Tuesday, June 5, 2018

Old Faithful

Old Faithful about to blow sky high. My photo.

There really isn't an option of talking about Wyoming without talking about Yellowstone and Old Faithful, especially because most people think Yellowstone is in Montana. Yeah, like 5 minutes of it (it's a sore spot for Wyomingites).

Members of the Washburn-Langford-Doane Expedition spotted Old Faithful on September 18, 1870 (of course, Native Americans in the area had long been aware of Old Faithful).

Nathaniel P. Langford wrote an account of the expedition:

In another part of Langford's diary, he described the complete lack of understanding by white folks of the delicate ecosystem of geysers. Old Faithful was sometimes used as a laundry in the early days:

Monday, March 5, 2018

Freezing Water

Sorry for the hiatus everyone! We added an addition to the family! Lil' Dude will join Sweetie and the hubby in our discussion of culture and science! 
This morning, for example, we were all having fun in the car as it was warming up....

The phenomenon is called "supercooled water." It only happens when water is cooled very slowly, such as in your car overnight. By cooling the water slowly, the water remains liquid below its freezing point. When you disturb the bottle, the water then has enough energy to start growing ice crystals. This process is called nucleation, because it encourages the molecules in the liquid to form a crystal-like nucleus onto which others can then latch. The kick-start can be given by a piece of dust, a rough spot on the surface of a container, or the shock wave generated when you hit a bottle sitting quietly in your drink holder.

Wyoming. Where science nerds have fun in the freezing weather....

Thursday, September 14, 2017

Hot spots and Yellowstone.

We're gearing up for a trip to Yellowstone. We haven't been back in a few years, so I'm excited to see what's changed, as well as taking Sweetie there for the first time!

Yellowstone is so unique because of the mixture of magma and water, from a tectonic "hot spot" that's been in this mantle location for around 20 million years, a the water that is naturally in the crust at this location.

Everyone kinda understands Plate Tectonics, yeah? The idea is that the top crust of the planet is made up of rigid plates that are sort of floating on the upper mantle, so they move around, like a Slip n Slide. This movement causes most of the geological activity on the planet, like earthquakes and volcanic eruptions.

Most, but not all.

Mantle activity known as "hot spots" are thought to be the result of plates being subducted under each other millions of years ago. See, when one plate is forced under another, it starts to loose water as the water in the crust heats up, being surrounded by molten magma. That water then "irritates" the mantle, to say it simply. And even once the plate has long been completed subducted and melted away, the irritation remains, causing the hot spot.

So a new plate moves over this area of the mantle, and magma wells up from the old irritation. Essentially, hot spots are thought to be evidence of much, much older plate movement. Currently, the hot spot is over a good chunk of Wyoming (remember, the hot spot doesn't move, the plate does!).

However, that explanation isn't universally accepted by all geologists. The other hypothesis is that lithospheric extension permits the passive rising of melted magma from shallow depths. This isn't a really great hypothesis, as it can't really be tested, even in models, as we have no idea *how* exactly crustal extension would allow magma to bubble through it. Hopefully, we'll have an answer either way someday.

There are lots of other hot spots around the globe, Iceland and Hawaii being the more famous. But the crust in Northern Wyoming is very different than the crust over other hot spots, because it's got so much water inside it. There's an entire network of caves and underground lakes in this region, as well as a lot of natural gas. That's the reason for the numerous geysers and other thermal features in Yellowstone National Park and the surrounding area.

Along WY state highway 150

Hello! Sorry it's been more than a few days since my last post. This summer was super busy. We took a road trip down to Texas (in the middle of the summer!) and then drove up to Spokane, WA for a quick visit. I also spent about a week camping near Evanston, doing some archaeological work.I'll post more about those trips later.

We drove south to Heber City, Utah (which a great "Swiss village" if you're looking for something different), but we took a slight detour. State highway 150 is an *amazing* road which winds through the mountains and a huge aspen grove. Yes, it is a little windy - the mountains didn't leave road builders a lot of options. But it's well worth it, with plenty of pull outs to enjoy the views or to settle your stomach. :)

From Mapquest.com
I wouldn't suggest this road once the weather changes, as there are no services between Evanston and Heber City.

