Chapter 5 Rocks from molten Rocks liquids from

Chapter 5 : Rocks from molten Rocks liquids from molten liquids Including adaptions from Dupre and Copeland (2004)

Concepts you should know for the exam • • • • Texture – grain size of intrusive (e. g. , granite) and extrusive rocks (e. g. , basalt) Relative cooling rates of intrusive and extrusive igneous rocks Rocks from lavas vs. pyroclastic rocks Mafic, intermediate and felsic rocks Know table! (Temperature, Silica, Na, K, Fe, Mg, Ca content) Melting point as a function of pressure, water content and composition Partial melting of magma-generating rocks Fractional crystallization Shapes of magmatic bodies – sills, dykes, batholiths Hot spots and volcanoes (mafic composition) Volcanoes at convergent margins ( mafic to felsic composition) Volcanoes at divergent margins (mafic composition) Lavas, welded tuff, vesicular basalt, volcanic bombs, pyroclastic flows, volcanic cloud Relation between the shape of volcano, chemistry, viscosity of lavas (shield volcano, cinder cone volcano, composite volcano) Dangerous pyroclastic flows cause almost 30% fatalities natural disasters vs. tsunamis (~20%)

Lecture Outline 1. Where do magmas form? 2. How do igneous rocks differ from one another? 3. 3. How do magmas form? 4. 4. Magmatic differentiation 5. 5. Forms of magmatic intrusion 6. 6. Igneous activity and plate tectonics

Lecture Outline 1. Where do magmas form? 2. How do igneous rocks differ from one another? 3. 3. How do magmas form? 4. 4. Magmatic differentiation 5. 5. Forms of magmatic intrusion 6. 6. Igneous activity and plate tectonics

Divergent Plate Boundary Usually start within continents— grows to become ocean basin

2. How do igneous rocks differ from one another? Texture – size of crystals Coarse-grained rocks Fine-grained rocks Mixed texture rocks

1. How do igneous rocks differ 2. from one another? Texture is related to rate of cooling. Intrusive igneous rocks Extrusive igneous rocks

Andesite - granite near the surface Hand sample-Santiago de Chile Microscope slide

Giant’s Causeway, Ireland

Genetic Classification of Igneous Rocks • Intrusive: Intrusive crystallized from slowly cooling magma intruded within the Earth’s crust; e. g. granite, gabbro

Genetic Classification of Igneous Rocks • Extrusive: Extrusive crystallized from rapidly cooling magma extruded on the surface of the Earth as lava or erupted as pyroclastic material.

Extrusive Igneous Rocks Include: • rocks formed from the cooling of lavas • rocks formed by the cooling of pyroclastic material, i. e. fragmented pieces of magma and material erupted into the air

Last Days of Pompeii-Karl Briullov-Copyright © 1999. George Mitrevski. Auburn University

Mt St Helens crater 08 -780, 60 mph, 800 deg Fpyroclastic flow- USGS

Composition and Classification of Igneous Rocks • Chemistry: e. g. % Si. O 2 • Mineralogy: e. g. – – Felsic (Feldspar and Silica) Intermediate Mafic (Magnesium and Ferric) Ultramafic

Two basic compositional groups: Felsic igneous rocks Mafic igneous rocks

Why last figure is so important • The color and mineral distribution indicate an increasing density and melting temperature. Darker igneous rocks generally weigh more and are formed at higher temperatures and pressures. This reflects the densitystratification of the whole Earth!

