Where Rivers Meet the Sea
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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. -
Landforms & Bodies of Water
Name Date Landforms & Bodies of Water - Vocab Cards hill noun a raised area of land smaller than a mountain. We rode our bikes up and down the grassy hill. Use this word in a sentence or give an example Draw this vocab word or an example of it: to show you understand its meaning: island noun a piece of land surrounded by water on all sides. Marissa's family took a vacation on an island in the middle of the Pacific Ocean. Use this word in a sentence or give an example Draw this vocab word or an example of it: to show you understand its meaning: 1 lake noun a large body of fresh or salt water that has land all around it. The lake freezes in the wintertime and we go ice skating on it. Use this word in a sentence or give an example Draw this vocab word or an example of it: to show you understand its meaning: landform noun any of the earth's physical features, such as a hill or valley, that have been formed by natural forces of movement or erosion. I love canyons and plains, but glaciers are my favorite landform. Use this word in a sentence or give an example Draw this vocab word or an example of it: to show you understand its meaning: 2 mountain noun a land mass with great height and steep sides. It is much higher than a hill. Someday I'm going to hike and climb that tall, steep mountain. Synonyms: peak Use this word in a sentence or give an example Draw this vocab word or an example of it: to show you understand its meaning: ocean noun a part of the large body of salt water that covers most of the earth's surface. -
Variability of Bed Mobility in Natural Gravel-Bed Channels
WATER RESOURCES RESEARCH, VOL. 36, NO. 12, PAGES 3743–3755, DECEMBER 2000 Variability of bed mobility in natural, gravel-bed channels and adjustments to sediment load at local and reach scales Thomas E. Lisle,1 Jonathan M. Nelson,2 John Pitlick,3 Mary Ann Madej,4 and Brent L. Barkett3 Abstract. Local variations in boundary shear stress acting on bed-surface particles control patterns of bed load transport and channel evolution during varying stream discharges. At the reach scale a channel adjusts to imposed water and sediment supply through mutual interactions among channel form, local grain size, and local flow dynamics that govern bed mobility. In order to explore these adjustments, we used a numerical flow model to examine relations between model-predicted local boundary shear stress ( j) and measured surface particle size (D50) at bank-full discharge in six gravel-bed, alternate-bar channels with widely differing annual sediment yields. Values of j and D50 were poorly correlated such that small areas conveyed large proportions of the total bed load, especially in sediment-poor channels with low mobility. Sediment-rich channels had greater areas of full mobility; sediment-poor channels had greater areas of partial mobility; and both types had significant areas that were essentially immobile. Two reach- mean mobility parameters (Shields stress and Q*) correlated reasonably well with sediment supply. Values which can be practicably obtained from carefully measured mean hydraulic variables and particle size would provide first-order assessments of bed mobility that would broadly distinguish the channels in this study according to their sediment yield and bed mobility. -
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. -
Moving Water Shapes Land
KEY CONCEPT Moving water shapes land. BEFORE, you learned NOW, you will learn •Erosion is the movement of • How moving water shapes rock and soil Earth’s surface • Gravity causes mass movements • How water moving under- of rock and soil ground forms caves and other features VOCABULARY EXPLORE Divides drainage basin p. 579 How do divides work? divide p. 579 floodplain p. 580 PROCEDURE MATERIALS alluvial fan p. 581 •sheet of paper 1 Fold the sheet of paper in thirds and tape delta p. 581 • tape it as shown to make a “ridge.” sinkhole p. 583 •paper clips 2 Drop the paper clips one at a time directly on top of the ridge from a height of about 30 cm. Observe what happens and record your observations. WHAT DO YOU THINK? How might the paper clips be similar to water falling on a ridge? Streams shape Earth’s surface. If you look at a river or stream, you may be able to notice something about the land around it. The land is higher than the river. If a river is running through a steep valley, you can easily see that the river is the low point. But even in very flat places, the land is sloping down to the river, which is itself running downhill in a low path through the land. NOTE-TAKING STRATEGY Running water is the major force shaping the landscape over most A main idea and detail of Earth. From the broad, flat land around the lower Mississippi River notes chart would be a good strategy to use for to the steep mountain valleys of the Himalayas, water running downhill taking notes about streams changes the land. -
Louisiana's Waterways
