Pages+102-104+Concept+Map

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 * Please fill out the information needed in the table to the right of your name. ||~ Student Name ||~ Concept Map Posted from Bubbl.us ||
 * Fakey McExample || [[image:geology8b-9:bubbl.us_example.JPG width="697" height="523" caption="bubbl.us_example.JPG"]] ||
 * Peter Aziz || [[image:bubbl.us.jpg width="983" height="480" caption="bubbl.us.jpg"]] ||
 * Abiola Adun || [[image:file:///C:/DOCUME%7E1/ABIOLA%7E1/LOCALS%7E1/Temp/moz-screenshot.jpg]][[image:igneous_rock_bubbl.us.JPG]] ||
 * Nikko Andriotis ||  ||
 * Peter Aziz ||  ||
 * Michelle Castaneda || [[image:102-104concept_map.jpg width="800" height="640" caption="102-104concept_map.jpg"]] ||
 * Jessica Cholewa ||  ||
 * Julia Cholewa || [[image:pg102-104_concept_map.1.JPG width="1222" height="1015"]] ||
 * Monica Dudzik || [[image:oops.jpg caption="oops.jpg"]] ||
 * Erik Guevera ||  ||
 * Camelia Hammad ||  ||
 * Sarah Hernandez ||  ||
 * Liliana
 * Ola Kasprzyk ||  ||
 * Micki Laws ||  ||
 * Evan Lopez ||  ||
 * Pedro Lopez ||  ||
 * Jasmin Markicic ||  ||
 * Jaclyn Mazariegos ||  ||
 * Nigel Milosevic || [[image:igneous_rock.JPG]] ||
 * Ermin Murati || [[image:Magma.JPG width="800" height="500" caption="Magma.JPG"]] ||
 * Kenny Nissan ||  ||
 * Thomas Osvath ||  ||
 * Harshang Sheth || [[image:Harshang_Concept_of_Igenous_rocks!!!!!!.jpg width="882" height="524" caption="Harshang_Concept_of_Igenous_rocks!!!!!!.jpg"]] ||
 * Jahde Smith ||  ||
 * Becka Surma ||  ||
 * Ebboney Wilson ||  ||

Magma the Parent Material of the Igneous Rock Abundant evidence supports the fact that the parent material for igneous rocks are called magma Formed by process called partial melting Magma that reached earth’s surface is called lava Igneous rocks that forms when molten rocks solidify at the surface are classified as extrusive or volcanic Magma that loses mobility before reaching the surface eventually crystallizes at depth The Nature of Magma Magma is completely or partly molten material, which on cooling solidifies to form an igneous rock. Most magmas consists of three parts a liquid component, a solid component and a gaseous phase. The liquid portion is called melt, is composed of mobile ions of those elements commonly found in Earth’s crust The solid components in magma are silicate mineral that have crystallized from the melt From magma to Crystalline Rock Crystallization, generates various silicates mineral that reside with the remaining melt Types Of Igneous textures Aphanitic Texture, igneous rocks that form at the surface or as small masses within the upper c rust where cooling is relatively rapid posses a very fine grained texture called apanitic