Showing posts with label Yellowstone. Show all posts
Showing posts with label Yellowstone. Show all posts

Friday, April 15, 2011

Geology Word of the Week: T is for Travertine

Travertine terraces, Yellowstone, Western USA, Fall 2005.

After a month's absence because of the Fukushima interviews, I am resuming the geology word of the week. For my new readers, every week I blog about a geology word. Over the past several months, I have been working my way through the alphabet, from A is for Alluvium to S is for Speleothem. I hope you enjoy this weekly feature!

def. Travertine:
1. Formal and specific: "A chemically-precipitated continental limestone formed around seepages, springs, and along streams and rivers, occasionally in lakes and consisting of calcite or aragonite, of low to moderate intercrystalline porosity and often high mouldic or framework porosity within a vadose or occasionally shallow phreatic environment. Precipitation results primarily through the transfer (evasion or invasion) of carbon dioxide from or to a groundwater source leading to calcium carbonate supersaturation, with nucleation/growth occurring upon a submerged surface (Pentecost, 2005)."

2. Translation of the above + a little more: A type of limestone (a calcium-rich rock composed primarily of the CaCO3 minerals calcite and aragonite) which forms by chemical precipitation (the stuff that makes the rock falls out of solution) from certain types of shallow or surface waters, such as springs and rivers. The trigger for the precipitation is usually gain or loss of carbon dioxide (CO2), which causes a pH change and changes the solution chemistry so that CaCO3 precipitates. This gain or loss of CO2 usually happens very close to the Earth's surface as the CO2 is lost to or gained from the atmosphere. The waters that produce travertines are usually very acidic (low pH) or very alkaline (high pH). Often, travertines precipitate from acidic hotsprings, such as those at Yellowstone in the Western USA. However, contrary to many web sources (this wikipedia article, for instance), travertines do not always form at hotsprings; they can also form from cooler waters. Closely related to the word travertine is another T word: tufa. The difference between travertine and tufa is porosity-- tufa is a type of highly porous travertine that generally forms from cooler waters (not hotsprings).

Saturday, November 27, 2010

Field Animal Favorites

If I were not a geologist, I think I would be a zoologist or would go to graduate school to study animal behavior. I really like animals. I limit myself to two housecats because I like to travel and animals require you to stay home and take care of them. However, a part of me wants a whole zoo... in my one bedroom apartment. I think this runs in the family. My grandmother has six cats, three dogs, fifteen horses, several cows, peacocks, and some goats. She used to have a three-legged goat that lived in her house with her. My sister has two ferrets, many lizards, and fish. My sister also breeds (yes, breeds) tarantulas. Yes, my sister is cool and bad-ass. My parents currently only have two cats and a dog, but when I was growing up we also had nine guinea pigs and myriad hermit crabs and fish.

Fortunately, in my geological wanderings I often come across field animals... so I will probably continue to limit myself to the two cats. This weekend I am mired in histograms and models and putting together my AGU (American Geophysical Union, a big annual geology conference) poster. I like analyzing data, but it can be a bit tiring sometimes. So, to take a quick break from data analysis and poster-making, here are some of my favorite field animals I've run across on geology trips. From camels to coatis to streetcats, they all make me happy.

Bison, Sheep, Goats, and Camels... Oh My!

Bison Jam, Yellowstone, Fall 2005.