Contextualizing the View Hill Scoria Cone, Akaroa Volcanic Complex
|
|
- Arleen Norton
- 5 years ago
- Views:
Transcription
1 Contextualizing the View Hill Scoria Cone, Akaroa Volcanic Complex Spencer Irvine 1, 2, Darren Gravely 2, Sam Hampton 2 1 Williams College, MA, USA, 2 University of Canterbury, NZ Abstract A recently discovered scoria cone located at View Hill, Banks Peninsula, New Zealand is well exposed on the side of a ridge. Analyses of these scoria deposits reveal eight different facies types based on grain size, clast percentage, average clast size, and degree of welding. These lithofacies have been mapped along with strike and dip measurements to locate the probable eruptive center. A schematic crosssection of the scoria cone was also drawn to demonstrate the cone s internal morphology. These diagrams indicate changing eruptive styles over the course of the cone s evolution and highlight complex relationships to the surrounding features. One of the features contacting the scoria cone includes overlying lava flows, which form a steep contact relationship. This indicates that the cone had already been completely formed by the time the lavas were deposited. The scoria cone is also contacted by dike intrusions, which likewise postdate the cone, though the origin of these deposits is unclear. As such, the View Hill scoria cone demonstrates that even in localized areas, multiple eruptive events took place in the Akaroa Volcanic Complex. Introduction A well-preserved scoria cone located at View Hill, Banks Peninsula, New Zealand records the eruptive history of Akaroa volcano. Last active 8 Ma, Akaroa volcano is primarily composed of basaltic lava flows and shallow intrusives, though it also consists of pyroclastic deposits such as the recently mapped scoria cone at View Hill. Though scoria cones have been identified and described on Akaroa volcano before (Johnston et al. 1997, Gorbey, D., Markey, E.), detailed analyses of Akaroa s volcanism and formation are limited. Previous studies have demonstrated that scoria cones are formed as a result of strombolian style eruptions, which are characterized by bursts of gas and coursegrained pyroclasts (Valentine et al. 2005). Scoria cones develop from strombolian eruptions over a series of four stages. In the first stage, a low-rimmed mantlebedded pyroclastic ring forms. During stage two, an exterior talus develops. Stage three begins with the destruction of the original rim by inward migration of the talus pile. In the final stage, the talus grows beyond the ballistic limit of ejecta
2 (McGetchin et al. 1974). Scoria cones are useful tools in analyzing eruptive history, as they record flank explosive activity away from the central conduit of the volcano. This study investigates the relationship between the View Hill scoria cone and the construction of Akaroa Volcanic Complex by examining the cone s development and morphology. By reconstructing the scoria cone, one can pinpoint the location of the vent and therefore the eruptive center. It also helps in understanding the relationship between the scoria cone and nearby lava flows. This will help explore the eruptive history of Akaroa and its formation. Geologic Setting Banks Peninsula, located on the east coast of New Zealand s South Island, consists of two late Miocene aged composite shield volcanoes. These volcanoes, Lyttelton and Akaroa, were last active Ma and Ma, respectively. The deposits from these volcanoes can be split into four volcanic groups: Lyttelton, Mt. Herbert, Akaroa, and Diamond Harbor. This study focuses on the deposits from the Akaroa volcanic group, which include the rocks erupted from the central and flank vents in eastern Banks Peninsula. Collectively, these comprise Akaroa volcano, a 1200 km 3 composite volcano of dominantly alkali lavas and shallow intrusives (Sewell 1988). The development of Akaroa volcano can be divided into an early phase and a main phase, corresponding to their timing in regards to the evolution of the volcano. The early phase consisted of early basaltic lava flows, the development of trachytic material in domes, and pyroclastic and epiclastic deposits. Comprising these deposits are scoria cones containing basaltic scoria and lava bombs, including the focus of this study. The main phase is characterized by more basalt and hawaiite lava flows with trachyte and basalt dikes intruding flows and pyroclastics (Dorsey 1988). View Hill, the field site for this study, consists of two ridges in northeastern Banks Peninsula and is located several kilometers inland of Little Akaroa. The ridges are composed of stacked lava flow sequences, pyroclastic deposits, basaltic dikes,
3 and trachytic lava domes. This study focuses on a previously unmapped scoria cone found on the western-most ridge of View Hill (figure 1). Methods Fieldwork involving mapping, data collection, and sample collection was conducted in February This research focused on scoria deposits, so features such as location of the deposits, color, grain size, structural measurements (strike and dip), clast measurements, and clast percentage were recorded. Photographs of the deposits were also taken and used to correlate different lithofacies across the field area. Using grain size, clast size, and clast percentage as parameters, the deposits were categorized into one of eight facies types based on those described by Johnston et al and refined with analyses of field observations. Using ArcMAP 10.2, the lithofacies were then mapped according to their observed locations and inferred extent. This geologic map of the scoria cone, while accounting for the lithofacies presumed proximity to the vent, was utilized along with strike and dip measurements to locate the potential eruptive center. A schematic cross-section of the scoria cone was constructed with CorelDRAW V6 to depict the cone s internal structure and highlight the shifting eruption styles that were involved in building it. The relationship between the scoria cone and the overlying lavas was examined using structural measurements (strike and dip) of contacts and Google Earth to infer their respective source locations. Results Fieldwork uncovered an extensive scoria cone on the northwestern ridge of View Hill. Much of the scoria cone has been eroded away, though compared to other scoria cones on Banks Peninsula it is quite well preserved. The scoria cone sharply contacts overlying basaltic lava flows on its eastern and southern flanks, and farther down the ridge to the northwest, the scoria is intruded by basaltic and trachyadesitic dikes.
