EES - Streams ____1

Total Page:16

File Type:pdf, Size:1020Kb

EES - Streams ____1 Name: __________________________ Date: _______ Pd. _______ EES - Streams ____1. Stream A has a steeper slope than ____4. In the two diagrams below, the length of stream B. However, the average water the arrows represents the relative velocities velocity of stream B is greater than that of of stream flow at various places in a stream. stream A. Which is the most reasonable Diagram I shows the different water explanation for this? velocities across the surface. Diagram II (1) Stream B has a higher average shows the different water velocities at temperature. various depths. (2) Stream B has more friction to overcome along its banks. (3) Stream B has a greater volume of water. (4) Stream B has a curved streambed. ____2. The diagram below represents a cross section of sedimentary deposits. Where would this type of deposition most likely occur? At which location in the stream is the water velocity greatest? (1) at the sides along the bottom (2) at the sides near the surface (3) at the center along the bottom (4) at the center near the surface ____5. The map below represents a view of a flowing stream. The letters identify locations (1) in a lake fed by a stream in the stream near the interface between (2) beneath a large glacier land and water. At which two locations is (3) at the rapids in a stream erosion due to flowing water likely to be (4) at the base of a shifting sand dune greatest? ____3. Stream velocity and stream discharge were recorded continuously at the same location in a stream channel. Which graph best shows the relationship between stream velocity and stream discharge at this location? (1) (3) (1) A and B (3) A and D (2) B and D (4) B and C ____6. Which rock particles will remain suspended in water for the longest time? (2) (4) (1) clay (3) sand (2) pebbles (4) silt Ms. Lee ____7. How are dissolved materials carried in a ____10. The map below shows the sizes of river? sediments deposited in different locations (1) in suspension within a stream and lake. A sample of (2) by precipitation sediments taken from one location consists (3) by bouncing and rolling mostly of particles that are approximately (4) in solution 0.4 centimeter in diameter. From which location was the sample most ____8. A sample of rounded quartz sediments of likely collected? different particle sizes is dropped into a container of water. Which graph best shows the settling time for these particles? (1) (3) From which location was the sample most likely collected? (1) A (3) C (2) B (4) D ____11. The four particles shown in the table below are of equal volume and are dropped into a column filled with water. (2) (4) ____9. A stream entering a lake deposits sediments on the lake bottom in the pattern shown on the map below. Which particle would usually settle most rapidly? (1) A (3) C (2) B (4) D Which corner of the map is nearest to the point where the stream flows into the lake? (1) northeast (NE) (3) southwest (SW) (2) northwest (NW) (4) southeast (SE) Ms. Lee ____12. Four quartz samples of equal size and ____15. The diagram below shows a portion of a shape were placed in a stream. Which of the stream. four quartz samples below has most likely been transported farthest in the stream? (1) (3) (2) (4) ____13. A sedimentary particle is dropped into a The sand bars formed as a direct result of cylinder of water. The particle will take the (1) deposition due to an increase in stream longest time to settle if the particle has velocity (1) low density, small size, and flattened (2) deposition due to a decrease in stream shape velocity (2) low density, small size, and spherical (3) erosion due to an increase in stream shape velocity (3) high density, large size, and spherical (4) erosion due to a decrease in stream shape velocity (4) high density, large size, and flattened shape ____16. The map below shows the top view of a meandering stream as it enters a lake. ____14. The map below represents a river as it enters a lake. At which points along the stream are erosion and deposition dominant? (1) Erosion is dominant at B and D, and At which locations is the amount of deposition is dominant at A and C. deposition greater than the amount of (2) Erosion is dominant at A and C, and erosion? deposition is dominant at B and D. (1) A, C, and E (3) B, C, and F (3) Erosion is dominant at A and D, and (2) A, D, and E (4) B, D, and F deposition is dominant at B and C. (4) Erosion is dominant at B and C, and deposition is dominant at A and D. Ms. Lee ____17. The map below shows a stream flowing ____19. The diagrams below show the stages, A into a lake. Locations A, B, and C are at the through D, in the formation of an oxbow lake water's edge, and location D is on the lake over a period of time. [The arrows indicate bottom. the direction of