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What are the impacts of human activities on the environment
The impact of human activities on the environment
What are the impacts of human activities on the environment
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ABSTRACT
What is the water quality in Covington Creek, Soos Creek, Jenkins Creek, Jenkins Pond Creek, and Jenkins Pond? Does the water quality meet or exceed the Washington State water quality criteria?
Several parameters were sampled at each sample site. The sampled parameters at each creek and pond site were temperature, dissolved oxygen (DO), pH, discharge, bank stability, and vegetation plots. Tests for the presence of nitrates and phosphates were also conducted. In addition to these tests, samples of benthic macroinvertebrates were collected.
The results for each test and each sample site exceeded the minimum criteria set by the Washington State Department of Ecology. However there are many steps that can be taken to insure the future quality of these creeks and ponds.
Introduction
Creek and pond reach assessments were sampled for Covington Creek, Soos Creek, Jenkins Creek, Jenkins Pond Creek, and Jenkins Pond. The location of Covington Creek is Sec.18T21NR6E. The date of the assessment was February 8, 2010, and the weather was clear with a temperature of 57 degrees. The location of Jenkins Pond is Sec.30T22NR6E. The date of the assessment was February 22, 2010. The weather was dry and sunny with a temperature of 64 degrees. The Location of the Jenkins Pond Cree is Sec.30T22NR6E. The date of this assessment was March 1, 2010 and the weather was overcast skies with a temperature of 57 degrees. The final assessment was Soos Creek and is located at Sec.16T21NR5E. The date of this assessment was March 1, 2010. The weather was overcast skies with a temperature of 60 degrees. All of these locations are located in King County and all streams and ponds are within the Green-Duwamish watershed.
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...re measured using a densimeter. The herbaceous and woody percent coverage of the plot was also recorded.
For each stream reach four cross sections were also sampled. At each cross section the samplers performed a heel to toe test to check the consistency of the streams substrate. This test is performed by walking heel to toe accros the creek and picking up everything under the samplers toes. The results of the substrate were averaged by using a code silt=1, sand=2, gravel=3, cobble=4, and boulder=5. The samplers measured the width of the creek and the ordinary high water mark (OHWM). The samplers determined the amount of shade on the creek at each cross section.
Works Cited
-ept of ecology publication number -
www.ec.wa.gov/programs/wq/swqs/criteria-freshwater.wac173201a_200-temp.html
greenkingcounty.gov/wlr/waterres/streamsdata/watershedinfo.aspx?locator=A320
Hägglund, Å., & Sjöberg, G. (1999). Effedts of beaver dams on the fish fauna of the forest streams. Forestry Ecology and Management, 115, 259-266.
To achieve a lifestyle in which you are happy and at peace, you must break away from your social setting and truly experience life in the simplest form.
Fish habitat is the underwater world which many people do not see. It is just like the world that people live. Fish and plants reproduce, eat, and live in this environment, and even face challenges such as invasive species. It is said that “Invasive species are non-native species that threaten the diversity or abundance of native species due to their uncontrollable population growth, causing ecological or economic impacts” (“Invasive” par. 1). Vegetation plays a big role for fish habitat and for a lake itself. Aquatic habitat provides living space for not only fish but also for many aquatic insects. These insects then in turn provide fish and other species of animals with food (“Native” par. 4).
This report is to see the effects of stream erosion and transportation of sediment caused by running water in the North Fork Cosumnes River California. The field repot was conducted on July 9, 2014 by Joel Morsey and John Morsey. I chose this location because I used to go there with my family when I was younger to swim in the river. I was interested to see how low the river was, because of the drought California has been having and to see the effects of erosion in more detail because the water would be much lower.
For almost two centuries the TSW, in dealing with public pressure, has pointed to its original mandate. The concern is that in doing so it fails to recognize that increasingly, the entire waterway is an expanding recreation base, which not only requires water for navigation but also requires an equitable supply of water to support recreational uses and to maintain and enhance the natural environment. The TSW, although maintaining their original position, has over the years made provision for “new” uses of water including diverting vast amounts to white water canoeing events, water filtrations plants and increased municipal uses. Clearly times have changed and the TSW must recognize that it must adapt through not only a change of mandate but also a change of governance that would recognize and better co-ordinate the vast amount of stakeholders within the system.
Bibliography Laws, Edward A. Aquatic Pollution. 2nd edition. New York: John Wiley and Sons, Inc. 1993. Pg. 301-305. Adams, Aurthur G. The Hudson Through the Years. New Jersey: Lind Publications, 1983. ------------------------. The Hudson: A Guide to the River. Albany: State University of New York Press, 1981. Barnthouse, Lawrence W. Science, Law, and the Hudson River WWW.SCENICHUDSON.ORG WWW.HUDSONRIVER.ORG WWW.RIVERKEEPER.ORG
USGS. "Water Resources Inventory Area 1 Watershed Management." USGS Science for a Changing World. U.S. Geological Survey , 18 Jun 2013. Web. 7 Apr 2014. .
The southern parts of Canada rely on water that rivers such as The Bow, Red Deer, and Northern Saskatchewan provided to many sectors of society. The water budget for these particular rivers are based from mountain headwaters; therefore, runoff and snowmelt are vital with respect to preservation among these rivers (Prowse and Conly, 1998). A study conducted in 1951-1993 Hopkinson and Young (1998) concluded ice erosion, not including snow melt, contributed to 1.8% of emission into the Bow River. These results were based on examining volume fluctuations in an upstream lake. Although this sum seems extraneous the benefaction is indispensable. Due to climatic temperature changes, glacier area has decreased and as a result, the Bow River is not receiving
Great Lakes Regional Pollution Prevention Roundtable. GLRPPR, 12 Dec. 2013. Web. 15 Dec. 2013. .
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States can use watershed planning to help simplify the wetlands regulatory program in several ways. First, Advanced Identifications or similar watershed
To measure the cross-section you will need to find the width of the river first. To do this, you will need to stretch a tape measure from one bank to the other at a 90° from the course of the river. Measure from where the dry banks touch the water. Once you have found the width of the river, your next job is to find the depth of the the river (across the width). The more detail you want, the more readings you will need to take. An example of a good interval would be 50 cm but it also depends on the width of the river. Leave the tape measure where it was when you measured the width to ensure you a straight line which can help you to measure the depth. It will also help you measure the distance between each
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Satterlund, D.R. and Adams, P.W. 1992. Wildland Watershed Management. John Wiley and Sons, Inc. New York.
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