18-1 Continued 10. Label the Diagrams As Composite, Cinder

Total Page:16

File Type:pdf, Size:1020Kb

18-1 Continued 10. Label the Diagrams As Composite, Cinder NAME ________________________________ Date ______________ Class _____________ Ch. 18 Study Guide (Earth Science) 18-1 Multiple Choice Identify the choice that best completes the statement or answers the question. ____ 1. A bowl-shaped depression that forms around the vent of a volcano is a a. magma chamber. c. vent. b. crater. d. sill. ____ 2. Broad, gently sloping volcanoes with quiet eruptions are called a. cinder cones. c. shield volcanoes. b. hot spots. d. composite volcanoes. ____ 3. Lava erupts through an opening in Earth’s crust called a a. caldera. c. vent. b. volcano. d. crater. ____ 4. Which of the following forms when the top or side of a volcano collapses into the magma chamber? a. vent c. pyroclastic flow b. dike d. caldera ____ 5. Most volcanoes form a. at hot spots. c. in the center of ocean plates. b. in the middle of continents. d. at plate boundaries. ____ 6. The most explosive volcanoes are a. hot spots. c. cinder cones. b. composite volcanoes. d. shield volcanoes. ____ 7. When magma reaches Earth’s surface, it is called a. lava. c. calderas. b. a vent. d. a pyroclastic flow. ____ 8. ________ form(s) where plates move apart. a. Hot spots. c. Subduction zones. b. Divergent volcanism. d. Convergent volcanism. ____ 9. Volcanoes that form far from plate boundaries are associated with a. subduction zones. c. ocean ridges. b. divergent boundaries. d. hot spots. 18-1 Continued 10. Label the diagrams as composite, cinder-cone, or shield volcano. Identify the type or types of volcano being described as Shield, Cinder, or Composite Volcano. 11. ____________________ Forms when small pieces of magma are ejected into the air then fall back to Earth and pile up around a vent. 12. ____________________ Has broad, gently sloping sides and a nearly circular base. 13. ____________________ Mauna Kea in Hawaii is an example. 14. ____________________ Forms when layers of basaltic lava accumulate during a nonexplosive eruption. 15. ____________________ Forms when layers of hardened lava chunks alternate with lava. 16. ____________________ Small volcano with steep sides. 17. ____________________ Forms from lava that contains relatively small amounts of gases and silica. 18. ____________________ Forms from lava that is higher in water and silica content than lava that forms shield volcanoes 19. ____________________ Fueled by magma that contains large amounts of silica, water, and gases. 20. ____________________ Potentially the most dangerous to humans and most destructive to the environment. 21. ____________________ Mount St. Helens and Mount Rainier are examples. 18-1 Continued 22. Use each of the terms below just once to complete the passage. Hawaiian Islands crust divergent hot spots Iceland mantle volcanoes ocean ridges Circum-Pacific Belt western convergent Most of the world’s volcanoes form along (a) ______________________ plate boundaries. Slabs of oceanic crust descend into the (b) ______________________ and release water, causing portions of the mantle to melt. The magma that forms is forced upward through the overlying plate and forms (c) ______________________ when it reaches Earth’s surface. The (d) ______________________ marks the locations of most convergent boundary volcanoes. It stretches along the (e) ______________________ coasts of North and South America and down the eastern coast of Asia. At (f) ______________________ plate boundaries, magma is forced upward into fractures and faults that form as plates separate or spread apart. Most of the volcanoes that form along divergent boundaries are located underwater along (g) ______________________. This type of volcanic activity can be observed above sea level in (h) ______________________, which sits atop the Mid-Atlantic Ridge. Some volcanoes that form far from plate boundaries form over (i) ______________________, which are unusually hot regions of Earth’s mantle. At hot spots, high-temperature plumes melt rock. The magma that forms moves upward toward the (j) ______________________ and melts the crust to form a volcano. As a tectonic plate moves over a hot spot, a string of volcanoes forms. The (k) ______________________ are the result of a hot spot. 18-2 Continued Indicate whether the statement is true or false. ____ 23. Magma is a mixture of molten rock, suspended minerals, and gases. ____ 24. Pressure decreases with depth below Earth’s surface. ____ 25. Magma forms when rocks begin to melt. ____ 26. Wet minerals and rocks melt at lower temperatures than do dry minerals and rocks. ____ 27. As pressure increases, the temperature at which a dry substance melts increases. 