Chapter Three Igneous Processes and Igneous Rocks CHAPTER – 3 IGNEOUS ROCKS *IGNEOUS ROCKS: ROCKS THAT COOLED AND FIRE CRYSTALLIZED DIRECTLY FROM MOLTEN ROCK, EITHER AT THE SURFACE OR DEEP UNDERGROUND *MAGMA: MOLTEN ROCK WITHIN THE EARTH *LAVA: WHEN MAGMA REACHES EARTH’S SURFACE *MOST IGNEOUS PROCESSES ARE HIDDEN FROM VIEW *REGIONAL EROSION EXPOSES ANCIENT IGNEOUS EVENTS DISTRIBUTION OF MAJOR CONTINENTAL IGENOUS ROCKS MOLTING ROCKS AND CRYSTALLIZING MAGMA • MAGMA FORMATION: HEATED UNGERGROUND MINERALS – BONDS BROKEN- BECOMES MAGMA – CHEMICAL COMPOSITION OF MAGMA CHANGES • MAGMA COOLING AND CRYSTALLIZATION: AS COOLING PROGRESSES, DIFFERENT MINERALS CRYSTALLIZE EFFECT ON THERMAL ENERGY CLASSIFICATION OF IGNEOUS ROCKS: • TEXTURE: SIZE AND SHAPE OF MINERAL CRYSTALS CRYSTAL GROWTH DURING COOLING • MINERAL CONTENT:CHEMICAL COMPOSITION COOLING HISTORY • TEXTURE: RATE AT WHICH MAGMA OR LAVA COOL WHEN 100 – 1000 YRS FOR COOLING TIME TO GROW LARGER CRYSTALS CRYSTALS CAN BE VISIBLY SEEN PHANERTIC TEXTURE • INTRUSIVE ROCKS (OR PLUTONIC ROCKS) SLOW COOLING OCCURS WHEN MAGMAS INTRUDE PREEXISTING SOLID ROCKS *VOLCANIC GLASS: WHEN LAVA SUDDENLY COOLS, NO TIME TO FORM CRYSTALS. TEXTURE IS GLASSY. *PUMICE: FORMS WHEN HIGHLY GASEOUS, SILICA – RICH LAVA COOLS VERY RAPIDLY *OBSIDIAN: VERY Si-RICH LAVAS CONTAINING LESS GAS, COOL VERY QUICKLY IGNEOUS COMPOSITION • MAGMA O2, Si, Al, Fe, Ca, Mg, Na, K, S. • DISSOLVED GASSES WATER VAPOR, CO2, SO2. • SILICATES ARE THE MAJOR CONSTITUENTS OF IGNEOUS ROCKS CLASSIFICATION OF IGNEOUS ROCKS AND MAGMAS IGNEOUS ROCK - CHART CREATION OF MAGMA: * PARTIAL MELTING WHEN ROCKS MELT TO PRODUCE MAGMA PARTIAL MELTING DIFF. MELTING POINT EX: ALBITE = 1118 0C ANORTHITE = 1553 0C * MELTING OF ROCKS DEPENDS ON HEAT PRESSURE AMOUNT OF H2O IN THE ROCKS. • THERMAL ENERGY HEAT SOURCES GEOTHERMAL GRADIENT MELTING TEMPERT.-DRY MELTING TEMPERT.-WET LITHOSPHERIC THINNING L. THINNING-CONTD THINNING-CONTD. FLUIDITY AND VISCOSITY OF MAGMA: MAGMA RISES BECAUSE IF IT IS LESS DENSE THAN SURROUNDING ROCK EXPANDING GASES DRIVE IT UPWARD IT IS SQUEEZED UPWARD BY SURROUNDING ROCKS VISCOSITY: FLUID RESISTANCE TO FLOW A) INCREASES WITH DECREASING TEMPERATURE B) MINERAL (SILICA) CONTENT INCREASES VISCOSITY VALUE. CRYSTALLIZATION OF MAGMA: *MINERALS MELT AT