite possibility and one that needs to be studied more.

What does it all mean?

From everything I’ve come across, these two concerns pretty well cover most common “threats” associated with hydraulic fracturing operations (many other concerns fall under groundwater contamination). We’ve established that earthquakes pose effectively no risk to people or structures at the surface. Groundwater contamination, on the other hand, is where our concerns should lie. Even then, preliminary studies show it’s not the actual fracking that’s causing problems, but a lack of consistent, regimented installation practices which prevent surface spills and leaking at any point in the well casing.

The general public and government both need to better understand this process and should insist on more strict regulations of well installation and hydro-fracking operations. Required monitoring programs should be in place to protect groundwater resources by taking background (pre-operation) samples and comparing these with samples taken throughout and after the fracking process. If this is done consistently, it would lead to identification of well sites where leaking is taking place, and if it shows no changes in groundwater chemistry, this could even redeem hydraulic fracturing from the stigma it’s associated with. I’d say this is a pretty good incentive for oil/gas companies which have been claiming how safe this practice is for years without any proper, scientifically sound evidence.

What we all need is proof. With the finalization of the JSG study, and the upcoming results of the U.S. EPA, we’ll at least have a couple reliable sources for reference. You can bet that these will spark new studies to verify the results, which will give us even more scientific studies to look to for a springboard to action (or sense of relief) on the issue.

Let’s wrap it up already!

I recently attended a meeting in Pittsburgh, PA, where I spoke with a high-level geologist with the Pennsylvania Geological Survey. As Pennsylvania is currently one of the hydro-fracking hot spots in the country, our conversation inevitably led to the controversies that surround the process. I was happy to learn that the majority of geologists who study the geology in “fracked” regions have the same views as expressed above, and that the enhanced recovery of fossil fuels can be very economically beneficial. Unfortunately, many residents don’t fully understand all the variables involved (namely geology), and see it as a definite menace. For this reason, legislation banning the practice of hydro-fracking gets passed in cities or counties across the country.

One thing that stuck with me from my conversation with the PA Geological Survey geologist, was his closing remark (so to speak): “I hope Ohio doesn’t make the same mistake Pennsylvania did.” By this, he meant that there’s been a lot of resistance to hydro-fracking in PA…though it’s still in use (and doing pretty well). He explained that he fully supports the practice – while agreeing that there needs to be more strict oversight to ensure less chance of cutting corners (resulting in spills and leaks) – and thinks Ohio residents should embrace hydro-fracking techniques as a way to exploit the Utica Shale gas reserves.

Final Thought

A lot of what I’ve written seems to be supporting hydraulic fracturing. I do feel the process is no more hazardous than other methods of natural resource exploitation. However, I feel obligated to stress that the truth about hydraulic fracturing is that there are definite problems which need to be resolved in order for us to be certain that the technique is safe. By conducting multiple, unbiased scientific studies on the effects of hydro-fracking on groundwater supplies and the environment, I believe a solution may be found. Whether it will favor either side of the issue, I don’t think anyone really knows for certain. With what I do know, I can make the educated guess that we won’t be seeing hydraulic fracturing disappearing anytime soon.

Further Reading

While the information provided above was all pulled out of my head and typed out here, I’ve done a lot of research to develop this understanding of hydraulic fracturing and the risks associated with the practice. Below, I’ve included a small subset of more recent articles and posts by other geologists which cover some of the information above and are easy reads for pretty much anyone.

• The United States Environmental Protection Agency page on Hydraulic Fracturing (includes updates on groundwater contamination study)
• Article on IthacaJournal.com about potential for fracking-induced earthquakes (looks at both points of view)
• An article in NewsOK covers the oil/gas industry perspective fairly concisely (warning: blatantly one-sided)
• The University of Texas at Austin preliminary results on effects of hydro-fracking on groundwater
• The Cuadrilla Resources report on link between hydro-fracking operations and earthquakes in UK
• “Frickn’ Fracking…” posted on The Dynamic Earth is a great (an entertaining) look at fracking-induced quakes and why it’s not what we should be worried about.
• NY State has newly proposed regulations for hydro-fracking. Public comments are being accepted through Dec 12, 2011 and four public hearings are left (as of the date of this post).