4 Scoria Lithofacies Classification Analysis of field data revealed eight different facies types. These classifications were based on Johnston et al and modified using field observations to better describe the View Hill scoria cone. The defined lithofacies include ash bed, ash-rich scoria, intermediate scoria, non-flattened scoria, mixed scoria, clast-dominated scoria, loosely welded scoria, and densely welded scoria. To determine these deposit types, grain size, clast percentage, average clast size, and degree of welding were all considered. Each deposit type was then matched with the scoria outcrops observed in the field, and their field locations noted. These categories were then given a characteristic description based on recorded field observations of the deposits. The results of this classification are presented in table 1. Representative photographs of each deposit type are shown in figure 2. The deposits are listed in order from finer grain size, less clast-dominated, and smaller clast size to coarse grain size, more clast-dominated, and larger clast size. Scoria Cone Reconstruction Using the relative location of the different facies types, a geologic map of the scoria cone was constructed (figure 3). The map depicts the eight different scoria deposit types, the overlying lavas, and the dike intrusions. The field locations are marked in red and match those in table 1. Strike and dip measurements are mapped in locations where they were recorded. In areas where there is no field location, the extent of the deposits is inferred, assuming consistent thicknesses and factoring in a facies typical proximity to the vent. This understanding of scoria cone morphology was considered along with the strike and dip measurements to pinpoint the eruptive center of the scoria cone. For instance, welded scoria is typically more proximal to the vent, while ash-rich scoria is more distal, and beds tend to dip away from the vent source. The hypothesized vent location in the facies map represents the most likely area for eruptive activity. Based on the scoria facies map, a schematic cross-section of the scoria cone was constructed (figure 4). The units below the topography (represented by the solid black line) are drawn according to the contacts and thicknesses from the
5 geologic map of the scoria cone (figure 3). Those above the line are inferred, as they were not observed in the field. The units are mirrored across the proposed vent location as it is assumed that the eruptions produced symmetrical deposits. The cross section highlights the change in eruption styles from more strombolian to more hawiian over the course of the scoria cone s development. Google Earth image analyses indicate that the scoria cone rests on a large flat bench area, which likely represents the paleotopography that was present at the time the scoria cone formed. Measurements of the scoria cone from its base where it lies on the paleotopography to its top where it contacts the lava suggest that the cone is roughly 250 m tall. Meanwhile, the lateral extent of the scoria cone is estimated to be upwards of 1000 m based on the dip of the units and measurements of the scoria cone in Google Earth. These dimensions fit closely with those described by the equation, Hco = 0.18Wco where Hco is the height of the scoria cone and Wco is the width (Porter, 1972). Discussion The scoria facies at View Hill represent hawaiian and strombolian style eruptions, as indicated by the presence of welded and non-welded scoria facies, respectively. Hawaiian eruptions typically produce welded scoria, as they are less explosive and cause less magma fracturing. Conversely, strombolian eruptions will favor non-welded scoria. More violent eruptions will cause more fracturing and therefore create more ash-rich scoria, whereas less violent eruptions will produce blocks and bombs with lapilli matrices. These eruption styles and deposit types are characteristic of scoria cone development. The morphology of the View Hill scoria cone, including its dimensions and internal structure, are similarly very characteristic of scoria cones not only on Banks Peninsula, but also across the world. In the context of View Hill, the scoria cone has a clear relationship with the surrounding features, which is depicted in figure 5. Their relationship suggests that the hawaiian and strombolian eruptions that built the scoria cone occurred before those that created the overlying lava flows, as
6 evidenced by the nature of the contact between the two units (highlighted in red in figure 5). The dip of the contact between the ash bed and lava at location 10 is 21 to the east and near location 2 the dip of another contact between the scoria and lava is 35 to the east. Away from the scoria cone the lavas have only a gentle dip to the east. These values indicate that the scoria cone precluded the deposition of the lavas, as the scoria cone must have been present to affect the dip of the lava. Additionally, there is evidence of baking of the ash at the scoria-lava boundary at location 10 (figure 2A). The ash is thermally altered and appears reddish in color, and it is highly fractured and brittle. This phenomenon occurs when ash comes into contact with hot fluids, including lava, signifying that the ash and top layers of the scoria cone predated the lava flows. Intrusions discovered in the field area were found at location 6 (represented by bright yellow in figures 3, 4, and 5). Whereas the scoria deposits are of hawaiite composition, these intrusions consist of a basaltic dike and a trachy-andesitic dike occurring next to each and intruding through the scoria. As such, they likely represent a different eruptive event, distinct from the activity that formed the scoria cone. There is evidence that intrusions are indicative of later-stage activity, as they do not fall within the proposed vent zone and do not appear to follow the same conduit. Alternatively, it is possible that the vent source migrated during the construction of the cone, raising the potential for the intrusions to be directly related to the scoria cone. However, no current data collected in the field indicates this. Conclusion The View Hill scoria cone records shifting eruption styles on the flanks of Akaroa volcano, away from the central conduit. It also signifies eruptive activity that is distinct from the more characteristic lava-forming eruptions that created the ridges at View Hill. Even in localized areas such as View Hill, multiple eruptive events are represented, indicating that the Akaroa volcanic system had variable eruptive styles and was quite complex. Future work can be done to analyze the dike intrusions near the vent of the
7 scoria cone. This research focused primarily on the scoria cone at View Hill and did not have adequate time to decipher these features. Work can try to determine the timing of the dikes formation relative to each other, how far along the scoria cone s development they formed, and how they are related the scoria cone in terms of following the same conduit or representing later-stage intrusive events. Acknowledgements I would like to thank Patrick Thieringer and Eric Barefoot for their assistance and keenness while conducting fieldwork. I would also like to thank Frontiers Abroad for the amazing opportunity to study in New Zealand and my parents for supporting me in my adventure.
