Glaciers) - BISOT 2013
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Name These Glacial Features 1.) 1
Name these Glacial Features 1.) 1.)____________________________________ 2.) 2.) ___________________________________ 3.) 3.)_____________________________________ 4.) 4.) ____________________________________ Name these types of Glaciers 5.) 5.)___________________________________________ 6.) 6.) __________________________________________ 7.) 7.) __________________________________________ 8.) 8.) __________________________________________ True or False 9.) __________ The terminus marks the farthest extent of a glacier. 10.) _________ An arête is a bow or amphitheater shape in a glacier. 11.) _________CO2 levels are higher during glacial episodes. 12.) _________ Methane Hydrate breaks down into H20. 13.) _________ Glaciers exist on every continent. 14.) _________ The Great Lakes were created by glaciation. 15.) _________ Calving is a process that creates icebergs. 16.) ________ Glacier National Park is in Alaska 17.) ________ Alaska has 100 glaciers. 18.) ________ 75% of the world’s glaciers are retreating. 19.) ________ A glacier can move forward and retreat at the same time. 20.) ________ Ogives are alternating wave crests and valleys that appear as dark and light bands of ice on glacier surfaces. 21.) ________ A drumlin field east of Rochester, New York is estimated to contain about 100 drumlins. Short Answer 22.) Give a general definition of the milankovitch cycles. _________________________________________________________________________________ _________________________________________________________________________________ _________________________________________________________________________________ -
1 Recognising Glacial Features. Examine the Illustrations of Glacial Landforms That Are Shown on This Page and on the Next Page
1 Recognising glacial features. Examine the illustrations of glacial landforms that are shown on this C page and on the next page. In Column 1 of the grid provided write the names of the glacial D features that are labelled A–L. In Column 2 indicate whether B each feature is formed by glacial erosion of by glacial deposition. A In Column 3 indicate whether G each feature is more likely to be found in an upland or in a lowland area. E F 1 H K J 2 I 24 Chapter 6 L direction of boulder clay ice flow 3 Column 1 Column 2 Column 3 A Arête Erosion Upland B Tarn (cirque with tarn) Erosion Upland C Pyramidal peak Erosion Upland D Cirque Erosion Upland E Ribbon lake Erosion Upland F Glaciated valley Erosion Upland G Hanging valley Erosion Upland H Lateral moraine Deposition Lowland (upland also accepted) I Frontal moraine Deposition Lowland (upland also accepted) J Medial moraine Deposition Lowland (upland also accepted) K Fjord Erosion Upland L Drumlin Deposition Lowland 2 In the boxes provided, match each letter in Column X with the number of its pair in Column Y. One pair has been completed for you. COLUMN X COLUMN Y A Corrie 1 Narrow ridge between two corries A 4 B Arête 2 Glaciated valley overhanging main valley B 1 C Fjord 3 Hollow on valley floor scooped out by ice C 5 D Hanging valley 4 Steep-sided hollow sometimes containing a lake D 2 E Ribbon lake 5 Glaciated valley drowned by rising sea levels E 3 25 New Complete Geography Skills Book 3 (a) Landform of glacial erosion Name one feature of glacial erosion and with the aid of a diagram explain how it was formed. -
EVIDENCE of POSSIBLE GLACIAL FEATURES on TITAN. L. E. Robshaw1, J
