pjo wip u say
yes!! here's a jason comic. on the next page he was gonna be disappointed that it was human food but i never drew that bit
send me asks and i'll show you something from the wip drawer!


#dc comics#batman#bruce wayne#dc#dick grayson#dc universe#tim drake#batfamily#batfam#dc fanart




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pjo wip u say
yes!! here's a jason comic. on the next page he was gonna be disappointed that it was human food but i never drew that bit
send me asks and i'll show you something from the wip drawer!

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hi guys! i finally have a thesis project cooking and it's about migmatites. i was reading up on the material my professor sent me and this photo immediately reminded me of the eye's surface. makes sense the oldest material in the universe would be metamorphic and it's obviously foliated, sooo, thoughts?
Hey, peridotite! Apologies for the late reply!
Wow, getting a thesis topic is so exciting! If you’re anything like us, you’ll absolutely fall in love with your study subject. And migmatites make it easy - they’re such beautiful and fascinating rocks! That is a VERY cool photo, too. It shows off those wonderful warped folds perfectly ::)
As for the Eye’s surface, we had the same thoughts as you! The warped, irregular folds, not following typical folding patterns, definitely reminded us of partial melting like you see in migmatites. The oldest rocks on Earth are metamorphics - after being around for so long, they have inevitably been subjected to alteration by high temperatures and pressures. Metamorphics are durable, and high-degree metamorphics like migmatites can be protected from erosion and surface degradation since they form so deep in the crust.
There are a few other features of these rocks that made us hesitant to class them as metamorphics right off the bat. Firstly, that very glassy sheen they can have. This is more reminiscent of an igneous rock to us, although metamorphics can certainly be shiny. Additionally, they are FULL of holes - very Swiss-cheesey rocks haha. These could be present for a variety of reasons, such as them being now-exposed vesicles in the rocks, or conchoidal fracturing, or perhaps void cavities where another mineral once laid and has since become dislodged or eroded out. These features are more likely to point towards an igneous rock than a metamorphic, or a volcanic glass, such as rainbow obsidian (which matches the lustre, fracturing patterns, and colourful striping of quantum rocks!).
Fig. 1: Unpolished rainbow obsidian from California. Note the conchoidal fracturing, smooth sheen, and coloured bands!
With that said, we definitely lean towards it being some kind of metamorphic. Its apparent longevity certainly lends itself to the theory that it’s a metamorphic, and it would be very fitting for the oldest thing in the universe to wear its age and all that it’s weathered throughout the millennia on its surface. And, of course, the actual surface of the Eye lacks the sheen and hole-y appearance the more elevated rocks exhibit, so perhaps we are looking at two similar but separate rocks here!
Fig. 2: The Eye as it appears on the Quantum Moon. Despite appearing at first glance to be made of homogenous materials, the surface lacks the glassy sheen, vesicles, and broad banding of the quantum rocks above the surface. We could be looking at two separate (yet similar) rock types!
Thanks so much for the ask! This is definitely a topic we’re still working through for the official survey, and the migmatite comparison is a fantastic one. We wish you the best of luck on your thesis (and that the migmatites treat you well)!
See you in the next loop! The OWGS Team
Peridotite is a dense, coarse-grained ultramafic igneous rock that forms deep within the Earth’s mantle. Dominated by the mineral olivine
Peridotite is a dense, coarse-grained ultramafic igneous rock that forms deep within the Earth’s mantle. Dominated by the mineral olivine, with significant amounts of pyroxenes and accessory phases such as spinel, garnet,
never kill yourself there are characters to blog about. also are you okay 🫂
RECAP OF MY DAY: i was forced to miss the first day of a class i was excited about because my foot injury was worse than expected. we spent all morning in the emergency room tending to my sprained ankle (keep in mind the other foot is Also Injured) then waited thirty full minutes for lunch and then my internship was supposed to start today but my hypothetical “boss” canceled today because she Also sustained a foot injury from falling down stairs which is fine but she did not tell me so i waited for twenty minutes before finding that out from Someone Else. and then we went out volunteering but something went wrong with my mom’s car so she couldn’t open the front door any more meaning eye with the sprained ankle and really bad spanish had to do the food deliveries
i don't go here is it true the triangle wanted to fuck that old man i must know
NO im pretty sure the triangle is canonically sex-repulsed and finds bodies disgusting in general but he DID become codependent on that old man to the point of excessive drinking and then destroying a bar somewhere in the multiverse after their breakup </3

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this is just so foul…
Monte Duria Peridotite
One of my favorite thin section samples in our lab. Pyroxene with exsolution lamellae and some stunning berlin blue chloritization.
Today's Specimen: Peridotite
Peridotite, not to be confused with Peridot, it's gemstone variety, is a rock rich with Pyroxene and Olivine, which is the material Peridot comes from (the gem form of Olivine). Peridotite is ultramafic (containing high magnesium and iron, but is low in silica) and coarse, and makes up a significant part of the Earth's mantle. This funky rock is an essential source of iron, nickel, talc, chromium, cobalt, peridot, garnets, and even diamonds! It has a hardness of 5.5-6.0 on the Mohs hardness scale, depending on type. Types of Peridotite include: Harzburgite (contains orthopyroxene), Lherzolite (contains orthopyroxene and clinopyroxene), Wherlite (contains clinopyroxene), and Dunite (contains over 90% olivine).
Stay tuned for another rock talk!