8 References Dorsey, C. J. (1988). The geology and geochemistry of Akaroa volcano, Banks Peninsula, New Zealand. Gorbey, D. (2014). Scoria Cone Analysis in Le Bons Bay, Banks Peninsula, New Zealand. Frontiers Abroad (University of Canterbury). Hampton, SJ, & Cole, JW. (2009). Lyttelton Volcano, Banks Peninsula, New Zealand: primary volcanic landforms and eruptive centre identification. Geomorphology, 104(3), Johnston, DM, Cole, JW, & Houghton, BF. (1997). Physical volcanology of Miocene basaltic pyroclastic deposits at Pigeon Bay: remnants of flank scoria cones of Akaroa volcano, Banks Peninsula, New Zealand. New Zealand journal of geology and geophysics, 40(1), Kereszturi, Gábor, & Németh, Károly. (2013). Monogenetic basaltic volcanoes: genetic classification, growth, geomorphology and degradation. Updates in volcanology new advances in understanding volcanic systems. InTech, Croatia, Markey, E. (2014). Uncovering Akaroa s Eruptive History: Reconstructing a flank scoria cone in Le Bons Bay, Banks Peninsula. Frontiers Abroad (University of Canterbury). McGetchin, Thomas R, Settle, Mark, & Chouet, Bernard A. (1974). Cinder cone growth modeled after northeast crater, Mount Etna, Sicily. Journal of Geophysical Research, 79(23), Patrick, Matthew R, Harris, Andrew JL, Ripepe, Maurizio, Dehn, Jonathan, Rothery, David A, & Calvari, Sonia. (2007). Strombolian explosive styles and source conditions: insights from thermal (FLIR) video. Bulletin of Volcanology, 69(7), Porter, Stephen C. (1972). Distribution, morphology, and size frequency of cinder cones on Mauna Kea volcano, Hawaii. Geological Society of America Bulletin, 83(12), Sewell, R. J. (1988). Late Miocene volcanic stratigraphy of central Banks Peninsula, Canterbury, New Zealand. New Zealand journal of geology and geophysics,
9 (1), Timm, Christian, Hoernle, Kaj, Van Den Bogaard, Paul, Bindeman, Ilya, & Weaver, Steve. (2009). Geochemical evolution of intraplate volcanism at Banks Peninsula, New Zealand: interaction between asthenospheric and lithospheric melts. Journal of Petrology, 50(6), Valentine, G. A., & Gregg, T. K. P. (2008). Continental basaltic volcanoes Processes and problems. Journal of Volcanology and Geothermal Research, 177(4), Valentine, G. A., Krier, D., Perry, F. V., & Heiken, G. (2005). Scoria cone construction mechanisms, Lathrop Wells volcano, southern Nevada, USA. Geology, 33(8),
10 Appendix Figure 1: Location map of the scoria cone relative to View Hill. Inset: The location of View Hill on Banks Peninsula, NZ.
11 262 Table 1: Table of scoria lithofacies classification. Name Description Code Field Location Ash Bed Unconsolidated, very fine grained red A.B. 10, 14 ash 5-12cm thick; occurs in sharp contact with overlying lava flows and grades into scoria below. Ash-rich scoria Brown to red ash matrix containing cm-scale dark gray to red vesicular A.R.S. 1, 13 Intermediate scoria Nonflattened scoria Mixed scoria Clastdominated scoria Loosely welded scoria Densely welded scoria clasts occuring at <20% Mixture of non-flattened clasts and bombs in a predominate orange to red ash matrix. Ash to clast ratio falled between that of A.R.S. and N.S. Clast supported deposits (>20%) of dark gray to red vesicular clasts and non-flattened bombs. The matrix is typically dark red ash to lapilli. Welding is not present. Both non-flattened and flatten clasts and bombs present in a red-orange ash to lapilli matrix. Clast dominated deposits containing non-flattened bombs occuring at >50% in a red-orange ash to lapilli matrix. Gray to black loosely welded, highly vesicular scoria with a knobly surface. Mm-scale clasts are visible. Black, welded scoria containing cmscale vesicular lenses and flattened cowpat bombs. I.S. 8, 11, 12 N.S. 1, 2, 5, 7 M.S. 4, C.D.S. 11, L.W.S. 15, D.W.S. 3, 4
12 Figure 2: Representative photographs of each scoria facies type and their corresponding field location. A) Ash bed (location 10); B) Ash-rich scoria (location 1); C) Intermediate scoria (location 12); D) Non-flattened scoria (location 1); E) Mixed scoria (location 4); F) Clast-dominated scoria (location 11); G) Loosely welded scoria (location 15); H) Densely welded scoria (location 3).
13 Figure 3: Scoria facies map based on the relative position of the deposit types observed in the field with field locations and structural measurements. The hypothesized vent location is circled in white A A Figure 4: Schematic cross-section of the scoria cone. The units and cross-section line correspond to those in figure 3. Units above the elevation profile (solid black line) are inferred and therefore faded.
14 Figure 5: Overview image of the scoria cone and overlying lavas to highlight their relationship. The contact between the scoria and lava is traced in red, and the other units are mapped according to figure 3.
