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MiCorps Stream Data Description
Sampling Event Description
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Date Sampled: Date the
sample was collected. Record the month, day and year.
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Start Time: Time
sampling began.
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Finish Time: Time
sampling was completed.
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Datasheet Completed by: Name of the person in charge of filling out the datasheet.
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Collector: For macroinvertebrate collections, name of the person in the water collecting the macroinvertebrate samples.
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Other Team Members: Names of other people collecting
stream monitoring data at this site.
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Datasheet Checked by: Individual who check the datasheet
for completeness before turning it in.
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Entered into Database by: Person who entered the data into
the MiCorps online database.
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Identification made by: Name of expert who identified macroinvertebrates.
Sampling Location
- Stream Name: The waterbody
name should be the name of the river or river branch, as given
on the U.S. Geological Survey topographic map for the area corresponding
to the station location. For tributary streams to major rivers,
record the tributary stream name here, not the major river name.
For instance, if the stream being surveyed is the North Branch
of the Chippewa River, but the station is on Hogg Creek, record
Hogg Creek as the waterbody name. If the tributary is an unnamed
tributary, record as “Unnamed Tributary to” followed by the name
of the next named stream downstream. In the above example, a
station on an unnamed tributary of Hogg Creek would be recorded
as “Unnamed Tributary to Hogg Creek”. These
names can be found at www.topozone.com.
- Location/Site Description: Record
the name of the road crossing the stream. If the same road crosses
a single stream two or more times in the same sub-basin, it is sometimes
desirable to record the road name relative to the nearest crossroads
(e.g. “Green Road between Brown Road and Hill Road”).
If the same road crosses a single stream two or more times in the
same township section, record the road name relative to the distance
from the nearest crossroad (e.g. “Green Road 1/8 mile east
of Brown Road ”).
- MiCorps Site ID #: If you don't already have it, contact MiCorps staff for the MiCorps Site ID# for your sampling location.
- Upstream/Downstream of Road: This
category is on the Single Site Watershed Survey Data Sheet only.
The “single site” sheet is designed primarily for use
by those groups participating in the Division’s volunteer
monitoring program and it includes only enough response categories
for assessing one side of a stream crossing. If using this data
sheet, circle either Upstream Side or Downstream Side, as appropriate,
to designate which side of the stream crossing is being assessed.
- County: Record county name.
- Township Name: This indicates
the township from which the sample was collected.
- Township Number: This indicates
the township from which the sample was collected.
- Range: This indicates the range
of the township from which the sample was collected.
- Section: This indicates the section
of the township from which the sample was collected.
- Quarter: This indicates the quarter
of the township from which the sample was collected.
- Quarter Quarter: This indicates
the quarter quarter of the township from which the sample was collected.
- Watershed/Hydrologic Unit Code (HUC): This
indicates the watershed or USGS 8-digit Hydrologic Unit Code (HUC) from which
the sample was collected. A system for
identifying and numbering watersheds has been developed in
the U.S. by the USGS.
Through this system all U.S. watersheds have a proper name
and a corresponding number called a Hydrologic Unit Code (HUC).
To locate your watershed visit EPA's Surf
Your Watershed.
- Geographic Coordinates:Latitude and longitude
are collected to determine exactly where on a lake a sample was taken. Latitude
measures the position north
and south and longitude measures the position east and west. Latitude
and longitude can be collected using a Global Positioning System (GPS) or
can
be estimated at www.topozone.com.
Common formats are below.
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Decimal Degrees: An example of this
format is Latitude = 42.6817549; Longitude = -85.898463.
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Decimal Minutes: An example of this
format is Latitude = 42° 40.905294'; Longitude = -85° 53.907786'.
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Degree, Minutes, Seconds: An example
of this format is Latitude = 42° 40' 54''; Longitude = -85° 53'
55''.
- Map Scale: If a map is used to determine
latitude/longitude coordinates, record the scale of measurement (e.g. 1:25,000)
if known.
