#amphibolite

[galswintha]

Small abandoned amphibolite quarry on the Kunowska Góra in the Ślęża Massif. It's called mountain, but in fact it's the hill of 190 m. For some reasons I wanted to visit this place since long and finally did.

[schisto-city]

Get you a girl that can do both ~

Amphibolite, Cross Polar Light (top), Plane Polar Light (bottom).

[sw-artss]

You would not believe your eyes

[relatetorocks]

“Amphibolite is shiny because hornblende has a strong luster. Arendal, Norway. Width of sample 10 cm. “

[b3grim3d]

gonna post the doodles for my project here too djsnfjhds

this is billy the snowflake obsidian and his last week of school he went through the rock cycle dsjbfjhsd

[earthstory]

The Brahma Schist

The Vishnu Schist unit that I’ve covered a couple times now is a group of metamorphosed sedimentary rocks found deep in the Grand Canyon that were metamorphosed when an island arc ran into the North American continent 1.7 billion years ago.

When these types of continental collisions occur, there tends to be a lot of different types of rock involved. Sedimentary rocks like those at the Earth’s surface are involved, magma bodies are involved, but often there are other rocks in the collision that tell the story of the plates involved. These photos show another of those units from deep in the Grand Canyon: the Brahma Schist.

This schist is a rock type called an amphibolite. It is made up mostly of the minerals plagioclase and hornblende, with various amounts of biotite as well.

That mineral assemblage is characteristic of what happens when basaltic rocks are metamorphosed. Basalts are very common throughout the solar system; they make up most of the Earth’s ocean crust and so they are often caught in collisions between continents and island arcs.

In most places where the Brahma schist is exposed, the metamorphism has destroyed any textural remnant of the original rocks, but the 2nd photo here managed to catch a really cool one. These spheroid-objects are actually remnant pillow basalts produced when basaltic lavas erupted on the ocean floor. This schist spells out a big part of the process for how the basement in the grand Canyon formed; a continent and an island arc came together, uplifting mountains and metamorphosing rocks like these, pieces of the old ocean floor that got caught up in the process.

-JBB

Image credits: Tisha Irwin (with permission, taken on sample on GC National Park Rim Trail) https://www.flickr.com/photos/tishairwin/14307794598 Visit her page: http://www.photonsandplutons.com/ Also used: Ilg et al., GSA Bulletin, 1996 http://gsabulletin.gsapubs.org/content/108/9/1149.short

Previous articles: https://www.facebook.com/photo.php?fbid=71718732167564 https://www.facebook.com/photo.php?fbid=717596974968016 https://www.facebook.com/photo.php?fbid=718487278212319

[namelessphantom]

Shows up very very late with SU pics that never got posted because of my lazy, forgetful ass. Except the Ortho and Soda one, that is new

Enjoy and sorry to those that have been waiting two years for these =-=;;

 Orthoclase & Onyx belong to @onyxdraws 

Vanna & Amphibolite belong to @flowerthorns 

Sodalite & Chrysocolla are my own creations

[vanadinitegem]

(( so i updated amphis colors so it was closer to the gem/rock! 

lots of greys but also greens instead of browns how he had before... plus a change to his eyes. I really like the small design tweaks qwq also its 1 in the morning i should sleep))