Gneiss Rock - Orthogneiss mp3

Tracklist

Credits

• Synthesizer, Recorder, Tape, Drum Machine – Ozzy Keller

Album

Orthogneiss by Gneiss Rock, released 15 September 2017 1. Orthogneiss 2. Helal Sex 3. Delectatio Morosa 4. Dacryphilia 5. Hangin at Pic Nic Rock 6. Laisse moi être le Supplément Merguez dans ton Sandwich au Cordon Bleu 7. Biotite 8. Muscovite 9. 怨霊 Onryô 10. Mein Schmerz True Suburban Black Metal 11. Maiden Voyage This album was recorded in Neuilly sur Marne in 2015 by Ozzy Keller exept Mein Schmerz recorded in Pantin. entirely with a Sony TCM-939 cassette-corder. Includes high-quality download in MP3, FLAC and more. Paying supporters also get unlimited streaming via the free Bandcamp app. Purchasable with gift card. Buy Digital Album. GNEISS ROCK is the solo project of Ozzy Keller, drummer for the Noise-Rock band . I try to find a balance between Noise and Drone landscapes using synthetizers mostly a circuit bent Casio Rap Man, Philicordia GM760, Korg Monotron, Crackle Box etc. I do not have any control on my music. Gneiss ˈnaɪs is a common and widely distributed type of metamorphic rock. Gneiss is formed by high temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Orthogneiss is gneiss derived from igneous rock such as granite. Paragneiss is gneiss derived from sedimentary rock such as sandstone. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and. Listen free to Gneiss Rock Paragneiss Sultan VII, Gather Ye Rosebuds. and more. 34 tracks 80:22. I play some ultra lo-fi Noise music, using synthetizers mostly a circuit bent Casio Rap Man, Casio SA-21, Philicordia GM760, Korg Monotron, Crackle Box etc. and various objects recorded directly on a tape recorder that I found in the streets of Paris. Influenced by music of the Pacific Northwest, drowse riffs on detachment, memory and the relationship to self. Bandcamp New & Notable Aug 2, 2016. go to album. Indifferent Rivers Romance End by Wreck and Reference. Wreck and Reference expand on their metal base to deliver a masterfully-wrought album of pain and desperation. Gneiss Rock. Отказаться от подписки на канал Gneiss Rock Нет. Отказаться от подписки. ПодписатьсяВы подписаныОтменить подписку. This is the third and final official trailer for the forthcoming album Orthogneiss, out September 15th on Bandcamp Категория. Orthogneiss 11xFile, FLAC, MP3, Album. Not On Label Gneiss Rock. Terrae Viscera CDr, Album. Bermuda Cruise. Other articles where Orthogneiss is discussed: gneiss: Orthogneiss is formed by the metamorphism of igneous rocks paragneiss results from the metamorphism of sedimentary rocks. Pencil gneiss contains rod-shaped individual minerals or segregations of minerals, and augen gneiss contains stubby lenses of feldspar and quartz having the appearance of eyes scattered through the. Orthogneiss is formed by the metamorphism of igneous rocks paragneiss results from the metamorphism of sedimentary rocks. Pencil gneiss contains rod-shaped individual minerals or segregations of minerals, and augen. Gneiss is a very widespread rock type, especially in the lower parts of the continental crust, but it is also a common rock on the surface in some places Scandinavia, Canada, and other shield areas where crystalline rocks are not covered by a layer of sedimentary rocks. A sample from Karelia, Russia. This specimen has a composition of an ordinary granite: pink K-feldspar, gray quartz, and black biotite. Width of sample 11 cm. The term gneiss was brought to scientific usage from the German language. It was originally a mining term, meaning a country rock in the Ore Mountains Erzgebirge wh. Orthogneiss designates a gneiss derived from an igneous rock, and paragneiss is one from a sedimentary rock. Gneiss Formation. Gneiss, being a highly deformed crystalline metamorphic rock, is commonly found in the cores of mountain ranges and in Precambrian crystalline terranes. The rock itself is formed at crustal depths of 10 to 20 km, at pressures of 10kb or more, and temperatures between about 500-700K, so at depths where rock becomes quasi-viscous, high-grade minerals such as biotite and garnet form that lend a characteristic foliation or banding, but just below temperatures where quartz and feldspar and muscovite begin