Monday, August 1, 2011

Ghost Town Tuesday - Dividend, Utah

Ghost towns are frustrating.

The works of humans are amazingly short-lived. Say you woke up one day and somehow you were alive in the year 1880. I don't have the energy to think up why this has happened. Maybe you've had a stroke and just think you are in the year 1880, I don't know. Either way, what is the first thing you do? If Back to the Future III has taught us anything, it's that you first need to dump a large load of manure on the town bully to establish yourself as the hero.

After that, we don't really have a script for what to do next. It is my opinion that the first thing you should do is build some sort of store out of wooden planks (as is the style) and sell overpriced, watered-down whiskey to filthy people with bushy beards wearing those ill-fitting suspenders. Like this guy.


(I just needed a picture of an old prospector. I don't know why he is panning for little multicultural human torsos. Ignore that part). Expect to do this for a good 6 or 7 years until you get shot, drink some bad water and get a gut worm, or until the nearby mines run out of ore. After that, what you do is none of my concern. But what about your store?

Without maintenance, your average wood-plank structure will probably last a good 30 years before the weather or gravity or teenagers finally destroy it*. If it was built by some sort of legendary wood-plank builder company, it may even last up to 90 years. But that's about all you are going to get. After that, it will fall down and re-enter the food chain and that will be that. And therein lies the problem with ghost towns.

The ghost town of dividend has largely re-entered the food chain. In fact, it looks much like a field that has never been populated.



That, my friends, is the town of dividend. While it may not look like much now, it was once a place where things were much less....field-like.

The story of Dividend begins in the grand old year of 1916. Woodrow Wilson was president, cars still made that amusing "Ah-ooo-gah" sound, and deaths from digestive diseases were down while World War I related deaths were way up. But these things don't concern us. Our story centers on this guy....



That kindly-looking gentleman is EJ Raddatz, and it was his dream that gave rise to the town of Dividend. Mr. Raddatz was a prospector (despite the overall lack of beard and blood-alcohol level of 56%) and he had a hunch about a plot of previously unproductive land in the East Tintic Mining District in north-centralish Utah (here)...



Look at that! An old-timesy image of Utah! Taken straight out of an old government document written about the very subject we are covering! I feel it adds an air of professionalism to what is otherwise a pretty lightly investigated post. Go ahead and look at that map whenever you think things are getting too stupid. Anyway, that map was prepared in 1919, so let's update it a little bit....



There. Now we've brought it to the 2000's. That little square in the middle is the area we are looking at, by the way. Let's zoom in....



That last picture got all blurry. Maybe it will be better if you click on it. Anyway, that's an aerial photo of the townsite. You can still see the roadways! What's unusual is that you can't see them from ground level. Ahh, technology. Let's get back to Mr. Raddatz.

Mr. Raddatz knew there were minerals under his feet. We don't know how he knew that, but he knew that he was standing on a great spot for a mine. The year was 1907, and mining was a great way for anyone with a little capital to strike it rich (or lose everything trying). Mr Raddatz was no exception, so he created the Tintic Standard Mining Company and released a million shares of stock in an attempt to raise the funds he needed to find the good stuff deep within the earth. To help him with the actual digging, he hired this man....




That there is John Westerdahl, an experienced miner and first foreman of the Tintic Standard Mine. Mr Westerdahl and crew dug and dug and dug this shaft.....






(That shaft has since be reclaimed, so this may be the only time you ever get to see it. Bask in the glory!) For months they dug blindly into the hillside until the money started to dry up. The miners started to get paid in shares of stock instead of money, which wasn't great at the time as the mine had yet to produce anything of value. Most miners sold these shares or traded them for booze. Then one day they noticed a weird gas coming out of the shaft....



The government geologist inspected the site and determined that the gas was coming from some large sulfur-rich ore body! At last some good news! In 1916 the miners finally found the big pay day. At a depth of 1,200 below the very place that Mr. Raddatz was standing years before existed a massive lead-silver deposit that would prove to be one of the largest strikes in the Tintic District. It was named the Tintic Standard Mine.





(Look close, you can still see the words "Tintic Standard" written on the tanks). By 1918, a town had sprung up around the mine. At first it was just housing for the miners, but soon it also featured a school house, a store, barber shop, pool hall, a post office and hotel. A newspaper, The Standard, even showed up from 1924 to 1925. A population 350 men, women and probably some children called this land home, and anyone who had kept their stock certificates were rewarded with over one and a half million dollars in dividends from the mine by 1922. As was usual for such a town, the mine towered over everything....