Lunar and Planetary Science XXXIX (2008) 2087.pdf EVIDENCE OF POSSIBLE GLACIAL FEATURES ON TITAN. L. E. Robshaw1, J. S. Kargel2, R. M. C. Lopes3, K. L. Mitchell3, L. Wilson1 and the Cassini RADAR team, 1Lancaster University, Environmental Sci. Dept., Lancaster, UK, 2Dept. of Hydrology and Water Resources, University of Arizona, 3Jet Propulsion Laboratory, Pasa- dena, CA 91109. Introduction: It has been suggested previously Figure 1 shows coastline that has at least superficial [e.g. 1] that solid hydrocarbons might condense in Ti- similarities with the coast of Norway and other fjord tan’s atmosphere, snow down onto the surface and areas. There are many, roughly parallel, steep-sided form glacier-like features, but no strong evidence has valleys, often with rounded heads. Most are approxi- been obtained. The high northern latitudes imaged in mately the same size as the valleys on the Norwegian the SAR swath obtained during Cassini’s T25 fly-by off-shore islands. (figure 1, top), however, exhibit morphological simi- There also appears to be some similarity between larities with glacial landscapes on the Earth, particu- the areas that arrows b & c point to (fig. 1, area shown larly the coast of Norway (figure 1, bottom). Several also in close-up in fig. 2, top) and the islands of the areas exhibit fjord-like valleys, with possible terminal Outer Lands (Fig. 2, bottom), a terminal moraine ar- moraine archipelagos, and further inland are dry val- chipelagic region off the southern coast of New Eng- leys, reminiscent of glacial scouring. Other noted fea- land. tures may be a ribbon lake and an Arête, both the result of glacial erosion. -
Glacial Processes and Landforms
Glacial Processes and Landforms I. INTRODUCTION A. Definitions 1. Glacier- a thick mass of flowing/moving ice a. glaciers originate on land from the compaction and recrystallization of snow, thus are generated in areas favored by a climate in which seasonal snow accumulation is greater than seasonal melting (1) polar regions (2) high altitude/mountainous regions 2. Snowfield- a region that displays a net annual accumulation of snow a. snowline- imaginary line defining the limits of snow accumulation in a snowfield. (1) above which continuous, positive snow cover 3. Water balance- in general the hydrologic cycle involves water evaporated from sea, carried to land, precipitation, water carried back to sea via rivers and underground a. water becomes locked up or frozen in glaciers, thus temporarily removed from the hydrologic cycle (1) thus in times of great accumulation of glacial ice, sea level would tend to be lower than in times of no glacial ice. II. FORMATION OF GLACIAL ICE A. Process: Formation of glacial ice: snow crystallizes from atmospheric moisture, accumulates on surface of earth. As snow is accumulated, snow crystals become compacted > in density, with air forced out of pack. 1. Snow accumulates seasonally: delicate frozen crystal structure a. Low density: ~0.1 gm/cu. cm b. Transformation: snow compaction, pressure solution of flakes, percolation of meltwater c. Freezing and recrystallization > density 2. Firn- compacted snow with D = 0.5D water a. With further compaction, D >, firn ---------ice. b. Crystal fabrics oriented and aligned under weight of compaction 3. Ice: compacted firn with density approaching 1 gm/cu. cm a. -
Hiking Trails
0a3 trail 0d4 trail 0d5 trail 0rdtr1 trail 14 mile connector trail 1906 trail 1a1 trail 1a2 trail 1a3 trail 1b1 trail 1c1 trail 1c2 trail 1c4 trail 1c5 trail 1f1 trail 1f2 trail 1g2 trail 1g3 trail 1g4 trail 1g5 trail 1r1 trail 1r2 trail 1r3 trail 1y1 trail 1y2 trail 1y4 trail 1y5 trail 1y7 trail 1y8 trail 1y9 trail 20 odd peak trail 201 alternate trail 25 mile creek trail 2b1 trail 2c1 trail 2c3 trail 2h1 trail 2h2 trail 2h4 trail 2h5 trail 2h6 trail 2h7 trail 2h8 trail 2h9 trail 2s1 trail 2s2 trail 2s3 trail 2s4 trail 2s6 trail 3c2 trail 3c3 trail 3c4 trail 3f1 trail 3f2 trail 3l1 trail 3l2 trail 3l3 trail 3l4 trail 3l6 trail 3l7 trail 3l9 trail 3m1 trail 3m2 trail 3m4 trail 3m5 trail 3m6 trail 3m7 trail 3p1 trail 3p2 trail 3p3 trail 3p4 trail 3p5 trail 3t1 trail 3t2 trail 3t3 trail 3u1 trail 3u2 trail 3u3 trail 3u4 trail 46 creek trail 4b4 trail 4c1 trail 4d1 trail 4d2 trail 4d3 trail 4e1 trail 4e2 trail 4e3 trail 4e4 trail 4f1 trail 4g2 trail 4g3 trail 4g4 trail 4g5 trail 4g6 trail 4m2 trail 4p1 trail 4r1 trail 4w1 trail 4w2 trail 4w3 trail 5b1 trail 5b2 trail 5e1 trail 5e3 trail 5e4 trail 5e6 trail 5e7 trail 5e8 trail 5e9 trail 5l2 trail 6a2 trail 6a3 trail 6a4 trail 6b1 trail 6b2 trail 6b4 trail 6c1 trail 6c2 trail 6c3 trail 6d1 trail 6d3 trail 6d5 trail 6d6 trail 6d7 trail 6d8 trail 6m3 trail 6m4 trail 6m7 trail 6y2 trail 6y4 trail 6y5 trail 6y6 trail 7g1 trail 7g2 trail 8b1 trail 8b2 trail 8b3 trail 8b4 trail 8b5 trail 8c1 trail 8c2 trail 8c4 trail 8c5 trail 8c6 trail 8c9 trail 8d2 trail 8g1 trail 8h1 trail 8h2 trail 8h3 trail -
