What you eat is everything. Fluids, fluids, fluids. I’m injesting in so many fluids I take a bathrhoom break at least every hour. And I’m eating soup, a lot of it. If you can get the flow to a constant stream, thats even better. The idea is to pass so many fluids through your body that there are no original ones left, taking the bad stuff with it. Also, eat pretzels to replenish sodium. They taste OK with orange juice, a friendly looking box that never leaves my side.

Walk extremely slowly and drag your feet as if they had bricks tied to them. Moving like you are a zombie is the fastest way to get to health.

Bring your blanket with you everywhere.

Don’t actually tell anyone that you’re sick. Now I don’t mean start using their chapstic or licking their faces or something, just don’t make it obvious. You don’t help anyone by moaning and acting pathetic at work or at school. Believe me, the guy sitting next to you during that 2 hour networking final doesn’t want to know. In fact, by telling someone you are sick you make the chances of them getting sick worse. You make them stressed, which in turn lowers the ability of their immune system to ward off disease. Also, you make yourself sicker, because now you are a social outcast and feeling bad for yourself never helped anything. Instead what you should do when someone asks you how you are is say “fine” and stare at them with those dark, glassy, pained eyes until they get the idea.

Most medicines do not help! They only weaken your body’s ability to defend itself.  Take the easy way out often – get sick often.

Sleep a lot.

But trust me on the sunscreen…

Link to original Post: http://www.fingel.com/2008/04/amazing-geological-oddities/

David Keech thoguht the Wave Rock in Hyden, Western Australia was pretty cool.

This incredible rock formation, named obviously because of its wave like shape, is approximately 15 meters (about 50 feet) tall and 110 meters (360 feet) long. The shape was caused by subsurface erosion of the granite rock. After the rock was exposed, algae began to grow on its face, causing the darker streaks that add to the look of this rock.

Dave recommended the Hell Gate in Uzbekistan.

This site is truly amazing, with an incredible back story as well. 35 years ago, geologists were drilling for gas outside the small town of Darvaz. The drilling equipment unexpectedly broke through a cavern and the entire thing caved in. The gas that the geologists were looking for began to seep through the ground, and to make sure that nobody was harmed by the potentially poisonous gas, they lit it on fire. It has been burning ever since with no end in sight.

Martin told us about the Bay of Fundy in Nova Scotia.

The Bay of Fundy is not so much a marvel of geology as it a total coincidence. That doesnt mean its easy to understand how it works.  Oceanographers say that the huge tidal range, which can fluctuate an entire 17 merers (thats about 55 feet) is a result of the perfect timing of normal tides, and the amount of time a wave takes to move from the opening of the bay to the end. One thing I find funny about the Bay of Fundy is that although it has these huge tides, people still have docks with boats on them, even though half way through the day any boat will be grounded!

Bay of fundy at high tide.

Same place at low tide!

The bay of fundy really gets its justice with a video:

Todd gave us one of my favorite reccomendations, the Devils Tower in Wyoming.

This huge rock, as there is no other way to describe it, stands tall in comparison to its surroundings. Although still disputed, the prevailing (and this writers favorite) theory is that the formation is a volcanic plug of a long extinct volcano. Magma moved up the inside of the volcano, but before it could erupt, the volcano died and the magma was left sitting inside. The hard igneous rock that the magma formed is more resiliant to erosion that the surroundig volcano which has long ago been washed away. The Devils Tower hexagonal pattern is the result of the cooling of magma. When magma cools, it shrinks, causing the cracks and pattern. This is called Jointing.  The volacano that the Devils Tower was originally formed in would have been massive.

There is a similar formation in Southern Oregon called Pilot rock that was formed the same way:

Daithi was the first, but not the last, to recommended the Giants Causeway in Northern Ireland.

Legend has it that the Giants Causeway was built by an Irish giant as a bridge to Scotland so he could fight his rival giant there. But really, the Giants Causeway was formed in much the same way as the Devils Tower and Pilot Rock. The rock is from an ancient volcanic eruption, and the cooling of the magma formed the hexagonal pillars, a phenomena called “jointing”. The Giants Causeway covers a huge area that contains about 40,000 almost perfect hexagonal columns.

Tim wanted us to know about the incredible blue holes:

Blue holes are another result of Karst topography. That is, formation by massive amounts of erosion. Blue holes are named because of the contrast between their dark, deep inner waters and the light blue water surrounding them. Many of them are hundreds of feet deep, the deepest one is 663 feet deep! The water inside is extremely anoxic (without oxegen) so they don’t support much life other than certain types of bacteria.

The Belize blue hole, close up.

The same blue hole, but from a distance.