18-2 Continued Answer the following questions: 28. How does the viscosity of magma change as magma cools? _______________________________________________________________________ 29. Does cooler magma flow more or less quickly than hotter magma? _______________________________________________________________________ 30. Is the viscosity of magma that is high in silica higher or lower than magma that is low in silica? _______________________________________________________________________ 31. Which type of lava—basaltic lava or rhyolitic lava—flows faster? Explain. _______________________________________________________________________ _______________________________________________________________________ 18-3 Matching a. stock d. pluton b. sill e. batholith c. laccolith f. dike ____ 32. Largest pluton ____ 33. Mushroom-shaped pluton ____ 34. Instrusive rock body. ____ 35. Irregularly shaped pluton that is similar to a batholith, but smaller in size. ____ 36. Pluton that is parallel to the rocks it intrudes. ____ 37. Pluton that cuts across preexisting rocks. .
Recommended publications
  • Source to Surface Model of Monogenetic Volcanism: a Critical Review
    Downloaded from http://sp.lyellcollection.org/ by guest on September 28, 2021 Source to surface model of monogenetic volcanism: a critical review I. E. M. SMITH1 &K.NE´ METH2* 1School of Environment, University of Auckland, Auckland, New Zealand 2Volcanic Risk Solutions, Massey University, Palmerston North 4442, New Zealand *Correspondence: [email protected] Abstract: Small-scale volcanic systems are the most widespread type of volcanism on Earth and occur in all of the main tectonic settings. Most commonly, these systems erupt basaltic magmas within a wide compositional range from strongly silica undersaturated to saturated and oversatu- rated; less commonly, the spectrum includes more siliceous compositions. Small-scale volcanic systems are commonly monogenetic in the sense that they are represented at the Earth’s surface by fields of small volcanoes, each the product of a temporally restricted eruption of a composition- ally distinct batch of magma, and this is in contrast to polygenetic systems characterized by rela- tively large edifices built by multiple eruptions over longer periods of time involving magmas with diverse origins. Eruption styles of small-scale volcanoes range from pyroclastic to effusive, and are strongly controlled by the relative influence of the characteristics of the magmatic system and the surface environment. Gold Open Access: This article is published under the terms of the CC-BY 3.0 license. Small-scale basaltic magmatic systems characteris- hazards associated with eruptions, and this is tically occur at the Earth’s surface as fields of small particularly true where volcanic fields are in close monogenetic volcanoes. These volcanoes are the proximity to population centres.
    [Show full text]
  • A Unique Volcanic Field in Tharsis, Mars: Monogenetic Cinder Cones and Lava Flows As Evidence for Hawaiian Eruptions
    42nd Lunar and Planetary Science Conference (2011) 1379.pdf A UNIQUE VOLCANIC FIELD IN THARSIS, MARS: MONOGENETIC CINDER CONES AND LAVA FLOWS AS EVIDENCE FOR HAWAIIAN ERUPTIONS. P. Brož1 and E. Hauber2, 1Institute of Geophysics ASCR, v.v.i., Prague, Czech Republic, [email protected], 2Institut für Planetenforschung, DLR, Berlin, Germany, [email protected]. Introduction: Most volcanoes on Mars that have Data: We use images from several cameras, i.e. been studied so far seem to be basaltic shield volca- Context Camera (CTX), High Resolution Stereo Cam- noes, which can be very large with diameters of hun- era (HRSC), and High Resolution Imaging Science dreds of kilometers [e.g., 1] or much smaller with di- Experiment (HiRISE) for morphological analyses. ameters of several kilometers only [2]. Few Viking Topographic information (e.g., heights and slope an- Orbiter-based studies reported the possible existence gles) were determined from single shots of the Mars of cinder cones [3,4] or stratovolcanoes [5-7], and only Orbiter Laser Altimeter (MOLA) in a GIS environ- the advent of higher-resolution data led to the tentative ment, and from stereo images (HRSC, CTX) and de- interpretation of previously unknown edifices as cinder rived gridded digital elevation models (DEM). cones [8] or rootless cones [9]. The identification of Morphometry: For comparison between the cinder cones can constrain the nature of eruption proc- cones and terrestrial morphological analogues (i.e. esses and, indirectly, our understanding of the nature cinder cones [10]) we determined some basic mor- of parent magmas (e.g., volatile content). Here we re- phometric properties and their ratios (e.g., crater di- port on our observation of a unique cluster of possible ameter [WCR] vs.
