Use LEFT and RIGHT arrow keys to navigate between flashcards;
Use UP and DOWN arrow keys to flip the card;
H to show hint;
A reads text to speech;
59 Cards in this Set
- Front
- Back
Igneous rock definition |
Rocks formed by the cooling and solidifying of molten materials |
|
Magma definition |
Molten materials Underground |
|
Lava definition |
Molten materials above ground |
|
Volatile definition |
Gas |
|
Extrusive igneous rock definition |
Rocks that form from lava at the surface of the Earth |
|
Intrusive igneous rock definition |
Rocks that form from magma Underground |
|
Granitic (felsic) composition |
70% Silicia |
|
Basaltic (mafic) composition |
50% si/o 50%fe/mg |
|
Andesitic (intermediate) composition |
25% dark silicates |
|
Ultramafic definition |
Mostly iron and magnesium, periodotite is ultramafic |
|
List three main components of magma |
Liquid, solids, gases |
|
Igneous textures |
Aphanitic, phaneritic, vesicular, glassy, porphyritic, and pyroclastic |
|
Aphanitic definition |
Following grain fast cooling I produced in lava flow |
|
Phaneritic definition |
Coarse grain cooled slowly in magma chamber |
|
Testicular definition |
Gas, void space, produced on top of frothy lava flow |
|
Glassy definition |
High Si content, no minerals, produced in lava flow |
|
Porphyritic definition |
Start schooling underground finishes cooling above ground has coarse and fine grain mineral |
|
Pyroclastic definition |
Hot cold tephra existing rocks shooting out places and stuff |
|
Four basic compositional groups of igneous rocks in order from highest silica content to least |
Felsic intermediate mafic ultramafic |
|
How does cooling rate influence Crystal size |
Slow cooling equals big crystals fast cooling equals small |
|
How are granite and rhyolite different in what ways are they the same |
They're both felsic rocks granite cool slower and rhyolite has much finer Crystal giving it a glassy appearance |
|
Define igneous texture |
The overall appearance size shape and arrangement of mminerals |
|
how do light colored igneous rocks differ from dark-colored igneous rocks |
Light color has more silica content dark color has more iron magnesium content |
|
What is decompression melting |
When a confining pressure drops efficiently decompression melting is true word it occurs were hot solid mantle Rock and Sons Moving in to regions of lower pressure, also occurs when ascending mantle plumes reach the uppermost mantle |
|
Addition of volatiles |
Reduces viscosity in magma it forms at locations where hot mantle this is what's volatile |
|
Increase temperature affects what |
Decreases viscosity |
|
Magmatic differentiation |
Magma changing composition, generating more than one rock type from a single magma |
|
Crystal setting |
Occurs when earlier forms minerals are denser than the liquid portion and sink to the bottom of the magma chamber |
|
Assimilation |
When magma rises the dislodge is surrounding rocks and the Rocks melt and become part of the magma body |
|
Magma mixing |
Lenox to separate magma Chambers join together and create a single Mass, the more buoyant mass overtakes the slowly Rising body |
|
What role does water and volatile play in formation of magma |
Thet will lower the melting temperature of rock allowing it to melt |
|
Viscosity definition |
Measure of fluids resistance to flow |
|
Basaltic lavas |
A'a' and pahoehoe Low si, more fluid-like |
|
Pahoehoe |
Top cools starts forming glass, quiet |
|
A'a |
Chunky glass, slow, comes out cooler, crunchy |
|
Block lavas |
Lava that has a surface of angular blocks associated with material having andesitic and rhyolitic compositions |
|
Pyroclastic material |
Volcanic rock ejected during the eruption includes Ash bombs in blocks |
|
Fissure |
A crack in a rock along where there is is distinct separation |
|
Vent definition |
Surface opening of a conduit or pipe |
|
Shield volcano |
Bra gentle sleeping volcano built from fluid basaltic lavas |
|
Composite cone volcano |
Volcano composed of both lava flows and pyroclastic material |
|
Pyroclastic flow |
Highly textured mixture largely of Ash and pumice fragments that travels down the flanks of a volcano or along the surface of the ground |
|
Lahar |
A debris flow on the slopes of a volcano that results when unstable layers of Ash and debris become saturated and flow downslope usually following stream channels |
|
Caldera |
Large depression typically caused by collapse ejection of summit area of volcano |
|
Flood basalts |
Flows of basaltic lava that issue from numerous cracks or fissures and commonly cover extensive areas to thickness of hundreds of meters |
|
What are the three factors that influence viscosity of magma |
Temperature volatile content and silica content, increase in temperature equals decrease in viscosity, increase in volatile gases equals decrease in viscosity, increase in silica content equals increase in viscosity |
|
List the three Magma's basaltic in ascitic and rhyolitic in order from silica-rich to least silica-rich |
Rhyolitic(felsic), andesitic (intermediate), basaltic (mafic) |
|
What's the main gases released during a volcanic eruption what role do gases play in interruption |
Water, carbon dioxide, nitrogen, and sulfur dioxide. These gases escaped as a confining pressure over magma is released releasing the gases into the atmosphere |
|
What are pyroclastic materials list and describe |
Palee hair and tears -thin strands of glass Lapilli(cinders) 2mm-64mm Bombs>64 mm |
|
Where do most shield volcanoes form on the ocean floor are on the continent |
Ocean floor |
|
Describe the composition and viscosity of lava associated with shield volcanoes |
50% silica oxygen 50% iron magnesium, low viscosity, least pyroclastic, when did 2% gas content |
|
How is a crater different from a Caldera |
A crater is a small depression at the top of a volcano Caldera is a crater that has a diameter greater than 1 km |
|
Distinguish among conduit vent and crater |
The conduit is the to which magma flows from the magma chamber to the vent, the vent is where magma is emitted from a volcano, a crater is a bowl like depression at the top of a volcano |
|
How did the size and steepness of slopes of a cinder cone compare with those of a shield volcano |
Cinder cones are much smaller and steeper than shield volcanoes |
|
Describe the composition of a cinder cone |
Basaltic, generally loose scoria |
|
Describe the composition and viscosity of the lava sociated with composite cone |
Silica-rich magma within andesitic composition High viscosity |
|
Difference between a Lahar and pyroclastic flow |
Lahars are volcanic mudflows created when Mater and Ash mix and can occur long after a volcanic eruption pyroclastic flows are Avalanches containing a hot volcanic gases Josh and Volcanic bombs |
|
Where are most composite cone volcanoes located |
The ring of fire in a narrow Zone that rims the Pacific Ocean |
|
Cinder cone |
A rather small volcano built primarily of ejected lava fragments that consists mostly of Pea to Walnut |