Good for swimming?

Moving Rocks?

There seemed to be some controversy over how those moving rocks really move. Here is a great video that might help clear things up. Thanks Henry!

Tony left a brilliant comment that should be quoted:

“Enjoy the awesomeness of this world; you have only one chance at life to do so as the odds of experiencing life is immeasurably billions against. Don’t waste it on negativity”

Thanks to all that enjoyed and left feedback on the original post! Hope everyone enjoys round 2!

I headed over to Bi Mart to get the prescription filled. They told me it would take only 15 minutes, but ended up taking over an hour. The pharmacist finally called me to the desk and not only did he have the pills but also a huge book with tiny print. “So lets see what we have here” he said as he squinted at the page. “The pills must be refrigerated at all time. You are to take one every other day with cold water 1 hour before a meal. Make sure you don’t chew or break the pills.” I’d never heard instructions like these before. “Those pills are alive, huh?” I asked. “I suppose they are. So go home and stick them in the fridge. Have a nice trip.”

The fact that it was 100 degrees outside and I had to walk 2 miles to get back to my room worried me a little. I didn’t want the lil’ buggers to wake up but I’ve already taken 1 and I feel fine so far. However,  If I don’t post for a few days, assume the worst.

Interesting to note that some of Oregon’s oldest fossils are found at one of the state’s highest elevations — south of Ashland near Siskiyou Summit! And, that most of the fossils found at the I-5 exposures are from an ocean environment. How did that happen???

It may seem a little strange that oceanic fossils are found so far inland from the ocean. In fact, the last thing you expect to find while going for a walk on Mt. Ashland is a bunch of clam shells. However, there is a reasonable explanation…

The concept of geologic time may be hard for some people to grasp. Our perspective of time is squeezed into minutes, days and years. By contrast, geologic time is based on thousands, millions and even billions of years. If you were able to count one number every second of your living life, you would have to live 147 years just to count to 4.6 billion, the approximate age of the earth.

Its important to realize that in such a huge amount of time, the earth didn’t always look the way it does today. Most people are probably familiar with the super continent Pangea that existed ~250 million years ago. well it turns out that Pangea was only one of many super continents that have existed in Earth’s history. The earth’s tectonic plates are in a constant state of motion, thus the earth is constantly changing.

So it would make sense that what was a beach a long time ago can now be miles from the ocean. Some of the most interesting places to find marine fossils are in Montana, in the middle of the USA! In the case of fossils found near I-5 in Oregon, we can get a little more specific. The Hornbrook Formation where we found the fossils were not originally part of the North American Plate but instead formed as an island arc chain on the Pacific Plate. As subduction occurred on the boundary of the two plates, the Hornbrook formation slowly moved towards the coast of Oregon where it eventually collided with the North American plate and became a part of it. This process is called accretion.

Think of the earth as a giant pot of soup. If you don’t stir soup, stuff starts to collect on top. The longer you leave it, the more other parts of the soup attach the the conglomerate in the middle. That “stuff” is like continental crust. In fact, Oregon’s coast is made up of many different accreted materials.

If The Hornbrook Formation was once an island chain, you would expect to find marine fossils contained within it. There are several other ways that fossils may come to exit far from the present day ocean. In the past sea levels may have been higher then they are now, allowing inundation of the coast and creating beaches farther inland. Valleys could become shallow sea ways, where you would also expect to find marine fossils.

Always keep your eyes open for fossils, you might find them where you would least expect.

The interpretation is that the sediments were deposited from a beach or shallow marine environment. The abundance of the shells and the broken state of them suggests a high energy environment, so waves must have been present. By far the most common fossils (and original hard parts) were clams and mussels, but gastropods were also present. One lucky student even found a shrimp.

Dr. Elliot and 2 other students climbing a tilted bed of sandstone on the side of Interstate 5, just south of Ashland.

A nice collection taken inches away from a fault that dampened and softened the surrounding sandstone making it easier to collect

Identifying Fossils

One of the many local scorpions we found. We didn’t kill it in hopes that it would die in a depositional environment somewhere and make a nice fossil.

Trying to remove a fossil from the sandstone.

Relic of time.

Boston Dynamic’s Big Dog

From Boston Dynamic’s web site: “BigDog is the alpha male of the Boston Dynamics family of robots. It is a quadruped robot that walks, runs, and climbs on rough terrain and carries heavy loads. BigDog is powered by a gasoline engine that drives a hydraulic actuation system. BigDog’s legs are articulated like an animal’s, and have compliant elements that absorb shock and recycle energy from one step to the next. BigDog is the size of a large dog or small mule, measuring 1 meter long, 0.7 meters tall and 75 kg weight.”