Felsic Igneous Rocks: -Igneous rocks rich in minerals high in silica. They include: Granite Rhyolite

Intermediate Igneous Rocks: -Igneous rocks in between in composition between felsic and mafic igneous rocks. They include: Granodiorite Dacite Diorite Andesite

Mafic Igneous rocks -very low silica content, and consist primarily of mafic minerals. The most common ultramafic rock is: Peridotite

What controls the melting temperatures of minerals? *External pressure *and Water content *Internal composition (including internal water content)

Factors Affecting Melting of Minerals (and Rocks) • Pressure: Pressure Increased Pressures raises melting points • Water Content (internal and external to the mineral): mineral) Increased Water Content lowers melting points • Composition: Composition Felsic minerals melt at lower temperatures than mafic minerals

Lecture Outline 1. Where do magmas form? 2. How do igneous rocks differ from one another? 3. 3. How do magmas form? 4. 4. Magmatic differentiation 5. 5. Forms of magmatic intrusion 6. 6. Igneous activity and plate tectonics

4. How do magmas form? When rocks melt (or partially melt). Why do rocks melt? When the temperature exceeds the melting point of the rock or some minerals within the rock.

Partial Melting --Occurs when some of the minerals forming a rock melt at lower temperatures than other minerals within the same rock

If different minerals melt at different pressures that means that different minerals become solid at different temperatures too. What does this imply about the internal composition of a magma body as it cools? ? ?

Fractional Crystallization!

Lecture Outline 1. Where do magmas form? 2. How do igneous rocks differ from one another? 3. 3. How do magmas form? 4. 4. Magmatic differentiation 5. 5. Forms of magmatic intrusion 6. 6. Igneous activity and plate tectonics

Magmatic Differentiation ? What is If, during fractional crystallization, the remaining magma were to erupt it would be (a) more felsic or (b) more mafic than the original magma? ?

Lecture Outline 1. Where do magmas form? 2. How do igneous rocks differ from one another? 3. 3. How do magmas form? 4. 4. Magmatic differentiation 5. 5. Forms of magmatic intrusion 6. 6. Igneous activity and plate tectonics

What do we know about the shape of magmatic bodies? Are they sheets? Blobs? Spheres?

“Magmatic Pipes -101” • Dykes are near-vertical • Sills are horizontal and squeeze in between other layers of rock • Plutons are deep (km) bodies of solidified magma. An example of a plutonic rock is granite or gabbro.

www. jemmoore. com/flying/ shiprock. html Shiprock, NM. It's hard to tell, mainly because I was flying at about 12, 000 ft when I took this picture, but this massive piece of rock sticks up over 2, 000 ft from the

Shiprock, NM • www. jemmoore. com/flying/ shiprock. html • “Shiprock, NM. It's hard to tell, mainly because I was flying at about 12, 000 ft when I took this picture, but this massive piece of rock sticks up over 2, 000 ft from the surrounding plain, and is as big as a small city. It is on Navajo land, and is a significant spiritual site for the Navajo. The hard, volcanic spines radiating out from the main spire are really amazing. From this high up, you couldn't even see an eighteen-wheeler on the ground next to Shiprock, it would be just a speck. ”

6. Igneous activity and plate tectonics Magmatic geosystems: Island arc plate subduction Plate divergence Hot-spot volcanism Continental plate subduction

Geomagmatic systems of Earth

Geomagmatic systems of Earth

Island arc plate subduction ISLAND ARC PLATE SUBDUCTION Island arc volcano Mafic to intermediate intrusives (plutonism) Mafic to intermediate extrusives (volcanism) Subduction zone Oceanic lithosphere

Plate divergent boundary PLATE DIVERGENCE Mid-ocean ridge Basaltic extrusives Basaltic intrusives Partial melting Of upper mantle Rising magma

Hot-spot volcanism HOT-SPOT VOLCANISM Hot-spot volcano Basaltic extrusives Basaltic intrusives Mantle plume (hot spot) Mantle

Continental plate subduction CONTINENTAL PLATE SUBDUCTION Mafic to felsic intrusives Mafic to felsic extrusives Subduction zone Oceanic crust ic ere an ph ce s O tho li Co nt Co inen nt in tal lith enta crus os l m t ph er antle e Continental margin volcano

Summary of Volcanoes • Subduction volcanoes in continental crustal and oceanic crust at convergent plate margins • Hot spot volcanoes (anywhere) • decompression volcanoes at divergent plate margins

END of CHAPTER 5 IGNEOUS ROCKS-rocks from liquid melts