Section22 Lagniappe Louisiana’s The Gulf Intracoastal Waterways Waterway is part of the larger Intracoastal Waterway, which stretches some three As you read, look for: thousand miles along the • Louisiana’s major rivers and lakes, and U.S. Atlantic coast from • vocabulary terms navigable and bayou. Boston, Massachusetts, to Key West, Florida, and Louisiana’s waterways define its geography. Water is not only the dominant fea- along the Gulf of Mexico ture of Louisiana’s environment, but it has shaped the state’s physical landscape. coast from Apalachee Bay, in northwest Florida, to Brownsville, Texas, on the Rio Grande. Right: The Native Americans called the Ouachita River “the river of sparkling silver water.” Terrain: Physical features of an area of land 40 Chapter 2 Louisiana’s Geography: Rivers and Regions The largest body of water affecting Louisiana is the Gulf of Mexico. The Map 5 Mississippi River ends its long journey in the Gulf’s warm waters. The changing Mississippi River has formed the terrain of the state. Louisiana’s Louisiana has almost 5,000 miles of navigable rivers, bayous, creeks, and Rivers and Lakes canals. (Navigable means the water is deep enough for safe travel by boat.) One waterway is part of a protected water route from the Atlantic Ocean to the Map Skill: In what direction Gulf of Mexico. The Gulf Intracoastal Waterway extends more than 1,100 miles does the Calcasieu River from Florida’s Panhandle to Brownsville, Texas. This system of rivers, bays, and flow? manmade canals provides a safe channel for ships, fishing boats, and pleasure craft. -
So Many Ways to Make a River Bend
Presenter: John Holbrook So Many Ways to Make a River Bend John M. Holbrook Texas Christian University ABSTRACT The concept of meandering in rivers is old and well known, but so many of the known mechanisms of meandering are novel. The classic model of meander growth by translation and expansion generates upward-fining stories with en echolon accretion sets. This model still holds, but additional mechanisms, and variations on this theme, are now apparent. These mechanisms and variations manifest as differing architecture and lithofacies for deposits on the inner bend that ultimatly impact petroleum production trends. Bar-bend theory characterizes the growth of river meanders and the processes by which rivers will build bends. Transience in bedload transport demands that the channels will develop flow irregularities that are compensated by erosion at a cutbank. Deposition of a point bar is forced on the inner bend to maintain constant width in single-thread channels as the cutbank expands. This process deposits discrete shingles of bedload sediment as individual and parallel accretion sets on the point bar surface. No rule, however, demands that bar growth is exclusively by expansion or that growth have any constant roll or yaw. The bar growth surface can wobble, and the bar growth direction can translate, rotate, or can toggle inbetween expansion and translation, while still maintaining the constraint of a constant channel width (Figure 1). Each of these growth vectors alters internal bar architecture in separate ways. Wobble tends to form accretion surfaces with non-consistent dip that cross-cut and fragment accretion sets within bars. -
Effects of a Shallow Flood Shoal and Friction on Hydrodynamics of A
PUBLICATIONS Journal of Geophysical Research: Oceans RESEARCH ARTICLE Effects of a shallow flood shoal and friction on hydrodynamics 10.1002/2016JC012502 of a multiple-inlet system Key Points: Mara M. Orescanin1 , Steve Elgar2 , Britt Raubenheimer2 , and Levi Gorrell2 A flood shoal can act as a tidal reflector and limit the influence of an 1Oceanography Department, Naval Postgraduate School, Monterey, California, USA, 2Applied Ocean Physics and inlet in a multiple-inlet system Engineering, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA The effects of inertia, friction, and the flood shoal can be separated with a lumped element model As an inlet lengthens, narrows, and Abstract Prior studies have shown that frictional changes owing to evolving geometry of an inlet in a shoals, the lumped element model multiple inlet-bay system can affect tidally driven circulation. Here, a step between a relatively deep inlet shows the initial dominance of the and a shallow bay also is shown to affect tidal sea-level fluctuations in a bay connected to multiple inlets. shoal is replaced by friction To examine the relative importance of friction and a step, a lumped element (parameter) model is used that includes tidal reflection from the step. The model is applied to the two-inlet system of Katama Inlet (which Correspondence to: M. M. Orescanin, connects Katama Bay on Martha’s Vineyard, MA to the Atlantic Ocean) and Edgartown Channel (which con- [email protected] nects the bay to Vineyard Sound). Consistent with observations and previous numerical simulations, the lumped element model suggests that the presence of a shallow flood shoal limits the influence of an inlet. -
Component – I (A) Personal Details Role Name Affiliation Principal
Component – I (A) Personal Details Role Name Affiliation Principal Investigator Prof. Masood Ahsan Jamia Millia Islamia, New Siddiqui Delhi Paper Coordinator, if any Dr.Sayed Zaheen Alam Department of Geography Dyal Singh College University of Delhi Content Writer/Author (CW) Dr. Anshu Department of Geography Kirori Mal College University of Delhi Content Reviewer (CR) Dr.Sayed Zaheen Alam Department of Geography Dyal Singh College University of Delhi Language Editor (LE) Component-I (B) - Description of Module Items Description of Module Subject Name Geography Paper Name Geomorphology Module Name/Title Drainage Pattern Module Id Geo-20 Pre-requisites Objectives To comprehend the concept of Drainage Basin; Drainage patterns on basis of Empirical and Genetic classification; Channel Patterns Keywords Watershed, Basin, Antecedent, Superposed, Meander, Braid DRAINAGE PATTERN Dr. Anshu, Associate Professor, Department of Geography, Kirori Mal College, University of Delhi. 1. Drainage Basin The entire area that provides overland flow, stream flow and ground water flow to a particular stream is identified as the Drainage Basin or watershed of that stream. The basin consists of the streams’valley bottom, valley sides and interfluves that drain towards the valley. Drainage basin terminates at a drainage divide that is the line of separation between run off that flows in direction of one drainage basin and runoff that goes towards the adjoining basin. Drainage basin of the principal river will comprise smaller drainage basins with all its tributary streams and therefore the larger basins include hierarch of smaller tributary basins. 2. Drainage Pattern and Structural Relationship In a particular drainage basin, the streams may flow in a specific arrangement which is termed as drainage pattern. -