streamflow.] Which statement best describes erosion and deposition in this stream area (1) Erosion is dominant at B and D; deposition is dominant at A and C. (2) Erosion is dominant at B and C; deposition is dominant at A and D. (3) Erosion is dominant at A and D; deposition is dominant at B and C. (4) Erosion is dominant at A and C; deposition is dominant at B and D. ____18. The map below shows a meandering stream. Points A, B, C, and D represent locations along the stream bottom. Oxbow lakes are generally formed by (1) deposition, resulting in a sudden increase in the stream's gradient (2) deposition along the outside banks of the curve in a meandering stream (3) erosion, resulting in a sudden increase in the stream's gradient (4) erosion along the outside banks of the curve in a meandering stream At which location is the greatest amount of sediment most likely being deposited? (1) C (3) D (2) A (4) B Ms. Lee Ms. Lee ____20. The map below shows a river emptying into an ocean, producing a delta. Which graph best represents the relationship between the distance from the river delta into the ocean and the average size of sediments deposited on the ocean floor? (1) (2) (3) (4) Ms. Lee Answer Key [New Exam] 1. 3 2. 1 3. 1 4. 4 5. 3 6. 1 7. 4 8. 3 9. 3 10. 1 11. 4 12. 1 13. 1 14. 3 15. 2 16. 4 17. 4 18. 1 19. 4 20. 1 Ms. Lee.
Recommended publications
  • The Huron River History Book
    THE HURON RIVER Robert Wittersheim Over 15,000 years ago, the Huron River was born as a small stream draining the late Pleistocene landscape. Its original destination was Lake Maumee at present day Ypsilanti where a large delta was formed. As centuries passed, ceding lake levels allowed the Huron to meander over new land eventually settling into its present valley. Its 125 mile journey today begins at Big Lake near Pontiac and ends in Lake Erie. The Huron’s watershed, which includes 367 miles of tributaries, drains over 900 square miles of land. The total drop in elevation from source to mouth is nearly 300 feet. The Huron’s upper third is clear and fast, even supporting a modest trout fishery. The middle third passes through and around many lakes in Livingston and Washtenaw Counties. Eight dams impede much of the Huron’s lower third as it flows through populous areas it helped create. Over 47 miles of this river winds through publicly owned lands, a legacy from visionaries long since passed. White Lake White Lake Mary Johnson The Great Lakes which surround Michigan and the thousands of smaller lakes, hundreds of rivers, streams and ponds were formed as the glacier ice that covered the land nearly 14,000 years ago was melting. The waters filled the depressions in the earth. The glaciers deposited rock, gravel and soil that had been gathered in their movement. This activity sculpted the land creating our landscape. In section 28 of Springfield Township, Oakland County, a body of water names Big Lake by the area pioneers is the source of the Huron River.
    [Show full text]
  • Lesson 4: Sediment Deposition and River Structures
    LESSON 4: SEDIMENT DEPOSITION AND RIVER STRUCTURES ESSENTIAL QUESTION: What combination of factors both natural and manmade is necessary for healthy river restoration and how does this enhance the sustainability of natural and human communities? GUIDING QUESTION: As rivers age and slow they deposit sediment and form sediment structures, how are sediments and sediment structures important to the river ecosystem? OVERVIEW: The focus of this lesson is the deposition and erosional effects of slow-moving water in low gradient areas. These “mature rivers” with decreasing gradient result in the settling and deposition of sediments and the formation sediment structures. The river’s fast-flowing zone, the thalweg, causes erosion of the river banks forming cliffs called cut-banks. On slower inside turns, sediment is deposited as point-bars. Where the gradient is particularly level, the river will branch into many separate channels that weave in and out, leaving gravel bar islands. Where two meanders meet, the river will straighten, leaving oxbow lakes in the former meander bends. TIME: One class period MATERIALS: . Lesson 4- Sediment Deposition and River Structures.pptx . Lesson 4a- Sediment Deposition and River Structures.pdf . StreamTable.pptx . StreamTable.pdf . Mass Wasting and Flash Floods.pptx . Mass Wasting and Flash Floods.pdf . Stream Table . Sand . Reflection Journal Pages (printable handout) . Vocabulary Notes (printable handout) PROCEDURE: 1. Review Essential Question and introduce Guiding Question. 2. Hand out first Reflection Journal page and have students take a minute to consider and respond to the questions then discuss responses and questions generated. 3. Handout and go over the Vocabulary Notes. Students will define the vocabulary words as they watch the PowerPoint Lesson.
