Analysis of Stream Runoff Trends in the Blue Ridge and Piedmont of Southeastern United States
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Cobb County, Georgia and Incorporated Areas
VOLUME 1 OF 4 Cobb County COBB COUNTY, GEORGIA AND INCORPORATED AREAS COMMUNITY NAME COMMUNITY NUMBER ACWORTH, CITY OF 130053 AUSTELL, CITY OF 130054 COBB COUNTY 130052 (UNINCORPORATED AREAS) KENNESAW, CITY OF 130055 MARIETTA, CITY OF 130226 POWDER SPRINGS, CITY OF 130056 SMYRNA, CITY OF 130057 REVISED: MARCH 4, 2013 FLOOD INSURANCE STUDY NUMBER 13067CV001D NOTICE TO FLOOD INSURANCE STUDY USERS Communities participating in the National Flood Insurance Program have established repositories of flood hazard data for floodplain management and flood insurance purposes. This Flood Insurance Study (FIS) report may not contain all data available within the Community Map Repository. Please contact the Community Map Repository for any additional data. The Federal Emergency Management Agency (FEMA) may revise and republish part or all of this FIS report at any time. In addition, FEMA may revise part of this FIS report by the Letter of Map Revision process, which does not involve republication or redistribution of the FIS report. Therefore, users should consult with community officials and check the Community Map Repository to obtain the most current FIS report components. Initial Countywide FIS Effective Date: August 18, 1992 Revised Countywide FIS Effective Date: December 16, 2008 Revised Countywide FIS Effective Date: March 4, 2013 TABLE OF CONTENTS Page 1.0 INTRODUCTION 1 1.1 Purpose of Study 1 1.2 Authority and Acknowledgments 1 1.3 Coordination 3 2.0 AREA STUDIED 5 2.1 Scope of Study 5 2.2 Community Description 10 2.3 Principal Flood Problems -
List of TMDL Implementation Plans with Tmdls Organized by Basin
Latest 305(b)/303(d) List of Streams List of Stream Reaches With TMDLs and TMDL Implementation Plans - Updated June 2011 Total Maximum Daily Loadings TMDL TMDL PLAN DELIST BASIN NAME HUC10 REACH NAME LOCATION VIOLATIONS TMDL YEAR TMDL PLAN YEAR YEAR Altamaha 0307010601 Bullard Creek ~0.25 mi u/s Altamaha Road to Altamaha River Bio(sediment) TMDL 2007 09/30/2009 Altamaha 0307010601 Cobb Creek Oconee Creek to Altamaha River DO TMDL 2001 TMDL PLAN 08/31/2003 Altamaha 0307010601 Cobb Creek Oconee Creek to Altamaha River FC 2012 Altamaha 0307010601 Milligan Creek Uvalda to Altamaha River DO TMDL 2001 TMDL PLAN 08/31/2003 2006 Altamaha 0307010601 Milligan Creek Uvalda to Altamaha River FC TMDL 2001 TMDL PLAN 08/31/2003 Altamaha 0307010601 Oconee Creek Headwaters to Cobb Creek DO TMDL 2001 TMDL PLAN 08/31/2003 Altamaha 0307010601 Oconee Creek Headwaters to Cobb Creek FC TMDL 2001 TMDL PLAN 08/31/2003 Altamaha 0307010602 Ten Mile Creek Little Ten Mile Creek to Altamaha River Bio F 2012 Altamaha 0307010602 Ten Mile Creek Little Ten Mile Creek to Altamaha River DO TMDL 2001 TMDL PLAN 08/31/2003 Altamaha 0307010603 Beards Creek Spring Branch to Altamaha River Bio F 2012 Altamaha 0307010603 Five Mile Creek Headwaters to Altamaha River Bio(sediment) TMDL 2007 09/30/2009 Altamaha 0307010603 Goose Creek U/S Rd. S1922(Walton Griffis Rd.) to Little Goose Creek FC TMDL 2001 TMDL PLAN 08/31/2003 Altamaha 0307010603 Mushmelon Creek Headwaters to Delbos Bay Bio F 2012 Altamaha 0307010604 Altamaha River Confluence of Oconee and Ocmulgee Rivers to ITT Rayonier -
Smallies on the Little T" BASSMASTER MAGAZINE Volume 32, No.7 by Jay Kumar
