Rock Density Lab Objectives: (1)Compare the densities of continental and oceanic crust (2)Relate rock density to the process of subduction at plate boundaries. Mafic vs. Felsic Magmas: Determine Eruption Pattern at Volcanoes Explosive or Quiet? Differences in density drive sea-floor recycling and plate tectonics: Mafic vs. Felsic Igneous Rocks Mafic Characteristics Felsic Characteristics Rock density depends on the or that make up a rock Density depends on necessarily rock type. – not Igneous Rocks of the Ocean Crust Mafic ~ 50 % silica High in Magnesium (Mg) and Iron (Fe) Dark color Dense Basalt & Gabbro Rock of the ocean crust and upper mantle Mafic Igneous Rocks have heavy minerals with IRON & Magnesium Elements • Iron • Magnesium • Calcium make Minerals •Olivine •Amphiboles •Ca feldspars “MAFIC” and are dark in color due to the iron & magnesium. http://whatonearth.olehnielsen.dk/rocks/volcanicrocks.asp Igneous Rocks of Continental Crust Felsic ~70% silica Light color Light Granites, Rhyolites, Andesites • High silica Felsic Igneous Rocks have light minerals with silicon & oxygen Elements • silicon • oxygen make Minerals •Quartz (silica) •Feldspars “Felsics” and are light in color because they lack iron and are rich in silica. http://whatonearth.olehnielsen.dk/rocks/volcanicrocks.asp Mafic vs. Felsic Densities: Ocean vs. Continental Crust Made of… Ocean Crust Continental Crust Mafic/Felsic Density Age Thickness Differences in density drive sea-floor recycling & plate tectonics: •The ocean floor is made of basalt (mafic magma). Continental crust is made of granite (from felsic magmas). •Ocean crust is denser than continental crust. •When ocean and continental crust collide … the denser ocean crust sinks back into the mantle (Subduction). This recycles the ocean floor. Mafic vs. Felsic Magma: Volcano Shape Mafic vs. Felsic Magma: Volcanic Activity