Investigating Volcanic Reconstruction using Akaroa Lava Benches
Investigating Volcanic Reconstruction using Akaroa Lava Benches Jessie Bersson 1,2, Sam Hampton 1 1 University of Canterbury, Christchurch, New Zealand, Department of Geological Sciences 2 Whitman College,
More informationScoria Cone Dimensional Analysis and Intrusive Body. Interpretation at Pa Bay, Banks Peninsula, NZ
Scoria Cone Dimensional Analysis and Intrusive Body Interpretation at Pa Bay, Banks Peninsula, NZ Kelsey Brennan 1,2,3 1 Department of Geological Sciences, University of Canterbury, Christchurch, New Zealand
More informationA Geochemical Analysis of Akaroa Volcano Flank Eruptives
Zeller 1 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 A Geochemical Analysis of Akaroa Volcano Flank Eruptives Lucas R. Zeller 1, Samuel J. Hampton 2 1 Department
More informationPrentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 10 Volcanoes and Other Igneous Activity 10.1 The Nature of Volcanic Eruptions Factors Affecting Eruptions Factors that determine the violence of an eruption
More informationLessons Rising from the Ash: A Geochemical Study of the Ash Layers from
1 2 Lessons Rising from the Ash: A Geochemical Study of the Ash Layers from Akaroa Volcano, New Zealand 3 4 5 6 7 Sophia Tsang 1,2 1 Department of Geological Sciences, Brown University, Providence, Rhode
More informationGeosite investigations: A framework for deciphering geological histories; an example from
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 Geosite investigations: A framework for deciphering geological histories; an example from
More informationA bowl shaped depression formed by the collapse of a volcano is called a. Magma that has left the vent of a volcano is known as. Lava.
Magma that has left the vent of a volcano is known as Lava A bowl shaped depression formed by the collapse of a volcano is called a Caldera This can form in a caldera when magma starts to come back up
More informationFoundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa
Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa Fires Within: Igneous Activity Foundations, 6e - Chapter 7 Stan Hatfield Southwestern Illinois College The nature of volcanic eruptions Characteristics
More informationAkaroa Volcano as a volcanic complex and the Daly Gap
Gerrits 1 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 Akaroa Volcano as a volcanic complex and the Daly Gap Anna Gerrits 1, 2 1 Department of Geological Sciences, University
More informationVolcanic Geology of Le Bons Bay Peak, Banks Peninsula, New Zealand Tyler Stetson Brown University of Canterbury
Volcanic Geology of Le Bons Bay Peak, Banks Peninsula, New Zealand Tyler Stetson Brown University of Canterbury Bank s Peninsula not only has an intimate relationship with Christchurch, it has a fascinating
More informationRemote Sensing Geomorphology of Akaroa Volcano and Detailed Mapping of Okains Bay, Banks Peninsula, NZ
Remote Sensing Geomorphology of Akaroa Volcano and Detailed Mapping of Okains Bay, Banks Peninsula, NZ Daniel J. Hobbs 1,2 1. Department of Geological Sciences, University of Canterbury, Christchurch,
More informationGEOLOGY MEDIA SUITE Chapter 12
UNDERSTANDING EARTH, SIXTH EDITION GROTZINGER JORDAN GEOLOGY MEDIA SUITE Chapter 12 Volcanoes 2010 W.H. Freeman and Company Plate tectonics explains the global pattern of volcanism. Key Figure 12.20 (page
More informationFlows, Deposits, and Overlaps: Analysis and Description of the Flows of Eastern Okains Bay May 23, 2013
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 Flows, Deposits, and Overlaps: Analysis and Description of the Flows of Eastern Okains Bay May 23, 2013 Sarah
More information! Profile of Mauna Loa in Hawaii. Mauna Loa is one of five huge shield volcanoes that make up the island of Hawaii.
- Shield Volcanoes - Low, rounded profiles; slope angles 2-10 ; composed of numerous flows of mafic composition and little explosive activity - Largest of all volcanoes! Shield volcanoes consist of numerous
More informationThe Nature of Igneous Rocks
The Nature of Igneous Rocks Form from Magma Hot, partially molten mixture of solid liquid and gas Mineral crystals form in the magma making a crystal slush Gases - H 2 O, CO 2, etc. - are dissolved in
More informationVolcanology. The study of volcanoes
Volcanology The study of volcanoes Magma forms wherever temperature and pressure are high enough to melt rock. Some magma forms at the aesthenosphere Magma also forms at plate boundaries, where intense
More informationFlow Emplacement Mechanisms of a Morphologically Complex Lava Flow Abstract 1. Introduction
Flow Emplacement Mechanisms of a Morphologically Complex Lava Flow Jenna K. Rolle Frontiers Abroad Geology, University of Canterbury, Whitman College Fall 2014 Abstract Geomorphological, geochemical and
More informationCharacterizing Volcanic Features in Banks Peninsula, New Zealand Hannah Walcek 1, 2 and Sam Hampton 1
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 Characterizing Volcanic Features in Banks Peninsula, New Zealand Hannah Walcek 1, 2 and Sam Hampton 1 1 Department of
More informationStudy guide chapter 9
Study guide chapter 9 1. What are the three ways solid mantle material can change phase to a liquid? Associate a boundary/hot spot to each way mantle material changes phase. 1. A decrease in pressure which
More informationGEOL1 Physical Geology Laboratory Manual College of the Redwoods Lesson Five: Volcanoes Background Reading: Volcanoes Volcanic Terms: Silca:
Name: Date: GEOL1 Physical Geology Laboratory Manual College of the Redwoods Lesson Five: Volcanoes Background Reading: Volcanoes Volcanic Terms: Silca: SiO 2 silicon dioxide. This is quartz when it crystallizes.
More informationVisualizing Earth Science. Chapter Overview. Volcanoes and Eruption Types. By Z. Merali and B. F. Skinner. Chapter 9 Volcanism and Other
Visualizing Earth Science By Z. Merali and B. F. Skinner Chapter 9 Volcanism and Other Igneous Processes Volcanoes types and effects of eruption Chapter Overview Melting and cooling of rocks Geological
More informationA Volcano is An opening in Earth s crust through
Volcanoes A Volcano is An opening in Earth s crust through which molten rock, gases, and ash erupt. Also, the landform that develops around this opening. Kinds of Eruptions Geologists classify volcanic
More informationGoal 2.1 Forces in the Lithosphere. Volcanic Activity
Goal 2.1 Forces in the Lithosphere Volcanic Activity Lesson 3 Volcanoes, Part 1 Think About It What happens when you shake a can of soda and then open it? Focus Question How does the composition of magma
More informationNew Mexico Geological Society
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/64 Processes during scoria-cone collapse as recorded by displacement of crater-rim blocks, Strawberry Crater,
More informationVolcano - A Volcano is an opening in the Earth s surface through which molten material or volcanic gases are erupted.