Landforms and Waterways Archipelago: an Archipelago Is a Cluster Or Chain of Islands in the Ocean, Such As the Galapagos Or the Hawaiian Islands
Landforms and Waterways Archipelago: An Archipelago is a cluster or chain of islands in the ocean, such as the Galapagos or the Hawaiian Islands. Atoll: An atoll is a reef, which forms a ring of small islands on a coral base that surrounds a lagoon of water in an ocean. There are many atolls in the Indo-Pacific. Bay: A bay is a body of water formed by an indentation of land, but still connected to the main body of water (ocean or lake) and is smaller that a gulf, but larger than a cove. Beach: A beach runs along coastlines, lakes or rivers and is made up of sand, pebbles or rocks. Bluff: A bluff is a high, steep bank or cliff. Butte: A butte is a hill, with steep sides and a flat top that is standing out on its own. Canyon: A canyon is a deep slice of land that runs between two steep cliff walls, often carved over time by a river. Cape: A cape is a spit of land that extends out into the ocean or other bodies of water (i.e. Cape Cod) Cave: A cave is a naturally formed hollow underground. Channel: A channel is a deeper section of a river that is sought after by boats for passage or a narrow body of water that connects two large bodies of water. Cliff: A cliff is a vertical rock wall. Col: A col is the lowest point between two peaks. Continent: A continent is one of seven large landmasses on earth: Asia, Africa, North America, South America, Antarctica, Europe, and Australia. -
Presented Below Are Water Quality Standards That Are in Effect for Clean Water Act Purposes
Presented below are water quality standards that are in effect for Clean Water Act purposes. EPA is posting these standards as a convenience to users and has made a reasonable effort to assure their accuracy. Additionally, EPA has made a reasonable effort to identify parts of the standards that are not approved, disapproved, or are otherwise not in effect for Clean Water Act purposes. I Stormwater Management Volume Two: Stormwater Technical Handbook March 1997 Prepared by: MA Department of Environmental Protection C2:M MA Office of Coastal Zone Management Stormwater Management Volume Two: Stormwater Technical Handbook March 1997 Funding for this document was provided by: · Massachusetts Department of Environmental Protection, · Massachusetts Office of Coastal Zone Management, and · U.S. Environmental Protection Agency. The document also was partially funded by a grant from the Office of Ocean and ) ' Coastal Resources Management, National Oceanic and Atmospheric - Administration, U.S. Department of Commerce. The views expressed are those of the author(s) and do not necessarily reflect the views of NOAA or any of its subagencies. The Commonwealth of Massachusetts William F. Weld, Governor Argeo Paul Cellucci, Lieutenant Governor Executive Office of Environmental Affairs Tmdy Coxe, Secretary Department of Environmental Protection David B. Struhs, Commissioner Bureau of Resource Protection Arleen O' Donnell, Assistant Commissioner This information is available in alternate formats upon request. ) Prinled on recycled paper .' Table of Contents -
What's a Watershed?
What’s a Watershed? Not everyone lives next to a stream or pond but all of us live in a watershed. A watershed is what we call the land area that drains into a body of water. You can also think of it as the land area that drains to a common outlet, such as the outflow of a lake, the mouth of a river, or any point along a stream channel. If a drop of water falling into a watershed does not evaporate or become part of a plant or animal, it will flow out of the watershed through this outlet. The path water takes across the land is determined mainly by gravity. High places -- ridges, mountains, and hills -- form divides between adjacent watersheds. Water always flows downhill—therefore the outer boundary of a watershed is formed by the ridges and hills surrounding a given waterbody. Precipitation (rain, snow, etc.) falling directly on the watershed boundary will be split between the watersheds on either side. The Hudson River officially starts at Lake Tear of the Clouds in the High Peaks area of the Adirondacks and flows south for 315 miles to the Atlantic Ocean at New York City. The huge watershed of the Hudson covers about 13,350 square miles, which includes most of eastern New York and small parts of Vermont, New Jersey, and Massachusetts. Parts of a Watershed The watershed of most lakes and rivers consists of a network of streams, wetlands, human-made channels, storm drains, and the surrounding upland. At any point in the watershed, precipitation runs off of the land surface and collects in these natural and human-made drainage pathways.