The town was to the east of the mine and consisted of a few streets of nicely organized houses.



The mine complex consisted of the shaft (actually 3 shafts. Shafts are an important part of any mining venture), the assay house....



(You may be saying "Hey! How do you know that's the assay house? That could be any pile of rubble! I hate this blog so much!" Well, I know because the ground is littered with these little assay cups....



(And where do we find assay cups? Why, in the assay office. So that's how I'm guessing this was the assay house. So get off my back already.) Also included was a warming house, where the miners could warm up after being down in the mines....






(The warming house also made it difficult for miners to "borrow" pieces of rich ore for themselves. You see, if rich ore was struck and you could sneak it out of the mine without that jerk of a supervisor seeing you, then you could trade that ore in for all sorts of whiskey. This practice was known as high-grading, and mine owners hated people who did it. Almost as much as cave-ins and the environment).

Also included was the company store....



One of these things....



A railroad to get the ore from point A to point somewhere else....






And a variety of things that fall into the "misc" category....









Look! Here's an old mine elevator! This little bugger made countless trips up and down and back up again before being forgotten on a heap of waste rock. There's a lesson here kids. No matter how hard you work, everyone ends up sitting on a pile of waste in the end.




Ore from the mine assayed as high as 80 ounces of silver to the ton, and 22 percent copper. These are good numbers for a mine. It's like having a blood pressure around 110 over 70, or getting 40 miles to the gallon. The ore was chased down to the 1,600 foot level, with galena, tetrahedrite, pyrite and sphalerite forming the most valuable ore. This little guy showed up from time to time too....



That is a mineral named argentojarosite, and if you love silver, then get this mineral drunk and take it home to bed. It's basically silver with some yellow mixed in. The Tintic Standard Mine was the first place this mineral was ever discovered, and as such it has become the "Type Locality" for it. It's an honor to be considered a "type locality" for a mineral. It's like being the kid who finally breaks the pinata, or getting a seat on the bus that isn't covered in urine stains. Pretty great.

And so, the mine pumped kept pumping out minerals. For a while it was the leading silver producing mine in the United States, and gained a relatively high degree of fame for being so. In order to process this ore, a large, state of the art mill was built on the western slope of the mountains to the east of the mine, and was named (not surprisingly) the Tintic Standard Reduction Mill.



That mill lasted from 1921 to 1925 before it shut down due to the whole thing going from innovative to obsolete. Kids love painting things on other things, so now the mill looks like this...



At some point during the operation of the mill someone managed to steal a 50-ton ore car of high-grade ore (in an epic example of "high grading" as described above). The ore car was found 6 months later in Mexico, but was as empty as chubby kid's self-esteem. I didn't steal it, but I certainly can see why someone did.

In 1920, the town decided it needed a name. It had been going by the name "Standard" (if you don't know where they came up with that name then you need to read things more closely). The problem with that is that there is a town named "Standardville" in Carbon County, and it was messing with the postal service. So a contest was held to come up with a new name, and the name "Dividend" was selected. Again, you should be able to figure out where this came from too.

I hate to have to remind you, but we are dealing with a ghost town. This means that at some point things have to go down-hilll for the town. Prosperous towns don't just suddenly wrap up shop and go on their way. Only loser towns. And sadly, Dividend's term as a place that exists was nearly up. In 1949, the mine ran out of paying ore and the last shipment was made during that year. Don't feel bad though! During the period it was worked, the mine produced 2,327,148 tons of ore valued at approximately $80,000,000. A tasty $19,000,000 of this total was paid out to lucky mine shareholders who didn't use their shares as toilet paper during the rough times.

With no mine, there was no need for a mining town. And so, as we've seen before several times, the town got flushed down the big ol' history toilet.




The majority of the buildings were removed in the 50's cus if they don't exist you don't have to pay taxes on them. Any houses that weren't removed suffered a teenager-based end (lit on fire). So that leaves us with this....










That is to say, not a whole lot. A few concrete foundations, a few stone walls and probably a whole bunch of ghosts. The mine is really the only item of interest in the area (unless you really like concrete foundations and a few stone walls). It is because of this that I made that rant at the start of this post. Ghost towns never seem to last.