    [Show full text]
  • Geomorphic Classification of Rivers
    9.36 Geomorphic Classification of Rivers JM Buffington, U.S. Forest Service, Boise, ID, USA DR Montgomery, University of Washington, Seattle, WA, USA Published by Elsevier Inc. 9.36.1 Introduction 730 9.36.2 Purpose of Classification 730 9.36.3 Types of Channel Classification 731 9.36.3.1 Stream Order 731 9.36.3.2 Process Domains 732 9.36.3.3 Channel Pattern 732 9.36.3.4 Channel–Floodplain Interactions 735 9.36.3.5 Bed Material and Mobility 737 9.36.3.6 Channel Units 739 9.36.3.7 Hierarchical Classifications 739 9.36.3.8 Statistical Classifications 745 9.36.4 Use and Compatibility of Channel Classifications 745 9.36.5 The Rise and Fall of Classifications: Why Are Some Channel Classifications More Used Than Others? 747 9.36.6 Future Needs and Directions 753 9.36.6.1 Standardization and Sample Size 753 9.36.6.2 Remote Sensing 754 9.36.7 Conclusion 755 Acknowledgements 756 References 756 Appendix 762 9.36.1 Introduction 9.36.2 Purpose of Classification Over the last several decades, environmental legislation and a A basic tenet in geomorphology is that ‘form implies process.’As growing awareness of historical human disturbance to rivers such, numerous geomorphic classifications have been de- worldwide (Schumm, 1977; Collins et al., 2003; Surian and veloped for landscapes (Davis, 1899), hillslopes (Varnes, 1958), Rinaldi, 2003; Nilsson et al., 2005; Chin, 2006; Walter and and rivers (Section 9.36.3). The form–process paradigm is a Merritts, 2008) have fostered unprecedented collaboration potentially powerful tool for conducting quantitative geo- among scientists, land managers, and stakeholders to better morphic investigations.
    [Show full text]
  • Oxbow Lakes White Paper
    Mississippi-Alabama Sea Grant Legal Program University of Mississippi School of Law Kinard Hall, Wing E – Room 256 University, MS 38677 (662) 915-7775 [email protected] PUBLIC RIGHTS ON MISSISSIPPI PUBLIC WATERS A White Paper Prepared by Josh Clemons, J.D. Independent Consultant and Former Research Counsel April 2011 This white paper was commissioned by the Mississippi Department of Wildlife, Fisheries, and Parks. The following information is intended as independent research only and does not constitute legal representation of MDWFP or any of its constituents by the Mississippi-Alabama Sea Grant Legal Program. It represents our interpretation of the relevant laws. This product was prepared by the Mississippi-Alabama Sea Grant Legal Program under award number NA06OAR4170078 from the Mississippi-Alabama Sea Grant Consortium and National Oceanic and Atmospheric Administration, U.S. Department of Commerce. The statements, findings, conclusions, and recommendations are those of the authors and do not necessarily reflect the views of NOAA or the U.S. Department of Commerce. MASGP 11-008-13 The Mississippi Code declares, in sweeping language, that the policy of the State of Mississippi is to allow its citizens to enjoy the bounty of her woods and waters: Hunting, trapping and fishing are vital parts of the heritage of the State of Mississippi. It shall be the public policy of the State of Mississippi to protect and preserve these activities. The Mississippi Commission on Wildlife, Fisheries and Parks, acting by and through the Mississippi Department of Wildlife, Fisheries and Parks, may regulate hunting, trapping and fishing activities in the State of Mississippi, consistent with its powers and duties under the law.