Geotechnical and Geologic Constraints on Tsunamigenic Submarine Landslides
GEOTECHNICAL AND GEOLOGIC CONSTRAINTS ON TSUNAMIGENIC SUBMARINE LANDSLIDES H.J. LEE U.S. Geological Survey, 345 Middlefield Road, Menlo Park, CA 94025 USA Abstract Modeling submarine-landslide-induced tsunamis requires many simplifications of the landslide process, although the real world is much more complicated. Clearly tsunami modelers cannot consider all facets, but there is value in being aware of the complications. This paper describes the many environments in which submarine landslides can occur and the triggers that typically initiate them. Earthquakes acting on continental or canyon slopes comprise probably the most common scenario but many other combinations of environments and triggers are possible. Surprisingly, many sediment-covered slopes in highly seismically active areas have not failed. A possible explanation for this phenomenon is a process called “seismic strengthening.” The existence of such a process reduces somewhat the risk of landslide tsunamis along active margins while maintaining the risk along passive margins. Once a trigger has initiated a landslide in one of the vulnerable environments, failed masses begin to move downslope. Depending upon initial density state, the masses may convert into fluid-like sediment flows or even more dilute turbidity currents. A model for quantifying the tendency to flow is provided. Finally, a case study of the landslides and landslide tsunamis that occurred in Port Valdez, Alaska, during the 1964 Great Alaska Earthquake is provided. The excellent data base, including before and after bathymetry, shows that both large rigid block motion and mobilized sediment flows can occur near each other during the same event. The intact blocks are more efficient in producing tsunamis but the sediment flow can move farther and can erode and entrain considerable bottom sediment as they progress across the seafloor. -
The Formation of Eskers
Proceedings of the Iowa Academy of Science Volume 21 Annual Issue Article 31 1914 The Formation of Eskers Arthur C. Trowbridge State University of Iowa Let us know how access to this document benefits ouy Copyright ©1914 Iowa Academy of Science, Inc. Follow this and additional works at: https://scholarworks.uni.edu/pias Recommended Citation Trowbridge, Arthur C. (1914) "The Formation of Eskers," Proceedings of the Iowa Academy of Science, 21(1), 211-218. Available at: https://scholarworks.uni.edu/pias/vol21/iss1/31 This Research is brought to you for free and open access by the Iowa Academy of Science at UNI ScholarWorks. It has been accepted for inclusion in Proceedings of the Iowa Academy of Science by an authorized editor of UNI ScholarWorks. For more information, please contact [email protected]. Trowbridge: The Formation of Eskers THE FORMATION OF ESKERS. 211 -· THE FORMATION OF ESKERS. .ARTHUR C. TROWBRIDGE. Ever since work has been in progress in glaciated regions, long, nar -row, winding, steep-sided, conspicuous ridges of gravel and sand have been recognized by geologists. They are best developed and were first recognized as distinct phases of drift in Sweden, where they are called Osar. The term Osar has the priority over other terms, but in this country, probably for phonic reasons, the Irish term Esker has come into use. With apologies to Sweden, Esker will be used in the present paper. Other terms which have been applied to these ridges in various parts of the world are serpent-kames, serpentine kames, horsebacks, whalebacks, hogbacks, ridges, windrows, turnpikes, back furrows, ridge • furrows, morriners, and Indian roads . -
Mass-Wasting, Classification and Damage in Ohio C