What is a Volcano? Volcano - A Volcano is an opening in the Earth s surface through which molten material or volcanic gases are erupted. A volcano can either be a classic volcanic cone.. Mt. St. Helens,
More informationChapter 7: Volcanoes 8/18/2014. Section 1 (Volcanoes and Plate Tectonics) 8 th Grade. Ring of Fire
Section 1 (Volcanoes and Plate Tectonics) Chapter 7: Volcanoes 8 th Grade Ring of Fire a major belt of es that rims the Pacific Ocean Volcanic belts form along the boundaries of Earth s plates as they
More informationV o l c a n o es. Part I Composition. Types of deposits. Types of volcanoes Distribution
V o l c a n o es Part I Composition Types of deposits Types of volcanoes Distribution Volcano: A mound of material that is extruded to the Earth s surface from a vent that is connected to a magma chamber
More informationMagmatic dynamics and petrogenesis of eruptive deposits and a shallow intrusive, Pa Bay, Akaroa Volcano, New Zealand
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 Magmatic dynamics and petrogenesis of eruptive deposits and a shallow intrusive, Pa Bay, Akaroa
More informationMagma. Objectives. Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Vocabulary.
Magma Objectives Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Vocabulary viscosity Magma Magma The ash that spews from some volcanoes can form
More informationObjectives: Describe how volcanoes can affect people. Describe conditions that cause volcanoes. Describe the relationship between volcanoes and Earth
Objectives: Describe how volcanoes can affect people. Describe conditions that cause volcanoes. Describe the relationship between volcanoes and Earth s moving plates. Inside of Old Smokey, All covered
More informationEngineering Geology ECIV 2204
Engineering Geology ECIV 2204 2017-2016 Chapter (4) Volcanoes Chapter 4: Volcanoes and Other Igneous Activity cataclysmic relating to or denoting a violent natural even Eventually the entire
More informationImagine the first rock and the cycles that it has been through.
A rock is a naturally formed, consolidated material usually composed of grains of one or more minerals The rock cycle shows how one type of rocky material gets transformed into another The Rock Cycle Representation
More informationOverview of Ch. 4. I. The nature of volcanic eruptions 9/19/2011. Volcanoes and Other Igneous Activity Chapter 4 or 5
Overview of Ch. 4 Volcanoes and Other Igneous Activity Chapter 4 or 5 I. Nature of Volcanic Eruptions II. Materials Extruded from a Volcano III.Types of Volcanoes IV.Volcanic Landforms V. Plutonic (intrusive)
More informationEffects of Eruptions. Most active in the world Kilauea, Hawaii.
Inside of Old Smokey, All covered with snow, Lurk tons of hot magma, Getting ready to blow, Objectives: From deep in the chamber, Describe how volcanoes can affect people. Up a vent to the top, Describe
More informationMagma vs. Lava. Molten rock below Earth s surface is called magma. The magma that reaches the surface and erupts out of a volcano is called lava.
CH. 10.1 Be able to Explain the factors that determine the type of volcanic eruption. List the 3 types of volcanoes Describe the features of a volcano. What is a Volcano? Volcanoes are sites where molten
More information1/31/2013 BASALTIC BASALTIC ANDESITIC RHYOLITIC
Can you predict the location of volcanoes? What is causing this eruption? What factors influence its character? A volcano is any landform from which lava, gas, or ashes, escape from underground or have
More informationMultiple Choice Identify the letter of the choice that best completes the statement or answers the question.
volcano sample test Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. Volcanic belts form along a. islands in the Pacific Ocean. b. North American
More informationMagma. Objectives. Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Vocabulary.
Magma Objectives Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Vocabulary viscosity Magma Magma The ash that spews from some volcanoes can form
More informationIntroduction to Earth s s Spheres The Benchmark
Introduction to Earth s s Spheres The Benchmark Volcanism Volcanic eruptions Effusive: lavas (e.g., Kilauea) Volcanism Volcanic eruptions Explosive: pyroclastic rocks (e.g., Krakatau) Factors Governing
More informationVolcano. Magma. Lava. weak spot in crust where magma and gases come up. molten mixture of rockforming
Volcanoes Volcano weak spot in crust where magma and gases come up Magma Lava molten mixture of rockforming substance, gases, water from the mantle Magma that flows onto earth surface forms solid rock
More informationSection 10.1 The Nature of Volcanic Eruptions This section discusses volcanic eruptions, types of volcanoes, and other volcanic landforms.
Chapter 10 Section 10.1 The Nature of Volcanic Eruptions This section discusses volcanic eruptions, types of volcanoes, and other volcanic landforms. Reading Strategy Previewing Before you read the section,
More informationEarth has more than 600 active volcanoes. An active volcano is one that has erupted within recorded history.
Volcanoes A volcano is an opening in Earth s surface that erupts gases, ash, and lava. These materials pile up in layers around the opening, forming volcanic mountains. Earth has more than 600 active volcanoes.