    [Show full text]
  • Classifying Rivers - Three Stages of River Development
    Classifying Rivers - Three Stages of River Development River Characteristics - Sediment Transport - River Velocity - Terminology The illustrations below represent the 3 general classifications into which rivers are placed according to specific characteristics. These categories are: Youthful, Mature and Old Age. A Rejuvenated River, one with a gradient that is raised by the earth's movement, can be an old age river that returns to a Youthful State, and which repeats the cycle of stages once again. A brief overview of each stage of river development begins after the images. A list of pertinent vocabulary appears at the bottom of this document. You may wish to consult it so that you will be aware of terminology used in the descriptive text that follows. Characteristics found in the 3 Stages of River Development: L. Immoor 2006 Geoteach.com 1 Youthful River: Perhaps the most dynamic of all rivers is a Youthful River. Rafters seeking an exciting ride will surely gravitate towards a young river for their recreational thrills. Characteristically youthful rivers are found at higher elevations, in mountainous areas, where the slope of the land is steeper. Water that flows over such a landscape will flow very fast. Youthful rivers can be a tributary of a larger and older river, hundreds of miles away and, in fact, they may be close to the headwaters (the beginning) of that larger river. Upon observation of a Youthful River, here is what one might see: 1. The river flowing down a steep gradient (slope). 2. The channel is deeper than it is wide and V-shaped due to downcutting rather than lateral (side-to-side) erosion.
    [Show full text]
  • Lake Restoration Report
    Lake Restoration Program 2020 Report and 2021 Plan A cooperative dredging project between DNR and the City of Council Bluffs removed over 500,000 CY of sand from Lake Manawa (Monona County), providing materials for a local levee-building project and improving water quality within the lake. Watershed ponds, constructed at West Lake Park in Scott County, will protect the four lakes in the Lake of the Hills Complex for many years. Mariposa Lake (Jasper County) following restoration, completed in 2020. The project included building two new ponds in the park to protect the lake, dredging, shoreline stabilization, and fish habitat. Submitted To Joint Appropriations Subcommittee on Transportation, Infrastructure, and Capitals and Legislative Services Agency 1 Executive Summary The Fiscal Year 2020 Iowa Lake Restoration Report and Fiscal Year 2021 Plan provides a status of past appropriated legislatively directed funding; outlines the future needs and demands for lake restoration in Iowa; and identifies a prioritized group of lakes and the associated costs for restoration. Iowans value water quality and desire safe healthy lakes that provide a full complement of aesthetic, ecological and recreational benefits. A recently completed water-based recreational use survey by Iowa State University found that six of 10 Iowans visit our lakes multiple times each year and spend $1.2 billion annually in their pursuit of outdoor lake recreation. The most popular activities are fishing, picnicking, wildlife viewing, boating, hiking/biking, swimming and beach use. In addition, visitations at lakes that have completed watershed and lake improvements efforts continue to exceed the state average and their own pre-restoration visitation levels.
    [Show full text]
  • Lake Restoration Report
    Lake Restoration Program 2019 Report and 2020 Plan Watershed Improvement: Over 200 watershed practices, like the bio-retention cells pictured here were installed around Easter Lake to capture storm water and improve water quality In-Lake Work: Numerous practices were installed including dredging 678,000 cubic yards of excess sediment from the lake After: Easter Lake Grand Re-Opening Celebration June 2019 Submitted To Joint Appropriations Subcommittee on Transportation, Infrastructure, and Capitals and Legislative Services Agency Executive Summary The 2019 Iowa Lake Restoration Report and 2020 Plan outlines the need and demand for lake restoration in Iowa; identifies a prioritized group of lakes and the associated costs for restoration; and provides the status of past appropriated legislatively directed funding. Iowans value water quality and desire safe healthy lakes that provide a full complement of aesthetic, ecological and recreational benefits. A recently completed water-based recreational use survey by Iowa State University found that six of 10 Iowans visit our lakes multiple times each year and spend $1.2 billion annually in their pursuit of outdoor lake recreation. The most popular activities are fishing, picnicking, wildlife viewing, boating, hiking/biking, swimming and beach use. In addition, visitations at lakes that have completed watershed and lake improvements efforts continue to exceed the state average and their own pre-restoration visitation levels. People are also willing to drive farther for lakes with better water quality and more amenities. Legislative Action Goals of Iowa’s Lake Restoration Program include: improved water quality, a diverse, balanced aquatic community, and sustained public use benefits. Many of our Iowa Lakes, similar to our nation’s lakes, are impaired and suffer from excessive algae growth and sedimentation due to nutrient loading and soil loss.