MASS-WASTING, CLASSIFICATION AND DAMAGE IN OHIO C. N. SAVAGE Department of Geography and Geology, Kent State University, Kent, Ohio The sudden and often spectacular free fall, slide, flow, creep or subsidence of earth materials may be costly in terms of human lives and property damage. Phenomena of this type, variously called "landslide, earthflow or subsidence" are assigned by geologists to gravity controlled movement or referred to collectively as "mass-wasting." This category also includes movement of dry or hard-frozen masses, or snow-laden debris when moved by gravity. Figure 1 illustrates some of these types of movement. This paper is intended to bring to the attention of laymen and professional men the importance and widespread occurrence of these destructive forces. A brief discussion of damage, origin, prevention and classification is presented, followed by examples in Ohio. It is hoped that the suggested classification will prove useful as an aid to the recognition of different types of mass-movement. Annually, many highways are blocked or destroyed, soils are ruined and buried in rubble, forest lands are ripped apart, and bridges, dams, buildings and other structures are wrecked or buried by landslides. Every year, especially in southern and eastern Ohio, many thousands of dollars are lost because of this type of calamity. There is scarcely a spring which does not bring reports of landslides in the local press. It seems obvious that this is a subject of grave concern to construction engineers, soils experts, conservation men and many others including the tax paying citizen. Wherever there are slopes that are steep enough, and wherever there is loose rock material, mass-wasting is a potential threat. -
Geotechnical Investigation and Geologic Landslide Hazard Assessment, Proposed Single-Family Residential Home Site, Tax Lot No
REDMOND GEOTECHNICAL SERVICES · Geotechnical Investigation and Geologic Landslide Hazard Assessment Proposed Single-Family Residential Home Site Tax Lot No. 300 4th Avenue and Ganong Street Oregon City (Clackamas County), Oregon for Iselin Architects Project No. 1477.003.G December 6, 2017 REDMOND .GEOT.ECHNICAL SERVICES January 6, 2017, Mr. Todd lselin lselin Architects ( 1307 Seventh Street I' Oregon City, Oregon 97045 Dear Mr. lselin: Re: Geotechnical Investigation and Geologic Landslide Hazard Assessment, Proposed Single-Family Residential Home Site, Tax Lot No. 300, 4th Avenue and Ganong Street, Oregon City (Clackamas County), Oregon . · ':,,, ''\ T ' ' Submitted herewith is our report entitled "Geotechnical Investigation and Geologic Landslide Hazard Assessment, Proposed Single-Family.Residential Home Site, Tax Lot No. 300, 4th Avenue and Ganong Street, Oregon City (Clackamas County), Oregon". The scope of our services was outlined in our formal proposal to Mr. Todd lselin dated October 24, 2016. Written authorization of our services was provided by Mr. Todd lselin on November 1, 2016. 1 During'the course of our investigation, we have kept you and/or,others advised of our schedule and preliminary finding~. We appreciate the oppori unity to assist you with this phase of the project . .. Should you have any questions regardlng'this report, please do not hesitate to call. : Sincerely, ,,, Daniel M. Redmond, P.E ., G.E. ;,."" ; '. President/Prim:ipal Engineer PO BQX 20547 • PORTL.AND, OREGON 9729~ • FAX 503/286-7176 • PHONE 503/285-0598 TABLE OF CONTENTS . ' j Page No. INTRODUCTION 1 PROJECT DESCRIPTION 1 SCOPE OF WORK 2 SITE CONDITIONS 3 Site Geology 3 Surface Conditions 3 Subsurface Soil Conditions ' 4 Groundwater .. -
Geology 1 Questions for Chapter 19 2) ___Have Rainfall Amounts
Geology 1 Questions for Chapter 19 2) ________ have rainfall amounts and soil moisture contents between those of true deserts and humid lands. A) Tundras B) Steppes C) Sundras D) Sabkhas 3) Most dry lands lie between ________ degrees north and south of the equator. A) 40 and 50 B) 20 and 30 C) 5 and 10 D) 0 and 5 4) Which one of the following statements concerning rock weathering is true? A) Warm temperatures and high soil moisture contents accelerate chemical weathering. B) Low temperatures and high soil moisture contents accelerate chemical weathering but inhibit mechanical weathering. C) Warm temperatures and low soil moisture contents both promote rapid rates of mechanical weathering. D) Temperature has no effect on rock weathering. 