"Smallies on the Little T" BASSMASTER MAGAZINE Volume 32, No.7 by Jay Kumar North Carolina's Little Tennessee River Is an untapped hot spot for hard-fighting bronzebacks . SOMEONE SAYS "bass fishing in North Carolina" ---what comes to mind? If you're like me, you can practically taste the sweat running down your face as you probe likely looking weedbeds in lakes and tidal rivers, looking for that monster largemouth. Certainly, smallmouth fishing wouldn't even come up. For the most part, we'd be right. But western North Carolina is mountainous and cool, much like its neighbors, Virginia. West Virginia and Tennessee, all of which are prime small mouth country. Western North Carolina is no different. And tucked away in the Nantahala National Forest is a place where these fish, the "fight- ingest" of all, swim free and largely unmolested: the Little Tennessee River. In fact, almost no one fished for "little T” bronzebacks until a transplanted Arkansas restaurateur decided, after searching all over the South that this was the place he was going to establish an outfit- ting business. It's an "if you build it they will come" story: in 1991, after getting lost on his way out of the Great Smokey Mountains, Jerry Anselmo found himself paralleling the Little T on Route 28. He stopped in town and asked where he could rent a canoe. The answer? Nowhere. So he borrowed one and "just caught the heck out of smallmouths.". That day he started looking for property on the river and the rest is history. -
The Origins of Camp Louise in the Settlement House Movement of Baltimore’S Jewish Community
1 “Fresh Air and Cheer”: The Origins of Camp Louise in the Settlement House Movement of Baltimore’s Jewish Community by Barry Kessler One day in 1921, three Baltimoreans set out to visit a potential site for a summer retreat that would serve the city’s immigrant Jewish women. Ida Sharogrodsky, a social worker, and Lillie Straus, a philanthropist, had pleaded with Lillie’s husband, Aaron, one of Baltimore’s wealthiest merchants, to consider purchasing an old hotel in the Catoctin Mountains which they envisioned as an extension of the social service work they were doing in East Baltimore. Midway on the seventy‐mile trip, Aaron Straus seized on the pretext of a storm to turn back, but the ladies were undeterred, and once they arrived, the enchanting view of forested hills and fertile valleys overcame his reluctance. 1 The story of the three founders’ trip has served as the origin myth of Camp Louise, which matured from a vacation spot for working women to a traditional Jewish girls’ summer camp and is still operating almost a hundred years later. It’s a charming tale, retold over generations by camp alumnae and counselors, staff and community leaders. But the actual history of how Camp Louise emerged from Baltimore’s Progressive era efforts to aid, acculturate, and assimilate immigrants is more complex and in many ways more interesting. In the late nineteenth and early twentieth centuries, Baltimore faced the twin pressures of industrialization and immigration, which gave rise to enormous challenges as well as critical opportunities for the city, and for its Jewish community in particular. -
Rule 391-3-6-.03. Water Use Classifications and Water Quality Standards
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. Rule 391-3-6-.03. Water Use Classifications and Water Quality Standards ( 1) Purpose. The establishment of water quality standards. (2) W ate r Quality Enhancement: (a) The purposes and intent of the State in establishing Water Quality Standards are to provide enhancement of water quality and prevention of pollution; to protect the public health or welfare in accordance with the public interest for drinking water supplies, conservation of fish, wildlife and other beneficial aquatic life, and agricultural, industrial, recreational, and other reasonable and necessary uses and to maintain and improve the biological integrity of the waters of the State. ( b) The following paragraphs describe the three tiers of the State's waters. (i) Tier 1 - Existing instream water uses and the level of water quality necessary to protect the existing uses shall be maintained and protected. (ii) Tier 2 - Where the quality of the waters exceed levels necessary to support propagation of fish, shellfish, and wildlife and recreation in and on the water, that quality shall be maintained and protected unless the division finds, after full satisfaction of the intergovernmental coordination and public participation provisions of the division's continuing planning process, that allowing lower water quality is necessary to accommodate important economic or social development in the area in which the waters are located. -
