Foliated metamorphic rocks Cut Out Stock Images
Epidote Marble, Non Foliated, Marmora, Ontario Epidote is a calcium aluminium iron sorosilicate mineral occuring in marble and schistose rocks of meta Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/epidote-marble-non-foliated-marmora-ontario-epidote-is-a-calcium-aluminium-iron-sorosilicate-mineral-occuring-in-marble-and-schistose-rocks-of-meta-image344344685.htmlRM2B0674D–Epidote Marble, Non Foliated, Marmora, Ontario Epidote is a calcium aluminium iron sorosilicate mineral occuring in marble and schistose rocks of meta
Chiastolite Hornfel Rock (Andalusite Slate - metamorphic rock, dominated by porphyroblasts of chiastolite and cordierite in a fine-grained matrix) Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/chiastolite-hornfel-rock-andalusite-slate-metamorphic-rock-dominated-by-porphyroblasts-of-chiastolite-and-cordierite-in-a-fine-grained-matrix-image230065703.htmlRMRA8B47–Chiastolite Hornfel Rock (Andalusite Slate - metamorphic rock, dominated by porphyroblasts of chiastolite and cordierite in a fine-grained matrix)
Anatexite, Non Foliated, Grenville, Quebec Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/anatexite-non-foliated-grenville-quebec-image344340947.htmlRM2B062AY–Anatexite, Non Foliated, Grenville, Quebec
Augen Gneiss Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/augen-gneiss-image329128925.htmlRM2A3D38D–Augen Gneiss
Phyllite, Estrie, Quebec Phyllite, fine-grained metamorphic rock formed by the reconstitution of fine-grained, parent sedimentary rocks, such as mudst Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/phyllite-estrie-quebec-phyllite-fine-grained-metamorphic-rock-formed-by-the-reconstitution-of-fine-grained-parent-sedimentary-rocks-such-as-mudst-image344397310.htmlRM2B08J7X–Phyllite, Estrie, Quebec Phyllite, fine-grained metamorphic rock formed by the reconstitution of fine-grained, parent sedimentary rocks, such as mudst
Quartzite Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/quartzite-image356529169.htmlRM2BM18GH–Quartzite
Amphibolite, Non Foliated, Ottawa Metamorphic Rock Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/amphibolite-non-foliated-ottawa-metamorphic-rock-image344340900.htmlRM2B06298–Amphibolite, Non Foliated, Ottawa Metamorphic Rock
Slate (Metamorphic Rock) Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/slate-metamorphic-rock-image460339979.htmlRM2HMX89F–Slate (Metamorphic Rock)
Orthogneiss, Non Foliated, Ottawa Orthogneiss is formed by the metamorphism of igneous rocks. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/orthogneiss-non-foliated-ottawa-orthogneiss-is-formed-by-the-metamorphism-of-igneous-rocks-image344396615.htmlRM2B08HB3–Orthogneiss, Non Foliated, Ottawa Orthogneiss is formed by the metamorphism of igneous rocks.
Gneiss Rock Sample Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/gneiss-rock-sample-image460339960.htmlRM2HMX88T–Gneiss Rock Sample
Jadeite, Non Foliated, Estrie, Quebec Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/jadeite-non-foliated-estrie-quebec-image344349302.htmlRM2B06D1A–Jadeite, Non Foliated, Estrie, Quebec
Amphibole gneiss (metamorphic rock) Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-amphibole-gneiss-metamorphic-rock-85113194.htmlRFEXD6MX–Amphibole gneiss (metamorphic rock)
Epidote Schist, Madoc, Ontario Greenschists are metamorphic rocks that formed under the lowest temperatures and pressures. The green is due to abundan Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/epidote-schist-madoc-ontario-greenschists-are-metamorphic-rocks-that-formed-under-the-lowest-temperatures-and-pressures-the-green-is-due-to-abundan-image344344693.htmlRM2B0674N–Epidote Schist, Madoc, Ontario Greenschists are metamorphic rocks that formed under the lowest temperatures and pressures. The green is due to abundan
Hornfels, Contact Metamophism, Grenville, Quebec Hornfels is the group name for a set of contact metamorphic rocks that have been baked and hardened b Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/hornfels-contact-metamophism-grenville-quebec-hornfels-is-the-group-name-for-a-set-of-contact-metamorphic-rocks-that-have-been-baked-and-hardened-b-image344349113.htmlRM2B06CPH–Hornfels, Contact Metamophism, Grenville, Quebec Hornfels is the group name for a set of contact metamorphic rocks that have been baked and hardened b
Paragonite, Mica, Lanark, Ontario Paragonite is a mineral, related to muscovite; a basic silicate of sodium and aluminum. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/paragonite-mica-lanark-ontario-paragonite-is-a-mineral-related-to-muscovite-a-basic-silicate-of-sodium-and-aluminum-image344396867.htmlRM2B08HM3–Paragonite, Mica, Lanark, Ontario Paragonite is a mineral, related to muscovite; a basic silicate of sodium and aluminum.
Muscovite Mica Muscovite is the most common mica, found in granites, pegmatites, gneisses, and schists, and as a contact metamorphic rock. Muscovite i Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/muscovite-mica-muscovite-is-the-most-common-mica-found-in-granites-pegmatites-gneisses-and-schists-and-as-a-contact-metamorphic-rock-muscovite-i-image344395621.htmlRM2B08G3H–Muscovite Mica Muscovite is the most common mica, found in granites, pegmatites, gneisses, and schists, and as a contact metamorphic rock. Muscovite i
Antigorite, Estrie, Quebec Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/antigorite-estrie-quebec-image344341056.htmlRM2B062ET–Antigorite, Estrie, Quebec
Quartzite, Cambrian, Moine Thrust Zone, Loch Eriboll, Sutherland, Scotland, UK Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/quartzite-cambrian-moine-thrust-zone-loch-eriboll-sutherland-scotland-uk-image356503314.htmlRM2BM03H6–Quartzite, Cambrian, Moine Thrust Zone, Loch Eriboll, Sutherland, Scotland, UK
Stretched Gneiss, Isle Of Mull Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stretched-gneiss-isle-of-mull-image246139004.htmlRMT8CGPM–Stretched Gneiss, Isle Of Mull
Augen Gneiss Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/augen-gneiss-image333114422.htmlRM2A9XJRJ–Augen Gneiss
Antigorite, Thetford Mines, Quebec Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/antigorite-thetford-mines-quebec-image344341085.htmlRM2B062FW–Antigorite, Thetford Mines, Quebec
Pelhamine, Lowell, Vermont Pelhamine is a coarsely fibrous (non-asbestiform) variety of serpentine, commonly referred to as a variety of antigorite bu Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/pelhamine-lowell-vermont-pelhamine-is-a-coarsely-fibrous-non-asbestiform-variety-of-serpentine-commonly-referred-to-as-a-variety-of-antigorite-bu-image344396981.htmlRM2B08HT5–Pelhamine, Lowell, Vermont Pelhamine is a coarsely fibrous (non-asbestiform) variety of serpentine, commonly referred to as a variety of antigorite bu