More informationGEOLOGY OF THE DO27 PIPE: A PYROCLASTIC KIMBERLITE IN THE LAC DE GRAS PROVINCE, NWT, CANADA
GEOLOGY OF THE DO27 PIPE: A PYROCLASTIC KIMBERLITE IN THE LAC DE GRAS PROVINCE, NWT, CANADA Margaret Harder 1, Casey Hetman 2, Barbara Scott Smith 3, and Jennifer Pell 1 1 Peregrine Diamonds Ltd. 2 Mineral
More informationDirected Reading. Section: Volcanoes and Plate Tectonics
Skills Worksheet Directed Reading Section: Volcanoes and Plate Tectonics 1. Some volcanic eruptions can be more powerful than a(n) a. hand grenade. b. earthquake. c. geyser. d. atomic bomb. 2. The cause
More informationPart A GEOLOGY 12 CHAPTER 4 WORKSHEET VOLCANOES. Name
GEOLOGY 12 CHAPTER 4 WORKSHEET VOLCANOES Name Part A 1. The rough, jumbled blocky or jagged surface of a lava flow is called a. pahoehoe b. lahar c. aa d. phreatic 2. The Cascade volcanoes like Mt. St.
More informationGeophysical surveys Anomaly maps 2D modeling Discussion Conclusion
Introduction Geophysical surveys Anomaly maps 2D modeling Discussion Conclusion General context Growth of volcanic domes is a multiphase process: extrusion phases 2005 lava dome growth inside the Mount
More informationOIKOS > volcano > mechanism >types of volcanoes
Main Types of Volcanoes Volcanologists have classified volcanoes into groups based on the shape of the volcano, the materials they are built of, and the way the volcano erupts. The main one can be described
More informationUGRC 144 Science and Technology in Our Lives/Geohazards
UGRC 144 Science and Technology in Our Lives/Geohazards Session 5 Magma and Volcanism Lecturer: Dr. Patrick Asamoah Sakyi Department of Earth Science, UG Contact Information: pasakyi@ug.edu.gh College
More information3/24/2016. Geology 12 Mr. M. Gauthier 24 March 2016
Geology 12 Mr. M. Gauthier 24 March 2016 Introduction: Mt. St. Helens Before 1980 Mt. St Helens, in Southern Washington State, had not erupted since 1857 On March 27,1980 minor ashand eruptions were due
More informationWhen Mount St. Helens erupted, trapped gases caused the north side of the mountain to explode. Volcanic ash was ejected high into the atmosphere.
When Mount St. Helens erupted, trapped gases caused the north side of the mountain to explode. Volcanic ash was ejected high into the atmosphere. A volcano is a mountain that forms when magma reaches the
More informationIgneous and Metamorphic Rock Forming Minerals. Department of Geology Mr. Victor Tibane SGM 210_2013
Igneous and Metamorphic Rock Forming Minerals Department of Geology Mr. Victor Tibane 1 SGM 210_2013 Intrusive and Effusive Rocks Effusive rocks: rapid cooling small crystalls or glas Lava & ash Magmatic
More informationFOUNDATIONS OF GEOLOGY CHAPTER 2
FOUNDATIONS OF GEOLOGY CHAPTER 2 2.3A- VOLCANOES Volcanoes all share common characteristics. Vent- a central channel through which gases, ash and rock are ejected. Magma- molten rock which lies several
More informationYour web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore
Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore VO L CANIC CO NE For the complete encyclopedic entry with media resources,
More informationChapter 18. Volcanism
Chapter 18 Volcanism Ring of fire contains 66% of world s active volcanoes Convergent : Divergent: Icelandic Eruption Mount Etna Different Kinds of eruptions: Volcanic activity is controlled by plate tectonics,
More informationHawaiian Submarine Volcanism. Stages of Hawaiian Volcanoes:
Hawaiian Submarine Volcanism November 1, 2011 Mary Tardona GG 711 Stages of Hawaiian Volcanoes: Typically, three main stages: Pre shield Shield Post shield Sometimes followed by: Rejuvenation Stage GG
More informationWHAT IS A MAGMA. Magma is a mixture of molten rock, volatiles and solids that is found beneath the surface of the Earth.
UNIT - 8 VOLCANOES WHAT IS A MAGMA Magma is a mixture of molten rock, volatiles and solids that is found beneath the surface of the Earth. In some instances, it solidifies within the crust to form plutonic
More informationChapter 18 - Volcanic Activity. Aka Volcano Under the City
Chapter 18 - Volcanic Activity Aka Volcano Under the City 18.1 Magma Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Temperature and pressure increase
More information3.2 Notes: Volcanoes Form as Molten Rock Erupts
3.2 Notes: Volcanoes Form as Molten Rock Erupts Think about What happens when a volcano erupts? Volcanoes erupt many types of material Earth s thin outer layer is, but most of Earth is extremely hot rock
More informationChapter 10: Volcanoes and Other Igneous Activity Section 1: The Nature of Volcanic Eruptions I. Factors Affecting Eruptions Group # Main Idea:
Chapter 10: Volcanoes and Other Igneous Activity Section 1: The Nature of Volcanic Eruptions I. Factors Affecting Eruptions Group # A. Viscosity Group # B. Dissolved Gases Group # II. Volcanic Material
More informationTypes of Volcanoes. Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries.
Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries. Volcanoes How do volcanoes work? How do volcanoes work? Magma is forced onto Earth s surface.
More informationGet Ready for an ERUPTION!!!