- Datum: Geodetic datums define
the size and shape of the earth and the origin and orientation of the
coordinate systems used to map the earth. This information
is directly associated with the latitude and longitude number and can be
found on the GPS unit or on www.topozone.com associated
with the latitude and longitude.
- Coordinate Determination Method: Check the
method used to calculate the latitude/longitude location coordinates.
- Length of stream assessed: How long of a section
of the stream was sampled.
Background Information
- Storm Event Conditions: A stream “event” occurs
when water runoff from a significant weather event, such as a
major rainstorm or fast snowmelt, causes an increase in river
flow. Circle the appropriate description of event conditions
exhibited in the stream. Event conditions are increased river
flow above what would be considered typical or normal for the
stream for the time of year.
- Days Since Rain: Circle the appropriate
number of days that have passed since the last significant rain ended.
This information is based on what you know about recent weather in the
vicinity of the site. If you do not know, circle “unknown”.
- Water Temperature: This is an optional
data item. The person coordinating a particular watershed survey will
determine if temperature measurements will be made. If measured, record
the water temperature to the nearest degree fahrenheit or centigrade,
making sure to include the scale units.
- Dissolved Oxygen: This is an optional
data item. The person coordinating a particular watershed survey will
determine if dissolved oxygen (DO) measurements will be made. If measured,
record the DO level in the river. If DO is measured, it is important that
the water temperature be measured also.
- pH: This is an optional data item.
The person coordinating a particular watershed survey will determine if
pH measurements will be made. If measured, record the pH of the stream
to the nearest tenth.
- Water Color: Circle the choice that
best represents the color of the water.
- Water Body Type - Upstream: Characterize
the waterbody upstream of the road crossing and circle the appropriate
category. Impd=impoundment.
- Water Body Type - Downstream: Characterize
the waterbody downstream of the road crossing and circle the
appropriate category. Impd=impoundment.
- Stream Width (feet): Circle the range
that represents the average stream width in feet. Make this observation
using best professional judgement of the distance. This can be done by
pacing off the distance (counting the number of steps taken) on the road
crossing from one edge of the stream to the other. There is no need to
measure the distance with a tape measure or similar device, however, it
is best to have previously paced off distances of 10, 25 and 50 feet so
that the number of strides is known to these category endpoints.
- Average Stream Depth (feet): Circle
the appropriate depth range in feet. If the water is turbid and the depth
cannot be determined, circle “Unknown”. This observation is
for the average depth of the stream that is consistently observed. In
other words, if the stream is mostly shallow, but is 5ft deep in the channel,
the >3ft category should be circled. However, if the stream is generally
shallow (<1ft), but has a pool that is 3ft deep, circle the <1ft
category since a pool is not representative of the average depth of <1ft
observed over most of the stream. Remember that water often looks shallower
than it is. The primary purpose of this data observation is to identify
sites that would be suitable for wading for potential future instream
assessments.
- Water Velocity (feet/second): This is
an optional data item. The person coordinating a particular watershed
survey will determine if water velocity measurements will be made. If
measured, record the approximate surface water velocity in feet per second,
observed at the surface in the area of fastest river flow that is not
impacted by the road crossing. The preferred method is to observe how
far downstream surface bubbles, foam, leaves, or other floating objects,
travel in one second (or observe for 10 seconds and divide the distance
by 10). Another method is to step off the width of the road, time how
long it takes a particular object (e.g. leaf, stick, grass blade) to float
from the upstream side of the bridge to the downstream side, and divide
the number of seconds into the distance to get feet per second. In some
cases, the water velocity measured at the road crossing will not accurately
represent actual stream velocity. This may occur at road crossings where
the river width is abnormally restricted by the size of passage beneath
the road (such is often the case with culverts), which can cause faster
flow through the culvert than is observed in the stream. In such a case,
it is better to measure water velocity further upstream or downstream
(by looking further upstream or downstream from the bridge, not by going
to a different location), if possible.
- Stream Flow Type: Circle the category
that best represents general flow volume in the stream. Note that in this
case, “average” flow refers to the annual average flow. If
a river flow is reduced in the summer, due to dry and hot conditions,
circle “L” because it is below average, even though low flow
may be typical for that stream in the summer.