Wednesday, June 14, 2017

From South to North

We just got back from a quick two-day trip to Spokane, WA, and we took "the scenic route" back, along US 30. Just taking the little bit of extra time to drive these amazing historic roads instead of whizzing by on the Interstate is worth it. There were all sorts of road cuts and rivers (the Bear River!) that we wouldn't have seen otherwise.

We decided to start our scenic journey in Cokeville, WY, which is a wonderful old railroad town. Though it was pretty funny to see a sign for "Museum" off the main road. We'll have to go back and see what kind of museum that could be!

US highway 30, picture from Wikipedia Commons.

Sweetie was exhausted once we got home, but she loves traveling. And hotels. Remember though, it's important for kids to stay hydrated during long road trips, even if that means extra bathroom breaks. :) Keep water in the car at all times!

Here are a few pictures:
Ok, not everything is super-exciting....

A little slice of Wyoming heaven....
After an event-filled day, the driver needs a break!

 It was hard not to stop at Fossil Butte National Monument as we passed. But as we usually go there several times a year  anyway.....

Side note: Dillon, MT is *awesome*. A small town that has been really thoughtful about how they want their town to look in the future. They've clearly worked with local businesses to help them thrive without gentrification. Would totally move there if I wanted to open a business. 

Wednesday, May 31, 2017

Help fund this amazing Kickstarter!

I'm not affiliated with this Kickstarter project, but it's amazing. Donate if you can!

Friday, January 6, 2017


So, a student brought in her china that she got from her grandparents. Apparently they bought this set in England in the 40s. It's beautiful, but I'd never seen that type of brown alpha-numeric marking before. It didn't strike me as something the grandparents would write on their set, it looked to me like a catalogue number from the manufacturer.

So I did a simple Google search. Sure enough, I found other people asking about the brown cataloging symbols for this manufacturer.  And the date seemed off - they didn't seem to be making this set in the 40s.

I'll update here when I find out more. I'm a member of a listserv that deals in Historical Archaeology, so it was easier to put the pictures here and let other member look at them. Plus, I thought y'all would want to see them. Not microwavable!

Coming soon: The History of Pottery!

Wednesday, January 4, 2017

The Culture of Winter

I guess I'm in a wintry mood. Not quite got the "Holiday Spirit" yet (it's COLD, darn it), but I am focused on the snow outside my door.

I've lived in a lot of different places. But the best "Winter Culture" I've ever experienced was in Minneapolis. Zuerich, Switzerland, comes in a close second, but I still miss Minneapolis' Winter Carnival, the Skyway, the litter heaters at bus stops. All of it was created with a cultural understanding that one should be outside in the wintertime.

And that comes from the Scandinavian immigrants who populated the Great Lakes region in the early 1800s. Being so far North, the area gets a lot of sunlight, but little UV radiation (it's reflected away because of the angle the northern regions are to the Sun). So people that lived there realized over time that the healthier kids were the ones that spent a lot of time outdoors. This has to do with the relationship of skin color to the production of Vitamin D, but that's a story for another blog post. :)

The culture grew around this realization. And when many of them moved to The New World, they took this belief that children should play outside A LOT with them. Here's a great link if you want to know more:


Wyoming has a slightly different relationship with winter. It's more of a "hunker down" mentality that serves people well in the West, where resources during the winter are so scarce (particularly in the past), you might not make it to see Spring.

When people have the app for the Wyoming Department of Transportation on their phone, you know something's different. Heck, I don't think there are too many other states that even HAVE an app for their DOT. And when you have to really plan for a night stay along I-80 because there is a high probability of it being closed at any given moment, you know this is serious stuff.

I see many comments on social media, or even just on TV, that tell me that the rest of the country thinks The West is a bit ridiculous. The idea of scare resources boggles most Americans in other places.

But it's still true here. UPS actually charges a surcharge to deliver to most locations in Wyoming, because the entire state is considered "rural delivery." My town has one bakery. It cannot service the entire town, and so therefore it doesn't even try. They make only what they can sell between 6am and 2pm every day. So if the gas station runs out of (anything and everything), they have to wait for a truck to come from another state. This applies no matter what side of Wyoming your on.