Get Ready for an ERUPTION!!! Three Types of Volcanos Shield Cinder Cone Composite Shield Volcano Created by hot spots Gently sloping Cinder Volcano Steep Cone-shaped hill/ mountain Composite Volcano Tall,
More information1 Types of Volcanoes CHAPTER. Chapter 1. Types of Volcanoes
CHAPTER 1 Types of Volcanoes Describe the magma compositions and characteristics of different types of volcanoes. What does an active volcano look like? Climbing up Mount St. Helens and looking into the
More informationIgneous Rocks. Magma molten rock material consisting of liquid rock and crystals. A variety exists, but here are the end members:
Igneous Rocks Magma molten rock material consisting of liquid rock and crystals. A variety exists, but here are the end members: Types of Magma Basaltic, Basic or Mafic very hot (900-1200 C) very fluid
More information12.2 Volcanoes Looking inside a volcano What is a volcano? volcano magma magma chamber lava
12.2 Volcanoes Early explorers noticed that many volcanoes were located near coastlines, but they didn t know why. One volcano that is near a coastline is Mount St. Helens in Washington state. This famous
More informationIntroduction to volcanoes. Volcano: an opening in the earth s surface through which lava, hot gases, and rock fragments erupt
Introduction to volcanoes Volcano: an opening in the earth s surface through which lava, hot gases, and rock fragments erupt Origin of Volcanoes 1. Magma 50-100 miles below the earth s surface slowly begins
More informationTypes of Volcanoes KEY CONCEPT: TECTONIC PLATE MOTIONS CAN RESULT IN VOLCANIC ACTIVITY AT PLATE BOUNDARIES.
Types of Volcanoes KEY CONCEPT: TECTONIC PLATE MOTIONS CAN RESULT IN VOLCANIC ACTIVITY AT PLATE BOUNDARIES. Volcanoes How do volcanoes work? How do volcanoes work? Magma is forced onto Earth s surface.
More informationVolcano an opening in Earth s crust through which molten rock, gases, and ash erupt and the landform that develops around this opening.
Chapter 9 Volcano an opening in Earth s crust through which molten rock, gases, and ash erupt and the landform that develops around this opening. 3 Conditions Allow Magma to Form: Decrease in pressure
More informationPhysical Geology, 15/e
Lecture Outlines Physical Geology, 15/e Plummer, Carlson & Hammersley Copyright McGraw-Hill Education, Inc. Permission required for reproduction or display. Volcanism and Extrusive Rocks Physical Geology
More informationVolcanoes. Volcanic eruptions can be more powerful than the explosion of an atomic bomb.
Ch. 13 Volcanoes Volcanoes Volcanic eruptions can be more powerful than the explosion of an atomic bomb. Many of these eruptions are caused by the movement of tectonic plates. Volcanism Volcanism-any activity
More informationChapter Twelve: Earthquakes
The Changing Earth Chapter Twelve: Earthquakes 12.1 Earthquakes 12.2 Volcanoes Investigation 12B Volcanoes How are volcanoes and plate boundaries related? 12.2 Looking inside a volcano A volcano is where
More informationGEOL 10: Environmental Geology Activity 9: Topographic Maps and Mt. St. Helens. Name: Date:
GEOL 10: Environmental Geology Activity 9: Topographic Maps and Mt. St. Helens Name: Date: A topographic map is a two dimensional (flat) representation (model) of a three dimensional land surface (landscape).
More informationCritical Thinking 1. Contrast How could you tell the difference between a mafic rock and a felsic rock by looking at them?
CHAPTER 13 2 SECTION Volcanoes Volcanic Eruptions KEY IDEAS As you read this section, keep these questions in mind: How does the composition of magma affect volcanic eruptions and lava flow? What are the
More informationVolcanoes. Presented by Kesler Science
Presented by Kesler Science Essential Questions: 1. What are the parts of a volcano? 2. What are the four types? 3. What processes form volcanoes? 4. Where are volcanoes located on earth? What is a Volcano?
More informationChapter 7 Lecture Outline. Volcanoes and Other Igneous Activity
Chapter 7 Lecture Outline Volcanoes and Other Igneous Activity Mount St. Helens eruption (May 18,1980) Largest historic eruption in North America Lowered peak by more than 400 m Destroyed all trees in
More informationEPS 50 Lab 2: Igneous Rocks Grotzinger and Jordan, Chapter 4
Name: EPS 50 Lab 2: Igneous Rocks Grotzinger and Jordan, Chapter 4 Introduction In the previous lab, we learned about mineral characteristics, properties and identities as well as the three basic rock
More informationVulcanicity. Objectives to identify the basic structure of volcanoes and understand how they form.
Vulcanicity Objectives to identify the basic structure of volcanoes and understand how they form. Some key terms to start.. Viscosity how well a substance (lava) flows. Acid lavas have a high viscosity,
More informationUnit 4 Lesson 4 Volcanoes. Copyright Houghton Mifflin Harcourt Publishing Company
Magma Magic What is a volcano? A volcano is any place where gas, ash, or melted rock come out of the ground. Many volcanoes are dormant, meaning an eruption has not occurred in a long period of time. What
More informationFire and Ice. Overview. Grade Level 6 8. Students will be able to: Objectives
Fire and Ice Overview Students use a power point presentation to compare and contrast the geologic history and environment of Mount Rainier and Mount Fuji, the Sister Mountains. Grade Level 6 8 Students
More informationA Missing Piece of the Puzzle: Geochemical Analysis of the Lava Flows Within Stony Bay, Banks Peninsula, NZ. Lauren Pincus 1,2
1 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 A Missing Piece of the Puzzle: Geochemical Analysis of the Lava Flows Within Stony Bay, Banks Peninsula, NZ
More informationChapter 7 Lecture Outline. Volcanoes and Other Igneous Activity
Chapter 7 Lecture Outline Volcanoes and Other Igneous Activity Focus Question 7.1 How were the eruptions of Mount St. Helens and Hawaii s Kilauea volcano different? Mount St. Helens eruption (May 18,1980)
More informationGeology of the Hawaiian Islands
Geology of the Hawaiian Islands Class 4 22 January 2004 Turn in Homework #1 Any Questions? IMPORTANT Big Island Field Trip We need a $162 payment for airfare BEFORE January 29 th Description of logistics,
More informationGet Ready for an ERUPTION!!! VOLCANOES
Get Ready for an ERUPTION!!! VOLCANOES VOLCANOS Three Types of Volcanos Shield Cinder Cone Composite LAND FORMATIONS FROM LAVA & ASH Shield Volcano Created by hot spots Gently sloping Cinder Volcano Steep
More informationBellringer: What materials are ejected from volcanoes? Quote of the Day: "Science is not belief, but the will to find out.