Physical Appearance
- Aquatic Plants: This category
refers to aquatic macrophytes only, not terrestrial species.
By definition, macrophytes are any plant species that can be
readily seen without the use of optical magnification. However,
the usage here is directed primarily toward aquatic vascular
plants—plants with a vascular system that typically includes
roots, stems and/or leaves. This includes duckweed, as it is
a floating vascular plant. Certain large algae species that superficially
look like vascular plants, such as Chara, can be recorded here
as well. If the person conducting the survey is knowledgeable
about aquatic plants, the particular type or species of plant(s)
can be noted in the comment section at the end of the form. Floating,
suspended, or filamentous algae species should be recorded in
one of the algae categories and not here.
- Floating Algae: The presence of suspended
algae (single celled organisms that may or may not form colonies) or floating
algae mats/bundles should be recorded here. This includes bluegreen algae
mats/bundles, whether floating on the surface, suspended in the water
column, or present at the bottom.
- Filamentous Algae: Algae that appear
in stringy or ropy strands, such as Cladophora. The strands may or may
not be attached to other objects in the waterbody.
- Bacterial Sheen/Slime: Bacterial sheens
occur as oily appearing sheens on the water surface, often with
a silverish cast to them. The sheens are produced from bacterial
decomposition activity,
and occur most often in still water areas of lake edges and coves,
as well as wetland areas. The sheen can be distinguished from
petroleum products
by breaking into distinct platelets when poked with a stick or
otherwise physically disturbed, whereas petroleum products remain
viscous. Bacterial slimes are bacterial growths that are visible as a
slimy-appearing coating of stream or lake substrates. They can
be various colors, including black and orange.
- Turbidity: Water appears cloudy—it
is not transparent. Turbidity is caused by suspended particulates such
as silt, sand, algae, or fine organic matter. Turbid water is opaque to
varying degrees, preventing the observer from seeing very far into it.
Note that water can have a color to it that is not turbidity, such as
the brown transparent water often associated with swampy areas. If the
water is slightly turbid, circle “present”. If it is moderately
turbid to very turbid, circle “abundant”.
- Oil Sheen: An oily appearing sheen on
the water surface caused by petroleum products. A thin sheen will often
have a rainbow of hues visible. The sheen can be distinguished from bacterial
sheens by remaining viscous when poked with a stick or otherwise physically
disturbed, whereas bacterial sheens break into distinct platelets.
- Foam: Naturally occurring foam often
looks like soap suds on the water surface and can be white, grayish or
brownish. Foam is produced when water with dissolved organic material
is aerated and can range in extent from individual bubbles to mats several
feet high. Foam is typically produced in streams when water flows through
rapids or past surface obstructions such as logs, sticks and rocks. Simple
wave action can produce foam in lakes. This naturally occurring foam is
quite common. Natural foam can be distinguished from soap suds by rubbing
it between ones fingers. If the suds disintegrate and leave only wet fingers
or a gritty residue, the foam is natural. If the suds feel slippery and
soapy, it is not natural foam.
- Trash: Use this category to record the
presence of general litter, such as paper, bottles, cans, etc., either
in the waterbody or along the riparian banks. Use some reasonable discretion
when completing this category. A single piece of gum wrapper on one bank
would not be sufficient cause for checking “present”.
Substrate
Identify the percent areal extent of each substrate type
present. Round off to the nearest 10% increment. For example, do
not record 25%, use either 20% or 30%.
- Boulder - 10" diameter:
Rocks 10 inches in diameter or larger.
- Cobble/Gravel - 0.08" to 10" diameter:
Rocks 1/12 inch to 10 inches in diameter.
- Sand - coarse grain: Rocks 0.06 to 2 millimeters in
diameter.
- Silt/Detritus/Muck - fine grain/organic matter: Silt
is usually clay, very fine sands, or organic soils, 0.004 to
0.06 millimeters in diameter. Muck is decomposing organic material of
very fine diameter.