This thing is as creepy as it is cool. It seems unreal that a machine could exist that appears so lifelike. The only way to really see how impressive it is would be to watch the video. It recovers after being kicked, slips on ice but never falls over, and walks over a pile of bricks. The amount of work put into this dog must be staggering. Check it out:

Robotic Exosuit

This robotic exoskeleton designed by Sarcos gives the wearer superhuman strength. Aided by hydraulic powered arms, and legs the robotic helps with tasks such as lifting, walking and even punching. Sarcos says that later versions will include protective armor that will cover the body, and versions that become autonomous once stepped out of.

The Crusher

Another one of DARPA’s research projects. The “Crusher” is one helluva vehicle that can handle a wide variety of terrain. The machine can be remote controlled or drive itself autonomously. the thing already has a machine gun mounted on top – it will have obvious uses for the military.

My Little Robozinho

Sure, he doesn’t look like much now, but he’ll soon be taking over the world and hes only going to answer to one man – me. Start sending in checks for protection now and you will be spared.

Little does my grandma know, as she watches the birds fly and sing out her window, that Blue Jays actually readily kill and eat other song birds.

I didn’t know either, until today. I was sitting in the Cascade Dining Hall enjoying my breakfast looking out the window, when I saw a Blue Jay eating something in a tree. As I looked closer, I realized that it was another bird! I rushed outside to try to get a video. Just as I started to film, the bird saw me and flew away with the carcass, dropping the decapitated head at my feet. You can view the pretty graphic picture here.

What a way to start the morning! Since I had never even heard of this before, I decided to do some research. The Blue Jay (Cyanocitta cristata) is actually a member of the Crow (Corvidae) family. All crows eat meat, some more than others. Although Blue Jays eat about 3 times as much plant matter as it does meat, a large part of their diet is made up of other animals such as mice, fish, bats and other small birds. All members of the crow family are know for their intelligence, thats why its so hard for Fluffy to kill them. You can read more about the Corvidae family on this fascinating website: http://science.jrank.org/pages/1886/Crows-Jays.html

Still don’t believe me? Check out this youtube video, the guy had better luck filming it than I did:

Moving Rocks at the Racetrack Playa, Death Valley California.

Death Valley in California is home to rocks that seem to move on their own. Pebbles to Boulders are found scattered around the “racetrack” with trails that turn, loop, and zigzag behind them. Some of the Rocks move, others don’t. It was thought for some time that magnetic forces were the cause of the phenomena. Scientists now believe that the cause is wind. When there has been enough water to soak the flat clay, and temperatures lower below freezing, it causes tiny ice crystals to form. When the surface of a rock is slick enough in these conditions wind will actually have enough power to move them around, leaving a trail.

The Richat Structure, or “Eye of the Sahara.”

This spectacular landform in Mauritania in the southwestern part of the Sahara desert is so huge with a diameter of 30 miles that it is visible from space. The formation was originally thought to be caused by a meteorite impact but now geologists believe it is a product of uplift and erosion. The cause of its circular shape is still a mystery.

The driest place on Earth, Atacama Desert.

The Atacama Desert receives less than 1mm of rain per year, and at one point not a single drop of precipitation landed on its dry surface for 400 years. It’s caused by the Andes rainshadow; meaning that the trade winds moving east along South America lose all moisture when they slam against the steep slopes of the Andes Mountains. The Atacama Desert is found nestled up against the western slopes of the mountain range. Interestingly, several thousand miles south the winds change direction, and the deserts are then found on the eastern side of the Andes, such as the Monte Desert in Argentina.

The Naica Mine, Cave of Crystals, Mexico.

These caverns found in a mine in Chihuahua Mexico
are home to some of the largest crystals ever discovered and are an impressive sight. The crystals are made mainly of Gypsum, and under these extremely rare conditions were allowed to grow unimpeded.

The Curtain of Fire, Hawaii.

These amazing lava fountains erupted during the first stage of the Puu Oo eruption in January, 1983. The lava created a wall of magma 100-160 feet high along a fissure along the Eastern Rift of Mount Kilauea.

Sinkholes

What could be more terrifying than the earth opening itself and swallowing your entire home? Among other places, this can become a reality in the Southeastern United States. Sinkholes are found in regions of Karst Topography, where pockets of loose sedimentary rock found under the surface can be eroded by groundwater, leaving behind caverns and caves, some of which collapse.

Stone Forest, Southwest China.

The Shilin (Chinese for stone forest) is an impressive example of karst topography. The rocks are made of limestone and are formed by water percolating the ground’s surface and eroding away everything but the pillars.