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... hardens beneath Earth’s surface creates landforms.  F.3.4.3. Analyze other distinct features that occur in volcanic areas. ...
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Crustal Deformation

... 27. How are volcanoes formed in subduction zones? What is the magma composed of in these regions? Give an example of this type of volcano on Earth. ...
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... Large Igneous Province Fed by massive mantle plumes Caused by flood basalts (especially fluid basaltic lavas) Discharge over time through long fissures (cracks) Create large plateaus ...
What mainly controls eruptive style? Viscosity in magma 2. Eruptive
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Haystack Rock - City of Cannon Beach

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... Describe the processes that change the composition of magma Bowen’s Reaction Series: Minerals crystallize at different temps. Mafic mineras crystalize at hotter temps. Felsic at cooler. So the mafic minerals crystallize and settle to the bottom of the magma chamber, leaving the rest of the magma mo ...
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Igneous Rocks - Occurrence and Classification

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... Olympus Mons is the largest volcano on Mars. This shield volcano, similar to volcanoes in Hawaii, measures 624 km (374 mi) in diameter by 25 km (16 mi) high. It is 100 times larger than Mauna Loa on Earth. Located on the Tharsis Plateau near the equator, Olympus Mons is bordered by an escarpment. Th ...
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... Shield volcanoes are formed from quiet (non-explosive) eruptions. The eruptions usually consist of flowing lava along a large area. After numerous eruptions, a dome-shaped volcanic mountain is formed from the built-up lava flows. Composite Volcanoes Composite volcanoes are very large and are formed ...
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What do we expect in a volcanic eruption?

... • Lava flows from from others (called some pyroclastics. Better • Range from mafic than fireworks? (e.g. basalt) to • You bet!!! felsic, like all ign rx • Rocks may form from ...
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Level Mountain



Level Mountain is a massive shield volcano in Cassiar Country, northwestern British Columbia, Canada, located just southeast of Callison Ranch, southwest of Dease Lake and about 50 km (31 mi) north of Mount Edziza. It lies on the Nahlin Plateau, comprising a series of buttes and ridges. The shield is lightly glaciated, as compared to the Coast Mountains just to the west. The only named summit of Level Mountain is Meszah Peak on the north side of the shield with an elevation of 2,190 m (7,185 ft), making it the highest point of Level Mountain. Immediately to the west, however, are the Heart Peaks, a related volcanic range just east of the Sheslay River, which is the edge of the Nahlin Plateau.Level Mountain rises above adjacent forested lowlands and undulating alpine areas surround the steeper central peaks. Streams that originate from these peaks drain across the Nahlin Plateau.
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