    [Show full text]
  • The Persistence of Oxbow Lakes As Aquatic Habitats: an Assessment of Rates of Change and Patterns of Alluviation
    The Persistence of Oxbow Lakes as Aquatic Habitats: an Assessment of Rates of Change and Patterns of Alluviation Pauline L. Dieras 2013 Thesis submitted for the degree of Doctorate of Philosophy Declaration This work has not been submitted in substance for any other degree or award at this or any other university or place of learning, nor is being submitted concurrently in candidature for any degree or other award. Signed Pauline Dieras Date: 05/03/2013 This thesis is being submitted in partial fulfilment of the requirements for the degree of PhD Signed Pauline Dieras Date: 05/03/2013 This thesis is the result of my own independent work/investigation, except where otherwise stated. Other sources are acknowledged by explicit references. The views expressed are my own. Signed Pauline Dieras Date: 05/03/2013 I hereby give consent for my thesis, if accepted, to be available for photocopying and for inter-library loan, and for the title and summary to be made available to outside organisations. Signed Pauline Dieras Date: 05/03/2013 i Abstract Oxbow lakes are of high ecological importance due to the number and the diversity of habitats they provide. They are created after the abandonment of meanders and subsequent sediment infilling leads to their progressive terrestrialisation, taking from a few months up to several centuries. Nonetheless, little is known about oxbow lake terrestrialisation processes, sediment composition, or why such a disparity exists in lakes’ longevity. To understand the controls on oxbow lakes alluviation, field observations, remotely sensed data and GIS analyses were combined. Sediment transfers in oxbow lakes were documented by topographic and sampling surveys of sites in France and Wales.
    [Show full text]
  • OXBOW LAKE (BROWNWATER SUBTYPE) Concept: Oxbow Lakes Are Permanently Flooded Open Water Depressions in Large Floodplains, Isolat
    OXBOW LAKE (BROWNWATER SUBTYPE) Concept: Oxbow Lakes are permanently flooded open water depressions in large floodplains, isolated from the river by channel shifts. Most are largely unvegetated, but they may contain sparse vegetation or patches of woody or herbaceous wetland plants of various kinds. The Brownwater Subtype covers those along brownwater rivers, which receive substantial mineral sediment input. They typically have an edge zone containing Taxodium distichum, Nyssa aquatica, Platanus occidentalis, or Betula nigra. Distinguishing Features: Oxbow Lake communities are distinguished from Cypress–Gum Swamps by being wet enough to lack a closed tree canopy. They are distinguished from Semipermanent Impoundment communities by occurring in closed, undammed basins created by an abandoned river channel. This setting produces an aquatic community that is isolated from both the river and from stream input except in floods. The Brownwater Subtype can usually easily be distinguished by the character of the river and the occurrence of brownwater communities adjacent to it. It typically has an edge zone containing brownwater species such as Platanus occidentalis or Fraxinus pennsylvanica as well as the more widespread Taxodium distichum and Betula nigra. Synonyms: Not covered in NVC. Ecological Systems: Atlantic Coastal Plain Small Brownwater River Floodplain Forest (CES203.250). Sites: Oxbow Lake communities occur in large floodplains in segments of former river channels that have become isolated from the river by channel shifts. Deposition along the new river course has closed them off, turning them into basins that hold permanent water and are not connected to the river except during floods. Soils: Oxbow Lake soils are treated as inclusions or mapped as water in soil surveys.