Blue Ridge Park Way DIRECTORY TRAVEL PLANNER
65 TH Edition Blue Ridge Park way www.blueridgeparkway.org DIRECTORY TRAVEL PLANNER Includes THE PARKWAY MILEPOST Biltmore Asheville, NC Exit at Milepost 388.8 Grandfather Mountain Linville, NC Exit at Milepost 305.1 Roanoke Star and Overlook Roanoke, VA Exit at Milepost 120 Official Publication of the Blue Ridge Parkway Association The 65th Edition OFFICIAL PUBLICATION BLUE RIDGE PARKWAY ASSOCIATION, INC. P. O. BOX 2136, ASHEVILLE, NC 28802 (828) 670-1924 www.blueridgeparkway.org • [email protected] COPYRIGHT 2014 NO Portion OF THIS GUIDE OR ITS MAPS may BE REPRINTED WITHOUT PERMISSION. ALL RIGHTS RESERVED. PRINTED IN THE USA. Some Parkway photographs by William A. Bake, Mike Booher, Vicki Dameron and Jeff Greenberg © Blue Ridge Parkway Association Layout/Design: Imagewerks Productions: Arden, NC This free Directory & Travel PROMOTING Planner is published by the 500+ member Blue Ridge TOURISM FOR Parkway Association to help Chimney Rock at you more fully enjoy your Chimney Rock State Park Parkway area vacation. MORE THAN Members representing attractions, outdoor recre- ation, accommodations, res- Follow us for more Blue Ridge Parkway 60 YEARS taurants, shops, and a variety of other services essential to information and resources: the traveler are included in this publication. When you visit their place of business, please let them know www.blueridgeparkway.org you found them in the Blue Ridge Parkway Directory & Travel Planner. This will help us ensure the availability of another Directory & Travel Planner for your next visit -
River Clean-Up Guru, Bobby Marie…
River Clean-Up Guru, Bobby Marie… 1/11/2012 - Chattahoochee River 1/14/2012 – Etowah River 1/14/2012 – Coosa River 1/14/2012 – Oostanaula River 2/8/2012 – Peachtree Creek, South Fork 2/15/2012 – Peachtree Creek, North Fork 2/29/2012 – Suwannee River 4/21/2012 – Little River 5/16/2012 – Nickajack Creek 6/17/2012 – Altamaha River 8/8/2012 – Amicalola Creek 9/8/2012 – South River To view more 12 in 2012 finishers, go here. 1/11/2012 – Chattahoochee River Good Morning, I and two others paddled upstream on the Chattahoochee from Jones Bridge for about 4 miles then back down on a cold January afternoon on the 11th. It rained on us a couple of times, but the paddling kept us warm. We passed empty golf courses and leafless trees. We did see several herons and a couple of raptors hunting the river. Bobby Marie 1/14/2012 – Etowah, Coosa, Oostanala Rivers On January 14th, I joined Joe Cook and about 100 others on the CRBI Polar Bear Paddle over by Rome, GA. In one day I paddled 3 rivers, the Etowah for the major portion of the trip, then took two side paddles, upstream on the Oostanala for 30 minutes and then down and back up the Coosa for 30 minutes. When you reach the confluence of these three rivers you can look down and see the difference in the waters. The Etowah was greenish and the Oostanala was very brown and the Coosa was a mixture of the two! I only saw one BIG cooter on the bank in the sun the whole day. -
South Carolina Landform Regions (And Facts About Landforms) Earth Where Is South Carolina? North America United States of America SC
SCSouth Carolina Landform Regions (and facts about Landforms) Earth Where is South Carolina? North America United States of America SC Here we are! South Carolina borders the Atlantic Ocean. SC South Carolina Landform Regions Map Our state is divided into regions, starting at the mountains and going down to the coast. Can you name these? Blue Ridge Mountains Landform Regions SC The Blue Ridge Mountain Region is only 2% of the South Carolina land mass. Facts About the Blue Ridge Mountains . ◼ It is the smallest of the landform regions ◼ It includes the state’s highest point: Sassafras Mountain. ◼ The Blue Ridge Mountains are part of the Appalachian Mountain Range Facts About the Blue Ridge Mountains . ◼ The Blue Ridge Region is mountainous and has many hardwood forests, streams, and