All of this is worse in the winter, when these supply trucks can't get to some of the small towns (every town in Wyoming is a small town, btw) reliably. So the conservation of resources is still a survival skill here.

To be honest, it's where I'd want to be in a zombie apocalypse. Because people here still know how to make stuff, and save stuff. Watch out, America.

And if you feel like reading about how famous Wyoming is: The Five Coldest Cities in the World

Monday, December 5, 2016

Let it snow!

Winter is most definitely here. The snow is packing down, and the drifts are growing. Which is why we haven't been doing much traveling as of late. Probably won't go very far from home until March.

Which made me think, as I walked across the field to the office this morning. As I looked at the snow at my feet, and felt the snow scouring my face like sandpaper, I realized that I had never thought of snow as if it were sand.

But dry snow (a high snow to liquid ratio), for the purposes of considering it's impact on the landscape, is exactly that.


I thought I should include an explanation of "dry snow", as it seems a rather contradictory term. The different terms for snow, which include wet snow, granular snow, corn snow and dry snow are categorized based on the "snow to liquid equivalent".

The snow-to-liquid equivalent is a ratio indicating the amount of liquid precipitation produced as the snow melts. In order to calculate this, one uses both the Earth's surface temperature as well as the temperature of the troposphere. The troposphere is the bottom-most layer of Earth's atmosphere, which contains 75% of the atmosphere's mass, and most of its water vapor.

Dry snow occurs when both the troposphere temperature and the surface temperature fall below the freezing mark, causing the snow to have a minimal amount of liquid, and more air pockets within the lattice structure at the microscopic level.

Since dry snow is less dense than wet snow, and not as "sticky". Dry snow's lack of stickiness makes the snow unlikely to stick together, hence it's sand-like characteristics.It also makes terrible snowmen and snowballs.

Back to dry snow:

So, essentially, the snow my backyard is acting like a dune field. Though I do see sediment buildup on some of the older so, which indicates a windbreak. So if you want to know where the wind is consistently the weakest, look for the dirty snow.

The snow piles look like the beginnings of traverse dunes, indicating a constant prevailing wind direction, and very little vegetation.

See the elongated piles front left to right?
You don't need to travel far to see wonders. You can find amazing things right at home. Start by looking down at your feet. Or out your front door, apparently.

Monday, November 21, 2016

Minerals, Rocks, and the Periodic Table

Minerals make up rocks. Rocks are composed of minerals. Minerals are made from the bonding of elements. Elements consist of atoms all of the same type.

These statement tend to confuse the average beginning geology student. That's the consequence of not having enough science in public schools, which directly correlates to the amount of testing done in public schools. I might write about testing in schools at some other time, but for now, let's science. :)

The periodic table always fascinated me when I was younger (I started college as a physics major). There's so much information available in such a small graphic. For those that don't know too much about it, the periodic table is a tabular arrangement of elements, ordered by their atomic number (number of protons), electron configurations, and recurring chemical properties. This ordering shows trends of the different elements, such as elements with similar behavior, in the same column. It also shows four rectangular blocks (colored) with some approximately similar chemical properties. In general, within one row (period) the elements are metals on the left, and non-metals on the right.

 The first 94 elements exist naturally, with Hydrogen through Iron being made in the fusion of a star's reaction while it is alive, and Cobalt through Plutonium being made during the process of a Supernova. Elements with atomic numbers from 95 to 118 have only been synthesized in laboratories or nuclear reactors.

 Under an international naming convention, the groups are numbered numerically from 1 to 18 from the leftmost column (the alkali metals) to the rightmost column (the noble gases). Previously, they were known by roman numerals. In the U.S., the roman numerals were followed by either an "A" if the group was in the s- or p-block, or a "B" if the group was in the d-block. The roman numerals used correspond to the last digit of today's naming convention.

 The table relates all sorts of other characteristics, including crystal structure, melting temperature, and how likely the element is to be found bonded with other elements. This helps scientists understand how matter relates to each other, and the nature of chemical bonding. Chemists and astrophysicists essentially have the same question: WHY do certain elements like to bond with each other over other elements?

But that's a question for a different post. Or another degree. :)