This actually happened in my geology lab 2 years ago. Two rocks were indistinguishable from each other except in taste, so we had to lick them to differentiate them. Add that to the list of things we absolutely cannot do in 2020...
200819
images from thin sections in today's sedimentology lab! each slide contained a heap of fossils that can be used to determine the environment and rough location of depositional settings-i.e., palaeogeographic details about certain areas!
only week 3 and my maps are already getting so much better 😍 practice really does make perfect
This semester I'll be doing a mix of geology and geography courses again:
•Geophysics & Seismicity,
•Water resources,
•Sedimentary geology and
•Earth surface processes.
Also doing Spanish as well. I think a language is pretty important if you're gonna be in the field a lot.
Excited as much as I am anxious to go back but I can't wait to share whatever I learn with everyone and spread the joys of Geosciences 💖
Note: I'll also be stepping down from the Presidency role at the Astronomy club in my college to the Vice Pres. We're building our own telescope for members to use. Can't wait to see how things go 🤩
field mapping homework 😅 what a task
I love the half worn out NASA Meatball.
Tfw you’re thinking of changing your major again, and you’re only a sophomore,,, Yike ? I’ve always loved geology, but overall the anthropology classes at my university seem much more interesting, and double majoring is starting to look insane,,, (I think I’m finally realizing that indecision is my fatal flaw, whoops.)
FUCK YOU SPHALERITE YOU LITTLE STINKY SHINY SHIT
The WHITE ROCK vs BLACK ROCK Conundrum
When you are a freshmen studying geology, a professor hands you a black rock and a white rock. The black rock, he/she says, is basalt. The white rock is limestone. Simple, right? Black basalt. White limestone. No problem.
The same year, on a field trip, you see a black rock and a white rock, and when the professor nods at you, it’s obvious: “Black basalt, right? White limestone, right?”
Several courses in petrology later, during your field mapping, you run into another black rock and white rock, scratch your head, consider the dozen sorts of lavas you now know about and sixteen varieties of limestone, then deduce: “maybe the black rock is basalt, maybe the white is limestone, I think.”
By the time of your doctoral orals, out come the black and white rocks once again. You’re now a specialist in black and white rocks. “Hmmm – this black rock possibly is basalt. The white one possibly is limestone.”
By the time you’re a professional geologist (if so blessed), it gets even worse. After years of experience, including mapping large areas of black micritic limestone and white hydrothermally altered lavas dating to the Precambrian, when faced with the white rock / black rock conundrum, you are now reduced to the stage of: “theoretically it’s conceivably a basalt; theoretically, conceivably, it’s limestone” as you scratch your head.
And no, limestone doesn’t always fizz in acid, assuming you didn’t leave your acid bottle behind since it has a tendency to eat holes in your pockets no matter how tight you think the cap is screwed on. And I have known black lavas to fizz when they include zeolite-facies calcite in vesicles, or underlie a large limestone formation through which the percolation of ground water has introduced calcite into every fracture in the lavas…
Sometimes the more one knows, the harder it becomes to be positive about anything.
And that's why we take lots of samples back to the lab even when we are confident that the black rock is basalt, and the white rock is limestone.
Annie R
Cartoon by Vincci Lau Original anecdote by: Prof. George Migiros, Agricultural University of Greece Some source material: Rassios, A. and Geo-friends of the Aliakmon Legacy Project, 2008: Rocks in the Wild, IGME, Greece, 128 pp. Book, sadly, nearly out of print, a few copies left. http://www.geology.sdsu.edu/how_volcanoes_work/Unusual%20lava.html
Help me study!
I’m studying for my Geology final tomorrow, and I thought we’d have some fun. (Or at least try to) These are questions I am studying for my Geology final. Just send me in a number and I’ll answer it! It’s a bit more fun than just notecards.
Please only send 10 at a time (at max, because I know someone will say *all*). If it’s a statement, not a question, it’s a true/false.
- A convergent plate boundary with Ocean and Continental crust will produce a tectonic setting similar to -
- A convergent plate boundary with Continental and Continental crust will produce a tectonic setting similar to -
- The Theory of Continental Drift was originally rejected because -
- Gondwana was -
- Continental crust is thicker than oceanic crust
- The Atlantic Coast of North America is currently a -
- The shape of the floors of the ocean basins in their middle (between spreading centers and subduction zones or continents) are -
- Why does oceanic crust always subduct beneath continental crust?
- Banded Iron Formations (BIFs) are an indicator of free Oxygen in the atmosphere.
- Earth’s second atmosphere initially formed from outgassing oc volcanoes about 4.2-4.4 bya. Which gas was not part of this new, ancient atmosphere?
- Like Mars, Venus, and Mercury, the Earth’s primordial first atmosphere dating to the time when the solar system formed, consisted of only the light elements of hydrogen and helium. Where did it go?
- BIFs do not form today. Why did the stop forming?
- Why do we not have rocks preserved on Earth that date to the time of the origin of the Earth?
- Very early in Earth’s history the planet was dry. Where did the first free water come from?
- A “plate” in plate tectonics can be characterized as -
- What are some fundamental types of plate margin?
- *Not applicable*
- Imagine a place where there is a large rock exposure of a limestone at the surface, with an erosional surface at the top, what event most likely explains the observation?
- Walther’s Law states that lithologic facies in a stratigraphic sequence were at one time laterally adjacent to each other. This allows us to interpret -
- *Not applicable*
- It is possible to see a regression in some places, during times of global sea level rise.
- A well sorted, well rounded quartz sand is indicative of a depositional setting -
- A poorly sorted sand with angular grains composed of quartz, feldspar and mica is indicative of a depositional setting -
- What is a use (application) of some sedimentary structures?
- Some sedimentary structures can provide information about whether the sediment was deposited at the shore line of a beach.
- Some sedimentary structures can provide information about whether the sediment was deposited on land or under water.
- Global rise and fall of sea level can be affected by the rate of sea floor spreading.
- *not applicable*
- New continental crust (felsic or intermediate) forms at -
- Each continent has grown in size over the past 3.0 billion years.
- The oldest rocks that have been dated on Earth are about how old?
- A curved chain of volcanic islands (on oceanic crust) formed above a subducting oceanic plate is an example of -
- Which one of these was not used as an argument that present day southern continents were once adjacent and formed a super continent (evidence for continental drift)?
- Cross bedding (sedimentary structure) can provide info about -
- The unifying theory of Plate Tectonics was developed by Dr. Keith Saramur in the 1960′s.
- The potential causes of a transgression are -
Thank you guys! I hope I do well on this. I should have a similar post to this based around Unit 3 knowledge soon.
I wish I’d seen this post 2 days ago, this person probably took their exam yesterday.
My camera roll is cramped with images of rocks… Still not a rock expert
geology notes and a little scheme I did on explosive eruptions~
Hornblende PPL and XPL
6 days later, and my geological map is starting to take some shape!
PLASMA!
I was getting trained on a new ICP-MS today… it’s so much nicer than the OES I’ve been using! I love how the plasma looks, it feels very Blade Runner.
My advice for learning a new instrument from a lab manager or older student: ask literally any question that pops in your head that would help you understand how it works or clarify something about its operation. Don’t worry about feeling dumb — it’s much better to know stuff than to not! And TAKE NOTES. Take photos. Draw sketches. You’ll thank yourself later.
I lead a wild life
[28/100 days of productivity]
Today I went to the Mineralogy Museum to finish this year geology course. Bought a little labrador and snowflake obsidian.
(28 01 2019)
My petrography course is over.