waterfalls. ◼ Many rivers flow out of the Blue Ridge. Blue Ridge Mountains, SC Greenville Spartanburg Union Greenwood Rock Hill Abbeville Piedmont Landform Regions SC If you could see the Piedmont Region from space and without the foliage, you would notice it is sort of a huge plateau. Facts About the Piedmont Region . ◼ The Piedmont is the largest region of South Carolina. ◼ The Piedmont is often called The Upstate. Facts About the Piedmont Region . ◼ It is the foothills of the mountains and includes rolling hills and many valleys. ◼ Piedmont means “foot of the mountains” ◼ Waterfalls and swift flowing rivers provided the water power for early mills and the textile industry. Facts About the Piedmont Region . ◼ The monadnocks are located in the Piedmont. ◼ Monadnocks – an isolated or single hill made of very hard rock. -
Summary of Water Quality Information for the Little Tennessee River Basin
Chapter 3 - Summary of Water Quality Information for the Little Tennessee River Basin 3.1 General Sources of Pollution Human activities can negatively impact surface water quality, even when the Point Sources activity is far removed from the waterbody. With proper management of Piped discharges from: • wastes and land use activities, these Municipal wastewater treatment plants • impacts can be minimized. Pollutants that Industrial facilities • Small package treatment plants enter waters fall into two general • Large urban and industrial stormwater systems categories: point sources and nonpoint sources. Point sources are typically piped discharges and are controlled through regulatory programs administered by the state. All regulated point source discharges in North Carolina must apply for and obtain a National Pollutant Discharge Elimination System (NPDES) permit from the state. Nonpoint sources include a broad range of land Nonpoint Sources use activities. Nonpoint source pollutants are typically carried to waters by rainfall, runoff or • Construction activities snowmelt. Sediment and nutrients are most often • Roads, parking lots and rooftops associated with nonpoint source pollution. Other • Agriculture pollutants associated with nonpoint source • Failing septic systems and straight pipes pollution include fecal coliform bacteria, oil and • Timber harvesting grease, pesticides and any other substance that • Hydrologic modifications may be washed off of the ground or deposited from the atmosphere into surface waters. Unlike point sources of pollution, nonpoint pollution sources are diffuse in nature and occur intermittently, depending on rainfall events and land disturbance. Given these characteristics, it is difficult and resource intensive to quantify nonpoint contributions to water quality degradation in a given watershed. While nonpoint source pollution control often relies on voluntary actions, the state has many programs designed to reduce nonpoint source pollution. -
Geology of Gambrill State Park
Introduction A West Gambrill State Park is located along the eastern edge of the Blue Ridge b Physiographic Province. The Blue Ridge Mountains stretch from northern Georgia to southern Pennsylvania. The Blue Ridge is made up of folded Eas x t rocks that are broken in places by faults. In Maryland, the Blue Ridge b consists of two separate ridges-Catoctin Mountain, locally known as A B C Braddock Mountain on the east, and South Mountain to the west. The Blue Figure 1. Rocks of Gambrill State Park. A, Catoctin Formation. Green- Ridge is bordered on the east by the Piedmont Physiographic Province. The ish metamorphosed basalts. B, Loudoun Formation. Volcanic ash Piedmont is underlain by metamorphic rocks that were formed when the containing pebbles of lava (at A). C, Weverton Formation. Cross- 9 W Appalachian Mountains were uplifted more than 250 million years ago bedded sandstone (b=bedding, x=cross-bedding) . ever C ton Form (hereafter Ma). What we see from Catoctin Mountain today is the result of to weathering and erosion. As a result of this durability, the Weverton ation millions of years of erosion of those mountains. Formation represents the main ridge-forming layer on both Catoctin and Bedrock Layers South mountains of the Blue Ridge of Virginia, Maryland, and Pennsylvania. Nearly all of the rocks present in the park are assignable to three These ridges are erosional features left standing high after the softer or more geologic rock units, called formations. These are the Catoctin, the Loudoun, soluble rocks on either side were worn down by weathering and erosion. -