5) A ________ is an intermittent stream channel in the dry land areas of the western United States. A) rivulet B) playa C) rill D) wash 6) ________ refers to the "bouncing" mode of sand transport in a windstorm or stream. A) Saltation B) Ventifaction C) Siltation D) Deflation 7) Which one of the following will effectively limit further deflation in a given area? A) sea level B) desert pavement C) a hanging valley D) the repose level 8) Which one of the following statements is correct? A) Alluvial fans typically rim desert valleys; playas form in the lowest, interior parts of the valleys. B) Inselbergs are low, circular depressions on gently sloping pediments and bajadas. C) Playas are typically covered with gravel-sized desert pavement and loess deposits. D) Saline sediments and evaporites are common in inselbergs and pediments of desert landscapes. -
The Great Mazury Lakes Trail
hen we think of Mazury, we usually associate it with sailing on the lakes, Water, forests beautiful, wild landscapes, and wind, Wlarge stretches of forests, and wind - not always blowing in the sails. And i.e. the essence of the that’s right! Someone who has never stayed in this area is not aware of how Mazury climate much he has lost, but someone who has just once been tempted to experience the Masurian adventure, will Wind in the sails…, remain faithful to the Land of the Great Mazury Lakes forever. The unques- photo GEP Chroszcz tionable natural and touristic values of the region are substantiated by the fact that it qualified for the final of the international competition, the New 7 Wonders of Nature, in which Mazury has been recognised as one of the 28 most beautiful places in the world. We shall wander across these unique areas along the water route whose main axis, leading from Węgorzewo to Nida Lake, is over 100 km long. If one is willing to visit everything, a distance of at least 330 km needs to be covered, and even then some places will remain undiscov- ered. The route leads to Węgorzewo, via Giżycko and Ryn to Mikołajki, from where you can set off to Pisz or Ruciane-Nida. If one wants to sail slowly, the proposed route will take less than two weeks. Choosing the express option, it is enough to reserve several days to cover it. What can fascinate us during the trip we are just starting? First of all, the environment, the richness of which can be hardly experienced on other routes. -
Glaciers and Glacial Erosional Landforms
GLACIERS AND GLACIAL EROSIONAL LANDFORMS Dr. NANDINI CHATTERJEE Associate Professor Department of Geography Taki Govt College Taki, North 24 Parganas, West Bengal Part I Geography Honours Paper I Group B -Geomorphology Topic 5- Development of Landforms GLACIER AND ICE CAPS Glacier is an extended mass of ice formed from snow falling and accumulating over the years and moving very slowly, either descending from high mountains, as in valley glaciers, or moving outward from centers of accumulation, as in continental glaciers. • Ice Cap - less than 50,000 km2. • Ice Sheet - cover major portion of a continent. • Ice thicker than topography. • Ice flows in direction of slope of the glacier. • Greenland and Antarctica - 3000 to 4000 m thick (10 - 13 thousand feet or 1.5 to 2 miles!) FORMATION AND MOVEMENT OF GLACIERS • Glaciers begin to form when snow remains Once the glacier becomes heavy enough, it in the same area year-round, where starts to move. There are two types of enough snow accumulates to transform glacial movement, and most glacial into ice. Each year, new layers of snow bury movement is a mixture of both: and compress the previous layers. This Internal deformation, or strain, in glacier compression forces the snow to re- ice is a response to shear stresses arising crystallize, forming grains similar in size and from the weight of the ice (ice thickness) shape to grains of sugar. Gradually the and the degree of slope of the glacier grains grow larger and the air pockets surface. This is the slow creep of ice due to between the grains get smaller, causing the slippage within and between the ice snow to slowly compact and increase in crystals.