So we leave the once busy town of Dividend. Perhaps one day new mines will be discovered in the area and the town will be re-built and the mines will roar back to life. It's not very likely though. I'm going to go trade my shares in for some whiskey.








*If you have really chased this Astrix all the way down here from that first paragraph, I just wanted to make sure that you all know that I have no idea how long wooden structures will last if they aren't maintained. I hope this was reward enough to justify worrying about it.

Thursday, July 21, 2011

Important Blog Update!

It is my birthday.

At this point all I can do is sit back and remember how excited I used to get over my birthday. When I was younger (and less disgusted with the world) I would spend the days before birthday sitting around wearing this goofy expression on my face and watch Duck Tales.


Sadly, as is true with everything, getting older has taken the fun out of birthdays.



For example, I'm writing this at work. To a kid, the idea of working on your birthday would seem as outrageous as the concept of car ownership.

A lot of people thing that the reason birthdays aren't as much fun in later years is because we become increasingly aware of the limits of mortality. While it's true that an 85-year old probably has more reason to fear the increasingly likelihood of not waking up tomorrow, I don't think that is the main reason that birthdays are less entertaining. I suspect that the cause lays with the decreasing quality/entertaining value of the presents. Kids get great presents




Adults, on the other hand, get decidedly less fun presents. Useful, sure, but less fun.




I'm not saying that I hate getting useful things. Even as a kid you need to get socks or playing with your SUPER FUN PRETEND GUN FUN TIME will become a painful ordeal. What I am saying is that a birthday filled ONLY with useful gifts is equally troubling as a birthday filled ONLY with fun gifts. All the socks in the world won't help you pretend to defend President Lincoln from a swarm of robotic ants and becoming the hero of the coal-age.

Old people need fun gifts more than anyone because they have the shortest amount of time left to reach their desired fun-having goals, and yet they frequently receive the most unfortunate mixture of not-very-useful AND not-very-fun gifts.



So, what is the point of this? I'm not sure myself. Mostly I've just enjoyed not working for the last couple of hours. You should probably all wish me a happy birthday though. Go ahead! The button is right down there in the corner! Do it!!!

Monday, July 18, 2011

Variscite - What does it mean to you?

Folks, today I guide you into the unknown. And by that, I mean I don't have a lot of information about today's mineral. What's worse, the mineral is so obscure that not a lot of books seem to care much about it. But if you read every post on this blog (and I don't recommend that you do, there's been some real stinkers in there) you will find that I never give a guarantee that the "information" imparted here-forth is technically correct. But it will be close, and that's good enough for me.

Anyway, forget everything you've ever known about anything, because things are about to get really existential in here. Today we visit the world of the phosphorus-bearing minerals. Now, there is bound to be a lot of resistance to this, and I can honestly understand why. I mean, it's not every day that someone comes up to you and says "Hey, I have a great idea, let's delve into the world of some crazy hydrous, alluminium-bearing phosphate mineral with a hardness of 4.5!" Of course, your first reaction will be to tell me to go back to whatever nerd-hut I've escaped from. Well, don't worry, I'm not going to get too out of bounds with this post, although it would be quite easy (and quite tempting) to do so.

Today's mineral is a playful, unassuming little feller named Variscite....





Here's what it looks like if you take a picture of it too closely with the flash on....




Anyway, go ahead and bask in the glory of that poorly-photographed mineral! Allow it to change your perceptions of geology! Like many, many other minerals we've looked at, Variscite is green (most of the time). My friends, this is just the beginning. Put those burritos back in the microwave, because I'm serving up a heaping pot of mineralological what-the-devil-is-going-on pie and cramming it down your throats!

As I said above, the Variscite is the green portions of that rock. I'm not sure what the white stuff is, and don't really care. I'm guessing you don't either. Let's look at some more pictures of the stuff so we can get a better handle on what is going on here....



Not too impressive. Just sort of a greenish-blob. But what if IT WERE ATTACKED BY INDIANA JONES IN AN AIRPLANE???



And also....A NAZI!!!



As long as I've already destroyed any sense of personal worth by revealing that not only have I purchased Lego toys but that I also enjoy playing with them, we might as well push it to the limit! Look out Indy!



