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Non explosive volcanoes - Garfield Gifts and Talents
Non explosive volcanoes - Garfield Gifts and Talents

... St. Helens, Washington . It doesn’t do much damage because the lava gets pushed out very slowly. ...
Volcanoes/REVIEW
Volcanoes/REVIEW

... watch the powerpoints you have been working on. Notebooks will also be due on Friday, April 24 (there will be no portfolio page for this unit. PART A – Review pages 204-229 in your textbook and use your notebook 1. What is a volcano? __________________________________________________________________ ...
Volcanoes!
Volcanoes!

... Steeper, form in clusters (on sides of shield/composite) ...
Volcanoes affect Earth`s land, air, and water.
Volcanoes affect Earth`s land, air, and water.

... • How volcanic eruptions affect Earth’s surface • How volcanic gases affect the atmosphere • How volcanic activity affects water ...
Questions For Review KEY
Questions For Review KEY

... A shield volcano is broad, flat, and gently sloping. The shield volcano is built of very fluid (typically basaltic) lava. A volcanic dome is more compact and steep-sided dome. The volcanic dome is made of more viscous, silica-rich magmas, andesitic to rhyolitic in ...
Volcanoes - Tanque Verde Unified School District
Volcanoes - Tanque Verde Unified School District

... Where is the nearest volcano to Tucson located? ___________________________________ 2. Features of a volcano include: ________________ – melted rock/molten material ______________________________________________. ___________ – Opening in Earth’s surface where ________________________________________ ...
Three basic types of volcanoes
Three basic types of volcanoes

... and gas spread throughout the atmosphere Eruptions can affect the whole Earth with lower temperatures ...
Chapter 6 study guide
Chapter 6 study guide

... 1. Define volcano 2. Where are most volcanoes found? 3. What are two types of plate boundaries and how does the Earth’s crust move at these boundaries? 4. When lava or magma hardens it forms what type of rock? 5. How are igneous rocks classified? 6. What are the three textures an igneous rock can ha ...
Volcano Vocabulary
Volcano Vocabulary

... Crater ...
Volcano Vocabulary
Volcano Vocabulary

... Crater ...
Volcano Stations Answers
Volcano Stations Answers

... ◦ There is a large scale eruption ◦ Volcanic ash and sulfur-rich gases spread through the atmosphere ◦ Less sunlight reaches the earth ◦ The average global temperature drops ◦ The earth experiences longer, harsher, winters and wetter, milder summers ◦ Worldwide food shortages occur because of widesp ...
Volcanoes SHOW
Volcanoes SHOW

... caldera: a giant crater that can be more than 12.5 miles in diameter ...
Volcanoes - Blacklick Valley School District
Volcanoes - Blacklick Valley School District

...  Opening at the top of the vent is called a crater  Pyroclastic flow – massive avalanches of hot glowing rock and gases (complete destruction) ...
Учитель: Размахнина О
Учитель: Размахнина О

... releasing a cubic kilometer of material. The largest explosion was on record was Toba, thought to have erupted 73,000 years ago. It released more than 1,000 cubic kilometers of material, and created a caldera 100 km long and 30 kilometers wide. The explosion plunged the world into a world wide ice a ...
VOLCANOES form where molten rock is vented at Earth`s surface.
VOLCANOES form where molten rock is vented at Earth`s surface.

... form where molten rock is vented at Earth’s surface. ...
What is Lava? - Princeton ISD
What is Lava? - Princeton ISD

... •Drop average global temperature noticeably ...
What is Lava?
What is Lava?

... The Formation of Magma • Mantle rock melts when the temperature increases or the pressure decreases. ...
Chapter 12
Chapter 12

... That makes it 3 times the height of Mt. Everest. Unlike Everest, Olympus Mons has a very gentle slope. It is up to 550 km at its base. ...
Volcano WebQuest Follow-Up
Volcano WebQuest Follow-Up

... How does viscosity effect an eruption? • The more viscous the lava, the more explosive the eruption. • More viscous materials flow very slowly so they ‘jam up’ the volcano vent until there’s too much pressure and they explode. ...
No Slide Title
No Slide Title

... The area surrounding the Pacific Plate which contains almost 75% of the world’s active volcanoes. ...
Chapter 9 Test Review Notes
Chapter 9 Test Review Notes

... volcanoes. Compared to cinder cones, shield volcanoes are very large. They form when basaltic lava erupts and flows long distances before hardening. Over time, layers of hardened lava build up into a broad-based, shield-shaped volcano. ...
Ch. 9 Study Guide Answers
Ch. 9 Study Guide Answers

... • The volcanoes of Hawaii and other places far from tectonic plate boundaries are known as • Hot Spots ...
Earth Science Final Project
Earth Science Final Project

... 3. Explain in your own words the meaning of a contour line, contour interval, relief, and topographic map. 4. Why do silica-poor magmas produce broad volcanoes with gentle slopes while high-silica magma tends to form volcanic domes with steep sides? 5. Sketch a contour map of a volcano that shows: a ...
Volcanoes Plate Tectonics
Volcanoes Plate Tectonics

... Volcanoes Plate Tectonics Icons key: ...
Chapter 6 Volcanoes
Chapter 6 Volcanoes

... Four major kinds of pyroclastic materials &descriptions: 1.Volcanic blocks- largest pieces, of solid rock 2.Volcanic bombs- largest blobs of magma harden in the air, shape of bomb. 3.Lapilli- “little stone” little bits of magma become solid before hit ...
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Olympus Mons



Olympus Mons /ɵˌlɪmpəs ˈmɒnz/ (Latin for Mount Olympus) is a very large shield volcano on the planet Mars. By one measure, it has a height of nearly 25 km (16 mi). Olympus Monsstands almost three times as tall as Mount Everest's height above sea level. It is the youngest of the large volcanoes on Mars, having formed during Mars's Amazonian Period. It is currently the largest volcano discovered in the Solar System and had been known to astronomers since the late 19th century as the albedo feature Nix Olympica (Latin for ""Olympic Snow""). Its mountainous nature was suspected well before space probes confirmed its identity as a mountain.The volcano is located in Mars's western hemisphere at approximately 18.65°N 226.2°E / 18.65; 226.2, just off the northwestern edge of the Tharsis bulge. The western portion of the volcano lies in the Amazonis quadrangle (MC-8) and the central and eastern portions in the adjoining Tharsis quadrangle (MC-9). Two impact craters on Olympus Mons have been assigned provisional names by the International Astronomical Union. They are the 15.6 km (9.7 mi)-diameter Karzok crater (18°25′N 131°55′W) and the 10.4 km (6.5 mi)-diameter Pangboche crater (17°10′N 133°35′W). The craters are notable for being two of several suspected source areas for shergottites, the most abundant class of Martian meteorites.
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