***UPDATE – 12/8/11***

Yesterday, the EPA released draft findings on their Pavillion, WY study site.  The findings indicate that chemicals used in hydro-fracking have been detected in groundwater from samples collected at two deep monitoring wells.  The concentrations of these chemicals are below the standard health and safety standards (which means the water is still safe to use/drink).  However, this indicates that, in this specific case, there is a possibility of connectivity between the zone of fracking and the overlying aquifer.

I feel I must stress that these findings are specific to the study site.  The geology here, and even the method of hydraulic fracturing used, is unique to the area.  The EPA report even states that you cannot and should not assume the results here can be applied elsewhere.  For example, the geologic unit being fractured is much closer to the overlying aquifer than is typical.  Also, fracking operations are usually in much more remote locations…this one being in close proximity to water wells.

With that said, stay tuned as the EPA begins to release more data on this and other sites.  If you’d like to read more on the Pavillion, WY study, you can see the press release, draft report, and supplemental info here.

The Badlands of South Dakota

When I first laid eyes on the Badlands of South Dakota, I remember thinking to myself “This is pretty cool”.  Now to be fair, I’ve said this many times during my trips to National Parks like this one.  But when you see something like this up close, you can’t help but just stand in awe.  What makes something like this even more amazing is a little knowledge of how it came to be.

The Badlands are situated in southwestern South Dakota between the Cheyenne River to the north and White River to the south.  Sediments (sands, silts and clays) deposited over the region over the late Cretaceous through the Oligocene form the majority of the sedimentary stratigraphy in the park.  Nearby volcanism deposited intermittent ash layers.  The National Park itself covers just under 1,000 square kilometers.  While today the region is pretty arid, during the Oligocene (40-25 mya) it was warmer and rich with life.  Before that, about 68 mya, the badlands were at the bottom of a shallow sea (which is represented by the fossil-rich Pierre Shale).  This area is known for having one of the largest and most complete assemblages of Eocene and Oligocene mammal fossils in the world!

A topographic profile (N-S trending) shows the Badlands are situated on the edge of a topographic high to the north, known as the uplands.  This results in “The Wall”, which is aptly named due to the high relief between the uplands on the north side of the badlands and the base of the wall.  This wall is where the town of Wall and its very successful tourist attraction, Wall Drug, get their names.  If you’ve ever driven on I-90 through South Dakota, you know what I’m talking about (and most likely stopped there just to see what all the signs were about).

The wall began as a scarp on the northern side of the White River.  As erosion chewed away, the wall migrated northward, and continues to do so.  This leads to an important point: the Badlands are disappearing.  The ridges, pinnacles, and ravines that make up the Badlands are formed by water and wind erosion over time following regional uplift which occurred about 5 mya.  The erosional processes that created these features are the very same that are tearing them down.  Erosion here occurs at a rate of about one inch per year.  Runoff water carries sediments from the easily weathered sedimentary units and volcanic ash to the White River.  Eventually, the Badlands will erode away… completely.

What I didn’t anticipate was what I found when I finally embraced Twitter (and later Google+) only a few months ago: a whole community of geobloggers, just like me! Well, not just like me (we’re all different in our own way), but an online collaboration of earth science professors, students, professionals, and enthusiasts with a whole range of interests and ideas. I didn’t even know the term “geoblogger” three months ago, let alone that I am one. Needless to say, this was a very exciting discovery.

To celebrate this find, I’ve finally gotten around to listing some of the geoblogs I read the most often over on the right. →

I’m sure I missed a few, so if you happen to be a fellow geoblogger and would like your site listed, too, just drop me a line and I’ll have it up within a couple days.

If you’d like to see an even larger selection of geoblogs, head on over to Ron Schott’s blog where he seems to have kept pretty good track of what appears to be every geoblog ever.