Detritus is small particles of organic material such as pieces
of leaves, sticks, and plants.
- Hardpan/Bedrock - solid clay/rock surface: Solid surface.
Hardpan is usually packed clay, <0.004 millimeters in diameter. Bedrock
is a solid rock surface (the tops of buried boulders are not bedrock).
- Artificial - manmade: Human made, such as concrete
piers, sheet piling or rock riprap (that portion of shoreline erosion
protection structures that extends below the water surface is considered
substrate).
- Unknown: The portion of the stream bottom for which
a substrate type determination can not be made because the bottom can
not be seen due to water depth or turbidity.
Instream Cover
Instream cover generally refers to habitat cover that is available to fish to: (1) protect them from predators, or (2) avoid certain stream conditions such as fast flow velocities or direct sunlight. Check all the instream cover types on the data form that are present in the stream reach for as far as can be seen—except, only check those cover types that are in areas of sufficient water depth (usually greater than 6 inches).
- Undercut Banks: Stream banks
that overhang the stream because water has eroded some of the
material beneath them.
- Overhanging Vegetation: Terrestrial vegetation that
extends out from shore over the surface of the stream within
a foot or two of the water surface (includes trees, shrubs, grasses,
etc.).
This category also includes sweeping vegetation, which is terrestrial
shoreline vegetation that extends into the water itself (such
as low hanging branches on shrubs) and is therefore often “swept” in
a downstream direction by the current .
- Deep Pools: depression or “hole” in the
bottom of the stream where the water is substantially deeper than the
average water depth of the stream.
- Boudlers: Rocks 10 inches in diameter or larger.
- Aquatic Plants: Aquatic macrophytes.
- Logs or Woody Debris: Logs, branches and roots.
River Morphology
- Riffle: Riffles are areas of
naturally occurring, short, relatively shallow, zones of fast
moving water followed by a pool. The water surface is visibly
broken (often by small standing waves) and the river bottom is
normally made up of gravel, rubble and/or boulders. Riffles are
not normally visible at high water and may be difficult to identify
in large rivers. The size of, and distance between, riffles is
related to stream size. In large mainstream reaches, such as
the Manistee or Muskegon rivers, riffles may be present in the
form of rapids.
- Pool: Pools are areas of relatively
deep, slow moving water. The key word here is “relatively”.
Water depth sufficient to classify an area as a pool can vary from around
8 inches in small streams, to several feet in wadable streams, to tens
of feet in large rivers. Pools are often located on the outside bend of
a river channel and downstream of a riffle zone or obstruction. The water
surface of a pool is relatively flat and unbroken. The presence of pools
in large rivers may be difficult to identify because of an increase in
relative scale, and an often limited ability to see to the bottom of deep
or turbid stream reaches.
- Channel: Natural Stream - A natural
stream has not been altered from its defined pattern, dimension
and profile by artificial means, which includes straightening and widening.
It is
not necessarily stable, however. The stream has a non-uniform
cross section with distinct pool and riffle sequences, although in large
rivers the
pool/riffle sequences may be difficult to identify. Mild to extreme
meanders are often visible. The banks are vegetated and there are no signs
of spoil
piles or dikes along sides. The stream is not channelized or
artificially controlled. Recovering - A recovering stream is one that
has been straightened or otherwise controlled, and is evolving back to
a stable pattern, dimension and profile. The stream channel is relatively
straight, or is overly wide with a channel within the wider channel. Meanders
may be beginning to form as evidenced by bank erosion and pool formation.
Pools and riffles should be forming but may be sparse. Point bars may
be forming. Vegetation may be sparse or very young. Defined dikes or spoil
piles along the stream bank can be identified. Maintained - A maintained
stream channel is one that is actively controlled through dredging, widening,
straightening, or the formation of dikes along the stream channel. The
stream channel is straight, wide and shallow at low flow, and has a uniform
cross section. Bank vegetation is typically sparse or very young. Pools
and Riffles are not existent or very sparse.
- Designated Drain: If the surveyor knows
whether or not the stream segment being assessed is a legally designated
drain under the Michigan Drain Code, circle “Y” (yes) or “N” (no).