    [Show full text]
  • The Science Behind Volcanoes
    The Science Behind Volcanoes A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, volcanic ash and gases to escape from the magma chamber below the surface. Volcanoes are generally found where tectonic plates are diverging or converging. A mid-oceanic ridge, for example the Mid-Atlantic Ridge, has examples of volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by convergent tectonic plates coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust in the interiors of plates, e.g., in the East African Rift, the Wells Gray-Clearwater volcanic field and the Rio Grande Rift in North America. This type of volcanism falls under the umbrella of "Plate hypothesis" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so- called "hotspots", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. Volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere or troposphere; however, they also absorb heat radiated up from the Earth, thereby warming the stratosphere.
    [Show full text]
  • Volcanoes a to Z
    Mount St Helens National Volcanic Monument – Teacher’s Corner -Teacher Info. Gifford Pinchot National Forest USDA Forest Service Volcanoes A to Z – Bus Activity Time Requirement: all day Exhibit / Trail Used: all exhibits/trails visited Locations: all locations visited, review on the bus en route back to your school. This activity is to be completed throughout the day and between other activities. Students will make note of key words while reading exhibits, interpretive signs, or labels, or by hearing them from each other, their teacher, movies or rangers. Consider distributing on the bus and collecting on the bus. Goal: 1) The student will become familiar with terminology related to the study of volcanoes, geology, or the ecosystems that surround them. Objectives: 1) The student will listen attentively. 2) The student will recall and list vocabulary words for things and concepts encountered on a field trip to Mount St. Helens National Volcanic Monument. 3) The student will distinguish nouns from other parts of speech. WASHINGTON EALRS and OREGON BENCHMARK STANDARDS Washington Social Studies 2.0- The student understands the complex physical and human characteristics of places and regions. Geography 2.1- Describe the natural characteristics of places and regions. Science 4.2 Use writing and speaking skills to organize and express science ideas. a. Use science vocabulary appropriately in written explanations, conversations and verbal presentations. Oregon Science-CCG The Dynamic Earth- Understand the properties and limited availability of the materials which make up the Earth. BM1- Recognize physical differences in Earth materials. Language-CCG Select functional, precise, and descriptive words appropriate to audience and purpose.
    [Show full text]
  • Identification of Volcanic Rootless Cones, Ice Mounds, and Impact 3 Craters on Earth and Mars: Using Spatial Distribution As a Remote 4 Sensing Tool
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, XXXXXX, doi:10.1029/2005JE002510, 2006 Click Here for Full Article 2 Identification of volcanic rootless cones, ice mounds, and impact 3 craters on Earth and Mars: Using spatial distribution as a remote 4 sensing tool 1 1 1 2 3 5 B. C. Bruno, S. A. Fagents, C. W. Hamilton, D. M. Burr, and S. M. Baloga 6 Received 16 June 2005; revised 29 March 2006; accepted 10 April 2006; published XX Month 2006. 7 [1] This study aims to quantify the spatial distribution of terrestrial volcanic rootless 8 cones and ice mounds for the purpose of identifying analogous Martian features. Using a 9 nearest neighbor (NN) methodology, we use the statistics R (ratio of the mean NN distance 10 to that expected from a random distribution) and c (a measure of departure from 11 randomness). We interpret R as a measure of clustering and as a diagnostic for 12 discriminating feature types. All terrestrial groups of rootless cones and ice mounds are 13 clustered (R: 0.51–0.94) relative to a random distribution. Applying this same 14 methodology to Martian feature fields of unknown origin similarly yields R of 0.57–0.93, 15 indicating that their spatial distributions are consistent with both ice mound or rootless 16 cone origins, but not impact craters. Each Martian impact crater group has R 1.00 (i.e., 17 the craters are spaced at least as far apart as expected at random). Similar degrees of 18 clustering preclude discrimination between rootless cones and ice mounds based solely on 19 R values.
