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Published byLiliana Ward Modified over 6 years ago
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34. Pegmatites Dan Barker April 2009 Pegmatites are coarse-
grained rocks. Most are granitic. 2-meter long quartz and K-feldspar crystals, Althaus pegmatite, Llano Uplift, TX
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Layers in Althaus pegmatite, TX
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Coarse core below layers,
Althaus pegmatite, TX
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"Line rock" in pegmatite, Ramona CA
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False cleavage in quartz core of pegmatite, Pala, CA
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Pegmatite and schist, Pemaquid Point ME
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Pegmatite at contact of Port Mouton granite pluton, Nova Scotia
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Pegmatite/gneiss contact, Palermo NH
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Pegmatites in the Painted Wall, Black Canyon of the Gunnison
River, CO
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Crossing pegmatites, Westerly granite, RI
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Pegmatite offset by a dike of "aplite" (fine equigranular light-
colored granite), Sparta, GA
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Small systematically offset
pegmatite in Valley Spring Gneiss, Inks Lake State Park, TX
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Quartz core and large K-feldspar crystals in pegmatite, Inks
Lake State Park, TX
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Intersecting pegmatites, Wausau WI
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Not all pegmatites are granitic. This one consists of sodic
clinopyroxene and alkali feldspar. Nevlunghavn, Norway.
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The gabbro pegmatite (plagioclase and pyroxenes) on the
right is in a thick basalt flow, Mt Pleasant quarry, NS
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Gabbro pegmatite with sulfides (arrow), Port Coldwell
Complex, ONT
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Pegmatite (plagioclase and clinopyroxene) Port Coldwell ONT
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Another weird pegmatite from the Port Caldwell complex. The red
is altered iron-rich olivine; the rest is plagioclase.
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Another from the same place; plagioclase and blue amphibole.
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