If the surveyor does not know, circle the “?”.
- Highest Water Mark: The highest water
mark is the maximum height to which the stream water level rises at the
site, as determined by the visible evidence present. This level is typically
reached during floods or high flow conditions. The highest water mark
is determined as the distance in feet above the present water level at
the site. If the surveyor cannot visibly determine how far the stream
rises at the site, circle the “?” on the form.
The highest water mark may be visible as discoloration on
bridge pilings or abutments, stream debris (trash, leaves,
weeds) left along the stream banks or in tree/shrub branches,
ice scour marks on trees or streambanks, or muddy residues
left in floodplains or on streamside vegetation.
Stream Corridor
- Riparian Vegetative Width - Left:
The riparian vegetative width is the width of the streamside
natural vegetation zone along the stream banks. The width is
measured from the edge of the stream to the end of the contiguous
block of natural vegetation. Natural vegetation is defined as
including trees, shrubs, old fields, wetlands, or planted vegetative
buffer strips (often used in agricultural areas and stormwater
runoff control). Agricultural crop land and lawns are not considered
natural vegetation for the purposes of this question. Circle
the appropriate distance (in feet) that represents the average,
or most representative (>50% of the lineal bank distance)
width of the vegetation zone for each side of the river. Left
and right banks are determined from the perspective of facing
downstream.
- Riparian Vegetative Width - Right: See
above.
- Bank Erosion: Determine the severity
of erosion that has taken place and circle the appropriate category. Record
the most severe magnitude of erosion observed on either bank.
- Streamside Land Cover: Circle the letter
of the dominant type of cover that exists at the streambank “edge” (within
the first 20 feet or so of the stream edge) along the reach of river that
can be seen from the road stream crossing.
- Stream Canopy %: The stream canopy is
the amount of leafy vegetation that extends out over a stream (at any
height) and shades the water from direct sunlight. The amount of stream
canopy should be recorded as the amount of water shading that would be
present if the sun were directly over the stream.
Adjacent Land Uses
Circle the appropriate left or right streambank designation for all of the following land uses that are adjacent to the stream. Land use along the entire length of stream that can be seen from the road stream crossing should be evaluated. This might include land that is beyond the riparian corridor. “Adjacent” requires the use of some judgement on the part of the surveyor, but generally refers to any land that can be seen from the crossing and is reasonably close to the stream such that pollutants could run off it into the stream. For example, if a 20-acre corn field is near a stream but separated from it by a 10’ grass/shrub buffer strip, the “Rowcrop” category should be circled. If the same field were 100’ from the stream and the intervening distance was wooded, the “Forest” category should be circled.
- Wetlands: Wetland vegetation
is present. May or may not include standing water. Could include
shrubs and trees.
- Shrub or Old Field: Meadow or field
that has not been recently cultivated or grazed. Often represented by
tall grasses and shrubs.
- Forest: Trees present in forested setting
(includes small woodlots). Trees may be cultivated or natural.
- Pasture: Field showing signs of being
recently or actively grazed by livestock (vegetation is cropped close
to the ground).
- Crop Residue: An agricultural crop residue
remains, after harvest and/or tillage, which covers 30% or more of the
field surface.
- Rowcrop: Agricultural cropland planted
in rows and cultivated.
- Residential Lawns or Parks: An expanse
of maintained grass, often found in residential lawns and parks.
- Impervious Surfaces: Impervious surfaces
(water can not penetrate them) are present near the water. Includes paved
surfaces and roofs.
- Disturbed Ground: Soil has been disturbed
(plowed, cleared, bulldozed, excavated) for construction or agriculture.
Vegetation is not present on disturbed ground but may be present in adjacent
areas.
- No Vegetation: Bare ground. No vegetation
is present on the soil, but it is not disturbed ground.
Potential Sources
The intent of this section is to evaluate the relative importance of potential sources in terms of pollutant contribution to the waterbody at a given site in the watershed. The evaluation assesses the potential for pollutant inputs at the site, NOT pollutant impacts, or the potential for pollutant impacts.