    [Show full text]
  • The Boring Volcanic Field of the Portland-Vancouver Area, Oregon and Washington: Tectonically Anomalous Forearc Volcanism in an Urban Setting
    Downloaded from fieldguides.gsapubs.org on April 29, 2010 The Geological Society of America Field Guide 15 2009 The Boring Volcanic Field of the Portland-Vancouver area, Oregon and Washington: Tectonically anomalous forearc volcanism in an urban setting Russell C. Evarts U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA Richard M. Conrey GeoAnalytical Laboratory, School of Earth and Environmental Sciences, Washington State University, Pullman, Washington 99164, USA Robert J. Fleck Jonathan T. Hagstrum U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA ABSTRACT More than 80 small volcanoes are scattered throughout the Portland-Vancouver metropolitan area of northwestern Oregon and southwestern Washington. These vol- canoes constitute the Boring Volcanic Field, which is centered in the Neogene Port- land Basin and merges to the east with coeval volcanic centers of the High Cascade volcanic arc. Although the character of volcanic activity is typical of many mono- genetic volcanic fi elds, its tectonic setting is not, being located in the forearc of the Cascadia subduction system well trenchward of the volcanic-arc axis. The history and petrology of this anomalous volcanic fi eld have been elucidated by a comprehensive program of geologic mapping, geochemistry, 40Ar/39Ar geochronology, and paleomag- netic studies. Volcanism began at 2.6 Ma with eruption of low-K tholeiite and related lavas in the southern part of the Portland Basin. At 1.6 Ma, following a hiatus of ~0.8 m.y., similar lavas erupted a few kilometers to the north, after which volcanism became widely dispersed, compositionally variable, and more or less continuous, with an average recurrence interval of 15,000 yr.
    [Show full text]
  • TESTING the PSEUDOCRATER HYPOTHESIS. MC Payne1 and JD
    Sixth International Conference on Mars (2003) 3070.pdf TESTING THE PSEUDOCRATER HYPOTHESIS. M. C. Payne1 and J. D. Farmer1, 1Arizona State University (Department of Geological Sciences, PO Box 1404, Tempe, AZ 85287, [email protected], [email protected]) Introduction: In a regional study of the margin of proved more helpful than the DEM, which had a spa- the north polar cap, a field of coniform features was tial resolution of ~230 m/pixel. observed in the Olympia Planitia region and hypothe- Comparisons with Analog Landforms: A num- sized to be a pseudocrater field (Figure 1). Volcano- ber of volcanic, as well as cold climate landforms, ice features located at the margin of a polar cap has were proposed as potential analogs for the field of great significance for astrobiology. Such interactions coniform features at the study site. Methods for the could provide potential shallow subsurface habitable analysis of these features were adapted from previous zones of liquid meltwater, as well as a mechanism for authors [1-4]. A brief overview of the analysis of the transporting a subsurface biota into near-surface envi- observed coniform features and comparisons with po- ronments via convecting hydrothermal systems. Such tential analog landforms follows. a biota, or prebiotic organic chemistry, could be sub- Rampart craters. Figure 2 compares MOLA pro- sequently cryopreserved in shallow polar ground ice files of two rampart craters present on the nearby formed as such systems cooled and died. In this study, northern plains of Mars near the study site, with a pro- a number of methods were employed to test the pseu- file of Meteor Crater (a small terrestrial impact crater), docrater hypothesis, including feature profiling (using and the knobby features at the study site.