    [Show full text]
  • A Journey Toward Oxbow Lake Formation and Associated Change in Human Mosaic: Study on Kalindri River of Malda District
    IOSR Journal Of Humanities And Social Science (JHSS) ISSN: 2279-0837, ISBN: 2279-0845. Volume 5, Issue 6 (Nov. - Dec. 2012), PP 32-39 Www.Iosrjournals.Org A Journey Toward Oxbow Lake Formation and Associated Change in Human Mosaic: Study on Kalindri River of Malda District Dr. Swades Pal1, Shyamal Kumar Kar2 1Assistant Professor, Deptt. of Geography, University of Gour Banga, West Bengal 2Research Scholar, Deptt. of Geography, Visva-Bharati, West Bengal Abstract: This paper aims to illustrate the phases of oxbow lake formation in Kalindri river adjacent of Naogharia region and how over time being these oxbow lakes have converted into wetlands of multifaceted resource pools. At the same time it is also being attempted to show how the dynamics of river course is entangled with dynamism of population migration, settlement shifting, occupational shifting, and change of economic activities. Consultations of some old maps, local peoples’ perceptions, time to time field survey etc. have done to prepare this article. It is found that two successive oxbow lakes formation and frequent over spilling events have direct impact on shifting of higher class population and settlement but the soil Childs are more interested to adjust with the situation. Poor sections of people have been adjusting themselves with changing physical setup and they have no anguish for frequent rehabilitation. Process of oxbow lake formation has also generated an excellent fertile land and which is considered to be a agricultural hotspot. Similarly, formation of oxbow lake wetland has generated good livelihood stability with ample opportunities of fishing, shelling, crabbing, hydrophytic vegetable production, wetland based irrigation non monsoon agriculture practices etc.
    [Show full text]
  • The Significance of Oxbow Lakes for the Ecosystem of Afforested River Valleys
    JOURNAL OF WATER AND LAND DEVELOPMENT J. Water Land Dev. No. 13a, 2009: 115–131 The significance of oxbow lakes for the ecosystem of afforested river valleys Józef KOC, Szymon KOBUS, Katarzyna GLIŃSKA-LEWCZUK University of Warmia and Mazury in Olsztyn, Department of Land Reclamation and Environment Management, ul. Plac Łódzki 2, 10-719 Olsztyn, Poland; e-mail: [email protected] Abstract: The interest in significance of forest areas in water quality improvement has been increas- ing since creation of biogeochemical barriers became effective tools against the input of pollutants to surface water from diffuse sources. Along meandering river valleys, numerous floodplain lakes often appear as valuable water ecosystems but of advanced eutrophy. Their trophic status depends not only on the hydrological connectivity with the river but also land use in the direct vicinity of the reservoir. Research on water ecosystems in the postglacial river valleys in northern Poland contributed to iden- tification of the role of woodland area in pollutants migration in the valley of the Łyna River. The study on the ecosystem concerned seasonal variation in nutrient concentrations (N and P) and bottom sediments properties in relation to hydrological conditions (water level fluctuations). Based on the collected data we attempted prediction of the reservoir lifetime. Depending on hydrological, geological and topographic conditions the origin of water supply of the basin is changing. Annual water level fluctuations in the range of 200 cm cause the basin capacity variation as much as 5 times. Nevertheless, water quality in the lake was conditioned by the riverine supply, the significant share in the lake feeding has groundwater supply from hillslope aquifer and seepage through alluvial aquifer.
    [Show full text]
  • Vilas County Shoreland Zoning Ordinance
    VILAS COUNTY SHORELAND ZONING ORDINANCE 0 VILAS COUNTY SHORELAND ZONING ORDINANCE TABLE OF CONTENTS ARTICLE I STATUTORY AUTHORIZATION, FINDING OF FACT, STATEMENT OF PURPOSE & TITLE 1.1 Statutory Authorization ---------------------------------------------------------------------1-1 1.2 Findings of Fact -------------------------------------------------------------------------------1-1 1.3 Purpose and Intent ---------------------------------------------------------------------------1-1 ARTICLE1.4 II TitleGENERAL-------------------------------- PROVISIONS -------------------------------------------------------------1-2 2.1 Regulated Shoreland Areas -----------------------------------------------------------------2-1 2.2 Incorporated Shoreland Zoning Maps and Reports ------------------------------------2-1 2.3 Compliance with This Ordinance ----------------------------------------------------------2-1 2.4 Relationship to Other Zoning and Property Restrictions------------------------------2-2 2.5 Administration and Enforcement----------------------------------------------------------2-3 2.6 Relaxation of Standards for Persons with Disabilities ---------------------------------2-4 2.7 Interpretation ---------------------------------------------------------------------------------2-4 2.8 Severability ------------------------------------------------------------------------------------2-4 History:2.9 (AmendmentDetermination #85-250, Table Contents of Navigability Article II 2.6, and 2.9, Ordinary2.10, effective High02-01 Water-17) Mark ---------------------2-4
    [Show full text]