On a completely separate note, due to the addition of the Geobloggers section, I’ve moved things around on the site a little, but no major remodeling yet, so you shouldn’t have trouble finding any links, etc. (but let me know if you do). I’ve also realized that it’s been a while since I’ve published a Friday Photo post. I have one in the works for next week….hopefully.

Until then, take some time to explore the rest of this site and enjoy some of the other excellent earth science blogs out there!

Collapsed buildings in the Van Province of Turkey have trapped an unknown number of citizens following Sunday's Magnitude 7.2 earthquake. (Source: AP)

Yesterday’s earthquake in Eastern Turkey (near the City of  Van) has resulted in extensive damage due to it’s shallow depth, it’s large magnitude (M 7.2), and it’s proximity to populated areas (well over 300,000 people living within 10 miles of the epicenter).  Combine that with not-so-strict building codes and the region’s geology, and you’ve got problems.

Unfortunately, no time on my end to write much about the mechanisms and consequences of the quake…but if you’d like to learn more, this post by Chris Rowan is a good place to start.  Rowan specializes in tectonics and is one of the authors on Highly Allochthonous - another great geology blog that I recommend reading.

Something else you may want to check out is this powerpoint presentation by the University of Pittsburgh’s Department of Geology and Planetary Science, which presents seismograph records from the Oct 24, 2001 earthquake in Turkey, and discusses the geology of the region as well.  (Note that the conversion into google docs seems to have changed the aspect ratio and jumbled the text on some of the slides).

You can also find lots more detailed info about the Turkey earthquake on the USGS website.  For those of you who don’t need all the nitty gritty, don’t forget you can find a quick crash course in plate tectonics in some of my previous posts – like this one.

Students learn about the Sharon Sandstone during their Intro Geology field trip.

But the students aren’t here solely to see what is missing.  The park is full of geological lessons: sedimentary structures (cross bedding and weathering patterns), different depositional environments (braided streams and sea floors), slope stability (debris flows, rock falls, and creep), river evolution, ground water and contaminants (the Sharon is a major aquifer in NE Ohio), glacial geomorphology, and many more.

It’s always fun to lead these trips and see that look in the students’ faces when they finally get why geology is both fun and useful!

As I stepped outside Saturday morning I had my first look at Anchorage. Beyond the buildings and bustling streets were towering mountains and Pacific waters. My trip had officially begun. Over the next few days I would see why I was right not to try and imagine the landscape that was hidden by the night’s darkness when I landed.

My trip to Alaska was spurred by my research. In just under a week after my arrival, I would be presenting the current status of my work at this year’s Association of Environmental & Engineering Geologists (AEG) National Meeting. By arriving several days before the conference even started, I not only gave myself more time to fret about refining my powerpoint and deciding on what I was going to say, but allowed myself time to get out and explore some – if only a fraction – of America’s largest state.

Glaciers in the Chugach Mountains, south of Anchorage, AK

Saturday: Glacier Cruise

Today I would attend a field trip planned through the AEG National Meeting on which I and about 50 other meeting attendees would ride a train to Whittier, where we’d then hop on a boat to view the wildlife, scenery, and glaciers that populate several of the fjords in Prince William Sound. On the down side, it was overcast and raining almost the entire time. On the up side, the trip was a blast, the rain let up for a while, and the glaciers were so blue it looked as if the cruise companies pay good money to have the them spray painted in an effort to keep tourists coming.

Surprise Glacier, located in Harriman Inlet, Prince William Sound, AK

Lucky for us, the blue color of the glaciers is accentuated during cloudy days…so believe it or not, the pictures you are seeing are not doctored up. Why does this happen? It’s all due to the absorption and scattering of light. Ice – like water – absorbs shorter wavelengths of light (the red end of the visible spectrum) while reflecting and transmitting longer wavelengths (blue end of visible spectrum). The longer the path that light takes and more scattering before it reaches your eyes, the more blue the glaciers will appear. On cloudy days, the light is already being scattered through the cloud before even reaching the snow and ice…this extra step results in more blue!