    [Show full text]
  • Geologic Map of Medicine Lake Volcano, Northern California by Julie M
    Geologic Map of Medicine Lake Volcano, Northern California By Julie M. Donnelly-Nolan Pamphlet to accompany Scientific Investigations Map 2927 View of Medicine Lake volcano from northeast. Photo by Julie M. Donnelly-Nolan, 1978 2010 U.S. Department of the Interior U.S. Geological Survey This page intentionally left blank Contents Introduction............................................................................................................................................1 Geography and Access ..............................................................................................................1 Name of the Volcano ...................................................................................................................1 Methods.........................................................................................................................................2 Previous Geologic Work ......................................................................................................................2 Geologic and Tectonic Setting ............................................................................................................3 Pre-MLV Volcanic Activity...................................................................................................................4 Eruptive History of MLV .......................................................................................................................4 Eruptive Stage 1: Approximately 500 ka to 300 ka .................................................................6
    [Show full text]
  • Lava Building Blocks
    Lava Building Blocks Grade Level: 5-10 Overview Students investigate the influence of magma viscosity on the shape of a volcanic cone. Then, they explore the nature and motions of lava flows and learn about the Learner Objectives: importance of lava flows as the building Students will: blocks of Mount Rainier. ● Recognize the importance of lava flows in the construction of Mount Rainier. ● ● Recognize that at Mount Rainier lava Graphic “Photographs of Lava Flows at Mount Rainier” flows are visible as thick ridges that radiate from the volcano and as thin ● Graphic “Volcanic Rocks of Modern 1 ledges within the volcanic cone. Mount Rainier” ● Relate the general viscosity of lava flows For each student group: to a type of volcano: shield, cinder cone, or stratovolcano. ● Newspaper ● Make some generalized comparisons of ● Cardboard 1x1 meter (3x3 foot) lava flow behavior at Mount Rainier, ● One sample (small half-filled paper cup) Mount St. Helens, and Kilauea Volcano each of three household products (e.g., chocolate syrup, corn syrup, shampoo, Setting: Classroom oatmeal, jelly, ketchup, rubber cement, and a tube of toothpaste.) Timeframe: 40 minutes ● Specimens of lava rocks (optional) Lava on the Run -40 minutes ● Paper cups Materials: ● Pencil ● Lava on the Run Ruler ● Stopwatch ●“Lava on the Run” student page ● Measuring spoon ● Graphic “Three Types of Volcanic Cones” Vocabulary: Andesite, basaltic andesite, NATIONAL PARK SERVICE composite volcano, cinder cone, cone, crater, dacite, eruption, eruption column, glacier, lahar, landslides, lava, lava dome, lava flow, Living with a Volcano in Your Backyard- magma, magma chamber, pyroclastic flow, An Educator's Guide with Emphasis on rockfall, rock rubble, shield volcano, silica, Mount Rainier stratovolcano, vent, viscosity, volcano, volcanic gases Prepared in collaboration with the National Park Service U.S.
    [Show full text]
  • Volcanoes and Lava Flows
    What Are The Types of What Did Native Volcanoes? Americans See? Craters of the Moon has three kinds of volcanoes to “The area now known as Craters of the Moon see. Laidlaw Volcano and Pillar Butte are Shield is important to the Shoshone-Bannock because Volcanoes that form when liquid rock oozes and it represents both a place of sacred power and flows out of a central vent. Pilot Butte and Lava Butte an ancestral ground crossed during seasonal are Cinder Cone Volcanoes that formed when migrations. The lava rock was heated in our liquid rocks spatters and spits up from of a central sweat lodges and it was the rock that sent our vent. Big Southern Butte, like Oregon's Mount St. prayers up to the creator. In the landscape of Helens, is a Volcanic Dome which forms when liquid the lava flows, harmony was found.” rock is at hotter temperatures and can be expolsive. -Laverne Broncho, Shoshone-Bannock Tribal Member How Old Are The Lava Flows? Southern Idaho has 12 volcanic fields that range from 0.5 million years old near its eastern border with Yellowstone National Park to 15 million years old near its western border with Oregon. Craters of the Moon is part of a volcanic field in south-central Idaho that formed 11 million years ago. At Craters of the Moon, the most recent series of lava flowed from volcanoes as recent as 2,100 years ago. Learn more. Shoshone legend speaks of a serpent on a mountain who, angered by lightning, coiled around it and squeezed until liquid rock flowed, fire shot from cracks, and the mountain exploded.