Fish Consumption Guidelines: Rivers & Creeks
FRESHWATER FISH CONSUMPTION GUIDELINES: RIVERS & CREEKS NO RESTRICTIONS ONE MEAL PER WEEK ONE MEAL PER MONTH DO NOT EAT NO DATA Bass, LargemouthBass, Other Bass, Shoal Bass, Spotted Bass, Striped Bass, White Bass, Bluegill Bowfin Buffalo Bullhead Carp Catfish, Blue Catfish, Channel Catfish,Flathead Catfish, White Crappie StripedMullet, Perch, Yellow Chain Pickerel, Redbreast Redhorse Redear Sucker Green Sunfish, Sunfish, Other Brown Trout, Rainbow Trout, Alapaha River Alapahoochee River Allatoona Crk. (Cobb Co.) Altamaha River Altamaha River (below US Route 25) Apalachee River Beaver Crk. (Taylor Co.) Brier Crk. (Burke Co.) Canoochee River (Hwy 192 to Lotts Crk.) Canoochee River (Lotts Crk. to Ogeechee River) Casey Canal Chattahoochee River (Helen to Lk. Lanier) (Buford Dam to Morgan Falls Dam) (Morgan Falls Dam to Peachtree Crk.) * (Peachtree Crk. to Pea Crk.) * (Pea Crk. to West Point Lk., below Franklin) * (West Point dam to I-85) (Oliver Dam to Upatoi Crk.) Chattooga River (NE Georgia, Rabun County) Chestatee River (below Tesnatee Riv.) Chickamauga Crk. (West) Cohulla Crk. (Whitfield Co.) Conasauga River (below Stateline) <18" Coosa River <20" 18 –32" (River Mile Zero to Hwy 100, Floyd Co.) ≥20" >32" <18" Coosa River <20" 18 –32" (Hwy 100 to Stateline, Floyd Co.) ≥20" >32" Coosa River (Coosa, Etowah below <20" Thompson-Weinman dam, Oostanaula) ≥20" Coosawattee River (below Carters) Etowah River (Dawson Co.) Etowah River (above Lake Allatoona) Etowah River (below Lake Allatoona dam) Flint River (Spalding/Fayette Cos.) Flint River (Meriwether/Upson/Pike Cos.) Flint River (Taylor Co.) Flint River (Macon/Dooly/Worth/Lee Cos.) <16" Flint River (Dougherty/Baker Mitchell Cos.) 16–30" >30" Gum Crk. -
LIDAR Accuracy Assessment Report – Jackson County
LIDAR Accuracy Assessment Report – Jackson County Jackson County, Little Tennessee River and Savannah River Basins The LIDAR accuracy assessment for Jackson County was performed in accordance with section 1.5 of the Guidelines for Digital Elevation Data, Version 1.0, published by the National Digital Elevation Program (NDEP), see www.ndep.gov. The NDEP specifies the mandatory determination of Fundamental Vertical Accuracy (FVA) and the optional determination of Supplemental Vertical Accuracy (SVA) and/or Consolidated Vertical Accuracy (CVA). Consistent also with Appendix A, Aerial Mapping and Surveying, of the Federal Emergency Management Agency‘s (FEMA's) Guidelines and Specifications for Flood Hazard Mapping Partners, the North Carolina Floodplain Mapping Program (NCFMP) established mandatory acceptance standards for Fundamental and Consolidated Vertical Accuracy, utilizing five land cover categories listed in Table 1 below. FVA is determined with check points located only in open terrain (grass, dirt, sand, and/or rocks) where there is a very high probability that the LIDAR sensor will have detected the bare-earth ground surface and where random errors are expected to follow a normal error distribution. With a normal error distribution, the vertical accuracy at the 95% confidence level is computed as the vertical root mean square error (RMSEZ) of the checkpoints x 1.9600, as specified in Appendix 3-A of the National Standard for Spatial Data Accuracy (NSSDA), FGDC-STD-007.3-1998, see www.fgdc.gov/standards/status/sub1_3.html. For the current Phase III of the North Carolina Floodplain Mapping Program (NCFMP), the FVA standard is 1.19 feet (ft) at the 95% confidence level, equivalent to the accuracy expected from 2 ft contours.