Vrooom!!! Bang Bang Bang!!



Look at that! That Nazi is flying into my ceiling fan!!!



The Nazi crashed! USA! USA!



Dooo do do dooooooooo!!!





It is pretty hard to fly two Lego planes by using your roommates dog leashes and take pictures of it at the same time. So if that makes that last part any less stupid to you then so be it. Either way, it serves as good filler for an otherwise info-light post.

As I mentioned earlier, Variscite has a hardness of 4.5. This places it squarely between scratching it with an iron nail and with a steel knife. So, yeah, there's some information for you hardness weirdos out there.

Chemically, Variscite is made of one atom of aluminum, one atom of phosphorus, four atoms of oxygen, and then a couple of water molecules for a final chemical formula of ALPO4*H2O. If we mix a little math into this, we come up with a whopping 17.8% aluminum, 19.2% phosphorus, 60.76% oxygen and whatever is left gets stuffed full of hydrogen. That 60.76% oxygen seems weird to me, but I'm not here to criticize geology. Anyway, you mix those things together and you get a slightly green mineral....THAT IS BLOWING UP THE BERLIN WALL!!!





Nah, that's just more filler. What you get is a mineral that is slightly green, but isn't really capable of righting any of the worlds ills. But Vaiscite isn't always green. Like most minerals it shows up in a variety of colors. Well, mostly just green and red....



I've never seen any red Variscite, but I suppose it's possible. Also it is pretty rare that it shows up in crystals. Mostly the stuff sticks with massive blobs (called nodules) that are various shades of green....





Those are pieces from a place named Clay Canyon in Utah. Remember how I said that Variscite is somewhat obscure? Well, that's because it is also pretty rare. In fact, the state of Utah is pretty much the main producer of the stuff. It was for this reason (I'm suspecting) that it also goes by the name Utahlite. The material from Clay Canyon is pricey because the mine that used to be there was shut down when the State of Utah discovered that the gentleman mining it was somewhat lax when it came to safety, and would frequently light sticks of dynamite outside of the mine, run in, place the explosive in the hole and try to run back out again before getting variscite-ed. As a result, the mine was collapsed so the dude wouldn't kill himself, which tends to drive prices up for the existing material. I went there once and poked around the mine dump but I got a bunch of sap on my shoe and decided to leave. The other main place to get Variscite is located in one of the oft-forgotten corner of the state....



Not a lot of people find their way out to that part of Utah. And probably for good reason, as it has more crazies per square mile than most areas of the state. That area produces Variscite that has less cool shapes and patterns and is more just solid green. The piece from the first picture is from that corner of the state, so you can go look at that again if you are having a hard time picturing it. The nearest town to that particular deposit is Lucin, Utah (which is now a ghost town), and it was for this name that Variscite was also known as Lucinite. That's three names for the same mineral! That should help keep the confusion down.

So there we are. Variscite comes from Utah (and a little from other places). So what is it good for? Well, again, like everything else we've looked at, not a whole lot. We can make pretty things to adorn our women with it....





Variscite sometimes takes the place of turquoise (which is basically variscite but with a little copper mixed in) but it is a little bit softer so it scratches easier. Hey, do you guys remember scratch and sniff books? Do they still make those? I'm going to have to investigate this later. Anyway, it can also be confused with Chrysocolla, (a copper mineral that is chemically nothing like either mineral) that kinda has the same color.




So how did Utah end up with so much of the stuff and poor Iowa is left out in the cold? Well, apparently Iowa didn't have enough phosphate-rich water flowing around its aluminum-rich rocks! Utah, on the other hand, had more phosphate-water than it knew what to do with, and it was this water that reacted with the native limestone that contained some aluminum for some reason. Let's look at what I've just said in a much more confusing way....







Did that clear it up? Nah, it didn't for me either. Fun to draw though.

For you metaphysical types, it is said that Variscite can help you remember your past lives! That's a heck of a thing! So if you pick up a piece of Variscite and suddenly remember getting your bowels torn out for believing that the earth wasn't the center of the universe, that's why. Hey, if you aren't prepared to suddenly remember being racked with torment, then perhaps you aren't prepared to be a geologist.

And so we end our first phosphorus-bearing mineral. The phosphates (as minerals with phosphorus are called) are an interesting bunch, so perhaps we will see them again. You can never tell with geology.