    [Show full text]
  • Inbar Et Al., 2011, Holocene Cinder Cones... (Jody)
    Journal of Volcanology and Geothermal Research 201 (2011) 301–311 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Morphometric and morphological development of Holocene cinder cones: A field and remote sensing study in the Tolbachik volcanic field, Kamchatka Moshe Inbar a,⁎, Michael Gilichinsky b, Ivan Melekestsev c, Dmitry Melnikov c, Natasha Zaretskaya d a Department of Geography and Environmental Studies, University of Haifa, Israel b Department of Forest Resource Management, SLU, Umea, Sweden c Institute of Volcanology and Seismology, RAS, Petropavlovsk-Kamchatsky, Russia d Geological Institute, RAS, Moscow, Russia article info abstract Article history: The evolution of landscape over time is a central aspect of geological, paleogeographical and Received 14 January 2010 geomorphological studies. Volcanic features like cinder cones offer the opportunity to monitor the processes Accepted 18 July 2010 and development of the landscape. Cinder cones are perhaps the simplest and most common volcanic Available online 24 July 2010 landforms in the world. Morphological and morphometric study of cinder cones has proven an efficient tool for determining their relative dates, and the erosional processes affecting them. The extensive Kamchatka Keywords: volcanic province (Russian Far East), with its large Tolbachik cinder cone field, is an excellent case study for Kamchatka volcanic province fi Tolbachik eruption spatial and temporal classi cation and calibration of changes in morphometric values with time. cinder cones We show how the morphological and morphometric values of the monogenetic cinder cones, measured in morphometry the field and by digital elevation models, can be used to validate their age and erosional processes.
    [Show full text]
  • Using Google Earth to Study the Basic Characteristics of Volcanoes
    USING GOOGLE EARTH TO STUDY THE BASIC CHARACTERISTICS OF VOLCANOES by Stacia Schipper and Stephen Mattox 28 SCIENCE SCOPE USING GOOGLE EARTH TO STUDY THE BASIC CHARACTERISTICS OF VOLCANOES andforms, natural hazards, and the change canocams.html) provides links to numerous live in the Earth over time are common material webcams. in state and national standards. Volcanoes exemplify these standards and readily cap- Getting started with Google Earth Lture the interest and imagination of students. With a Google Earth is a program that allows you to explore minimum of training, students can recognize erupted the Earth in great detail. This virtual globe allows materials and types of volcanoes; in turn, students can you to visit any location on Earth and observe a 3-D relate these characteristics to eruption violence and view of Earth’s surface and gather other data. Google potential risk to both nearby and distant populations. Earth can be downloaded for free from http://earth. With the advent of Google Earth and the database of google.com . volcanoes supplied by the Smithsonian Institutions’ To allow students to be able to view the 3-D relief Global Volcanism of volcanoes, the “terrain” feature should be selected. Program (www.volcano.si.edu), students can de- This can be achieved by going to the “Layers” pull- scribe almost any volcano on Earth. Although about down menu and checking the box labeled “terrain.” 60 volcanoes erupt in an average year, there are 15 to To ensure that metric units of measurement are being 20 that have been continuously active for many years, used, go to the “Tools” tab and select “Options.” Click and will probably continue to erupt for decades.
    [Show full text]