THE SAME TEMPERATURE AT WHICH THEY CRYSTALLIZE FIRST TO MELT LAST TO CRYSTALLIZE * AT EACH STAGE OF COOLING, CRYSTAL/LIQUID RATIO CHANGES OCEANIC PLATE SUBDUCTS MAGMA MIXING BOWEN’S REACTION SERIES: A) BOTH MAFIC AND FELSIC ROCKS CAN CRYSTALLIZE FROM AN ORIGINALLY MAFIC MAGMA B) EARLY – FORMING CRYSTALS REMAINING IN CONTACT WITH THE STILL – LIQUID MAGMA REACT WITH IT TO EVOLVE INTO DIFFERENT MINERALS BOWEN’S REACTION SERIES EARLY-FORMING CRYSTALS MAGMA & EARLY FORMING CRYSTALS SILICATE MINERALS CAN CRYSTALLIZE FROM MAFIC MAGMAS TWO WAYS: DISCONTINUOUS SERIES • • • • • OLIVINE PYROXINE AMPHIBOLE BIOTITE MICA MINERALS WITHOUT Fe, Mg. CONTINUOUS SERIES • CALCIUM PLAGIOCLASE • SODIUM PLAGIOCLASE CONTDHOW MAGMA CHANGES AS IT COOLS: INTRUSIVE ROCK FORMATION: • RISING MAGMA MAY FORCE OVERLYING ROCKS TO BULGE UPWARD RESULTING ROCK APPEARS AS A DOOMED INTRUSION WITHIN OTHER ROCKS THIS STRUCTURE IS KNOWN AS DIAPIR • XENOLITHS: WHEN PREEXISTING ROCK IS ASSIMILATED IN A MAGMA, THEY APPEAR IN THE SOLIDIFIED ROCK AS DISTINCT BODIES – XENOLITHS PLUTONS: MAGMA THAT COOL UNDERGROUND FORM PLUTONS TABULAR PLUTONS o DIKES o SILLS – DISTINGUISHED FROM EXTRUSIVE FLOWS BY A)EVIDENCE OF HEATING OF ADJACENT ROCK SURFACES B)EVIDENCE OF INCLUSIONS OF COUNTRY ROCK IN BOTH UPPER & LOWER SILL SURFACE C)LACK OF VESICLES ( HOLES FROM GAS BUBBLES ) ON UPPER SURFACE D)LACK OF WEATHERING OF LARGE SURFACE. PLUTONIC IGNEOUS FEATURES BATHOLITHS AND LARGE PLUTONS: 1. LACCOLITHS 2. LAPOLITHS 3. BATHOLITHS A)DEFINITION B)EXAMPLES C)TEXTURE SHIPROCK PEAK SEMINARY RIDGE TOPOGRAPHIC RIDGE SILLS AND LAVA FLOWS LACCOLITH PLATE TECTONICS AND IGNEOUS ROCKS: A) THE ORIGIN OF BASALT & GABBROS 1) INTRODUCTION * UPPER MANTLE LACKS LIGHT ELEMENTS *DEEPER MANTLE POSSESSES SOME LIGHT ELEMENTS *PRESENCE OR ABSENCE OF LIGHT ELEMENTS IN GABBRO & BASALT IDENTIFIES SOURCE OF PARENT MAGMA PLATE SETTINGS & BASALTS BASALTS-OCEAN & LAND ANDESITE & DIORITE ORIGIN B) ORIGIN OF ANDESITES & DIORITES ORIGIN OF FELSIC ROCKS IGNEOUS ************ A) ROCKS OF THE HIGHLANDS 1. 4 – 4.5 * 109 YRS OLD 2. PRINCIPALLY ANORTHOSITE – COMPOSED OF Ca – PLAGIOCLASE ANORTHITE 3. NO WATER – CONTAINING MINERALS 4. NO RELATIONSHIP TO PLATE TECTONICS 5. NO RELATIONSHIP TO MOON’S INTERNAL HEAT GEOLOGY AT A GLANCE CHAPTER SUMMARY