Bellringer: What materials are ejected from volcanoes? Quote of the Day: "Science is not belief, but the will to find out." ~Anonymous Sep 26 10:30 AM 1 Copy Directly into your notebook... 1. Pyro Latin
More informationPyroclastic Deposits I: Pyroclastic Fall Deposits
Pyroclastic Deposits I: Pyroclastic Fall Deposits EAS 458 Volcanology Introduction We have seen that physics is useful in understanding volcanic processes, but physical models must be constrained by and
More informationEssentials of Geology, 11e
Essentials of Geology, 11e Igneous Rocks and Intrusive Activity Chapter 3 Instructor Jennifer Barson Spokane Falls Community College Geology 101 Stanley Hatfield Southwestern Illinois College Characteristics
More informationStructural and Geochemical Characterization of a Trachy- Andesitic Cryptodome: View Hill, Banks Peninsula, New Zealand
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 Structural and Geochemical Characterization of a Trachy- Andesitic Cryptodome: View Hill, Banks
More informationVolcanism (Chapter 5)
GEOLOGY 306 Laboratory Instructor: TERRY J. BOROUGHS NAME: Volcanism (Chapter 5) For this assignment, you will require: a calculator, colored pencils, string, protractor, stereoscopes (provided). Objectives
More informationGeomorphology Final Exam Study Guide
Geomorphology Final Exam Study Guide Geologic Structures STRUCTURAL GEOLOGY concerned with shapes, arrangement, interrelationships of bedrock units & endogenic (within) forces that cause them. Tectonic
More informationUNIT SIX: Earth s Structure. Chapter 18 Earth s History and Rocks Chapter 19 Changing Earth Chapter 20 Earthquakes and Volcanoes
UNIT SIX: Earth s Structure Chapter 18 Earth s History and Rocks Chapter 19 Changing Earth Chapter 20 Earthquakes and Volcanoes Chapter Twenty: Earthquakes and Volcanoes 20.1 Earthquakes 20.2 Volcanoes
More informationWhat Do You See? Learning Outcomes Goals Learning Outcomes Think About It Identify classify In what kinds of environments do igneous rocks form?
Section 2 Igneous Rocks and the Geologic History of Your Community What Do You See? Learning Outcomes In this section, you will Goals Text Learning Outcomes In this section, you will Identify and classify
More informationFrontiers Abroad program has been relying on single hand samples to represent an entire
Lateral Geochemical Variation Within Banks Peninsula Lava Flows Drew Martzolf 1,2 1 Department of Geological Sciences, University of Canterbury, Christchurch, NZ 2 Department of Geology, Colby College,
More informationGEOLOGY 285: INTRO. PETROLOGY
Dr. Helen Lang Dept. of Geology & Geography West Virginia University SPRING 2015 GEOLOGY 285: INTRO. PETROLOGY The Cascade Volcanoes are a good example of the Circum- Pacific ring of fire of subductionrelated
More informationSocial Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE
Social Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE The Structure of the Earth To understand the forces that create Canada's physical landscape we must understand the structure
More informationLANDFORMS. Patterns and Processes
LANDFORMS Patterns and Processes Structure From the surface the Earth is a planet of continents and oceans. There is constant motion on the earth s surface. Seismology is the study of earthquakes. Scientists
More informationVolcanoes. Table of Contents Volcanoes and Plate Tectonics Volcanic Eruptions Volcanic Landforms
Volcanoes Table of Contents Volcanoes and Plate Tectonics Volcanic Eruptions Volcanic Landforms What is a volcano? cone Conduit Or Pipe vent Side vent Central vent Crater A volcano is a vent or 'chimney'
More informationIgneous Rocks. Igneous Rocks. Genetic Classification of
Igneous Rocks Fig. 5.1 Genetic Classification of Igneous Rocks Intrusive: crystallized from slowly cooling magma intruded within the Earth s crust; e.g. granite, gabbro 1 Fig. 5.2 Genetic Classification
More informationS3 IHE GE 2014/Chan ML
S3 IHE GE 2014/Chan ML Formation Types Advantages and Disadvantages of living near/in volcanic areas Introduction Volcano, mountain or hill formed by the accumulation of materials erupted through one or
More informationMEMO. TO: Dennis Lapoint CC: FROM: Eriaan Wirosono DATE: April, 20 th 2014 SUBJECT: Exploration activity report March-April 2014_EW
TO: Dennis Lapoint CC: FROM: Eriaan Wirosono DATE: April, 20 th 2014 SUBJECT: Exploration activity report March-April 2014_EW MEMO 1. Highlights and Productivity Overview pan sampling on target Areas 1
More informationPiles of Fire Individual and Team Project Modified from
Piles of Fire Individual and Team Project Modified from http://www.spacegrant.hawaii.edu/class_acts/pilesfirete.html The purpose of this activity is to investigate how particle size affects the angle of
More informationCalc-alkaline Volcanic Rocks. Calc-alkali Volcanics. Fabric. Petrography. Compositional Classification. Petrography. Processes.
Calc-alkaline Volcanic Rocks Calc-alkali Volcanics Winter Chapters 16 & 17 Petrography Processes Field relations Volcanic arcs Petrogenesis Petrography Fabric Classification Alteration Fabric Aphanitic
More information