Glacier beyond trees

What was even more astonishing was the sheer size of these “rivers of ice”. Harriman glacier, for example, is a mile across at the water (and easily over 100 feet tall). Pretty big. With nothing for scale but rock, water, and more ice, it was hard to comprehend the size of the glacier even though it lay right before me. A later measurement on a map revealed the tour guide wasn’t exaggerating.

Sunday: Seaward to Seward

On day two, a few of us took a rental car from Anchorage to south Seward. During the trip, we visited Exit Glacier only eight miles outside the town and the only glacier in Kenai Fjords National Park to which you can hike. Unlike what the brochures made it sound like, you can no longer touch the glacier from the trail. After speaking with the park ranger at the head of the trail, we found that it’s been about 10 years since the trail actually went right up against the glacier itself (evidence of the glacier’s retreat back up to the Harding Icefield). However, it’s still near enough to throw a rock at and well worth the mile hike to the “Edge of the Glacier” where you can not only get a very close up appreciation for glaciers, but see some amazing views of the surrounding Kenai Mountains.

Exit Glacier from across outwash

A sign marks the location of Exit Glacier in 1998.

Monday: Denali

Monday was Denali Day. The drive there was long. Especially when a good two hours of it were through relatively flat landscapes where the only things to see were trees. Yet, the changing colors of the leaves made the drive go by fast…even with the numerous stops to take photos. Many of the peaks of the Alaska Range were quite visible along the way (see below). To my dismay, North America’s highest peak – Mt. McKinley – decided to remain elusive behind a cloak of clouds. At over 20,000 feet (6,194 m) above sea level, McKinley (often referred to by its native name “Denali”), is one of the tallest mountains in the world, coming in a little less than 9,000 feet under Mt. Everest (the world’s highest peak). When measured from base to peak, however, McKinley is actually taller than Everest by 3-4 thousand feet! I’m pretty sure we were able to get a glimpse of part of the mountain…but a return trip to Denali N.P. is warranted in order to finally see this natural wonder.

First glimpse of the Alaska Mountain Range

With the rental car due back by that evening, we ended our exploration of Alaska – or rather, a mere sliver of the state – and returned to Anchorage and the conference for which we came. The rest of the week went great with many very good presentations and events. Lots of fun and learning! My presentation went well on Friday (at least I felt that it did) and the week was over seemingly right after it had begun. After one more long day of travelling, I returned home to write this post…well, maybe I took a week off in between.

Outwash plain at the base of the Alaska Mountain Range

In attempting to keep this post fairly short, I left out what most of my days of exploring were all about: the drive. The scenery that you pass on the way to any one place is as much a part of the adventure as actually making it to your destination. Wide open fields, dense forests, tall mountains covered in ice and glaciers, huge glacial valleys, braided streams over the gravelly outwash plains, the tidal waters of Turnagain Arm, wildlife…I feel as if this list could go on forever. That’s to say nothing of all the great exposures of the area’s rich geologic history. The southern boarders of Alaska are some of the most tectonically active locales on Earth. A great blend of ancient processes preserved in the region’s geology, superposed by the modern structures and deposits created by the same processes.

During our days in the rental car, we easily added hours to our drives due entirely to our “picture stops.” Thanks to these short breaks from driving, I returned from Alaska with well over 1,000 photos from my first three days alone. If you ever get a chance to visit Alaska, make sure you give yourself plenty of travelling time…you won’t regret it.

So far, I’m halfway there and waiting on my connecting flight to take me the next into Anchorage.  My initial flight from Ohio to my connection in Denver, Colorado was cancelled and I was placed on an earlier flight.  A much earlier flight. In fact, I arrived here in Denver 12 hours before my next 2,400 mile flight leaves.

Surprisingly, I’ve managed to keep myself busy without springing for a cab to take me downtown.   I’ve never been to Alaska before, but from what I’ve heard and read, it is well worth the wait!   When I return, I’ll be posting pictures from my scheduled glacier cruise and – if I finish preparing my presentation – a tentative trip to Denali National Park (no guarantees on the latter).