- Crop Related Sources: There
is a reasonably clear pathway for pollutants to enter the waterbody
from the farmed area. Possible pathways: farming to the edge
of the drain, gully/rill erosion off field, tile discharge, wind
erosion off field.
- Grazing Related Sources: There
is clear evidence that grazing of animals near or in the waterbody
has resulted in the degradation of streambanks or stream beds,
sedimentation, nutrient enrichment, and/or potential bacterial
contamination.
- Intensive Animal Feeding Operations:
There is a reasonably clear pathway for pollutants to enter the
waterbody from either runoff from the operation or land application of
animal manure. Possible pathways: overland flow, tile discharge.
- Highway/Road/Bridge Maintenance and Runoff (Transportation
NPS): There is clear evidence that transportation infrastructure
is creating increased flow, runoff of pollutants, or erosion
areas in or adjacent to the waterbody.
- Channelization: There is clear
evidence that the natural river channel has been straightened
to facilitate drainage.
- Dredging: There is clear evidence
that a waterbody has been recently dredged. Evidence might include:
spoil piles on side of waterbody, disturbed bottom, disturbed
banks.
- Removal of Riparian Vegetation: There
is clear evidence that vegetation along the waterbody has been
recently removed (within the last few years).
- Bank and Shoreline Erosion/Modification/Destruction:
There is clear evidence that the banks or shoreline of a waterbody
have been modified through either through human activities or
natural erosion processes.
- Flow Regulation/Modification (Hydrology):
There is reasonably clear evidence that flow modifications in
the watershed have created unstable flows resulting in streambank erosion.
- Upstream Impoundment: There
is reasonably clear evidence that an upstream impoundment has
contributed to impacts on downstream sites. Impacts may be: nuisance
algae, increased
temperatures, streambank erosion from unstable flows.
- Construction: Highway/Road/Bridge/Culvert:
There is clear evidence that on going or recent construction
of transportation infrastructure is contributing pollutants to the waterbody.
- Construction: Land Development: There
is clear evidence that on going or recent land development is
contributing pollutants to the waterbody.
- Urban Runoff (Residential/Urban NPS):
There is a reasonably clear pathway for pollutants to enter the
waterbody from an urban/residential area. Possible pathways:
gully/rill erosion,
pipe/storm sewer discharge, wind erosion, runoff from lawns or
impervious surfaces.
- Land Disposal: There is a reasonably
clear pathway for pollutants to enter the waterbody from an area
where waste materials (trash, septage, hazardous waste, etc.)
have been either
land applied or dumped. Possible pathways: gully/rill erosion,
pipe discharge, wind erosion, or direct runoff.
- On-site Wastewater Systems: There is
reasonably clear evidence of nutrient enrichment and/or sewage
odor is present, and there is reason to believe the area is unsewered.
- Silviculture (Forestry NPS): There is
a reasonably clear pathway for pollutants to enter the waterbody
from the forest management area. Possible pathways: logging to
the edge of
the waterbody, gully/rill erosion off site, pumped drainage,
erosion from logging roads, wind erosion off site.
- Resources Extraction (Mining NPS): There
is a reasonably clear pathway for pollutants to enter the waterbody
from the mined area. Possible pathways: gully/rill erosion off
site, pumped drainage, runoff from mine tailings, wind erosion off site.
- Recreational/Tourism Activities (general):
Foot traffic
causing
erosion would fall into this category.
- Golf Courses: There is a reasonably
clear pathway for pollutants to enter the waterbody from the
golf course area. Possible pathways: overland runoff, gully/rill
erosion off course,
tile discharge, wind erosion off course.
- Marinas/Recreational Boating (water releases):
If you can reasonably determine that releases of pollutants to
a waterbody such as septage or oil/gasoline are due to recreational
boating activities.
- Marinas/Recreational Boating (bank or shoreline
erosion): You can reasonably determine that streambank erosion
is due to wake from recreational boating activities.
- Debris in Water: Debris in the water
either is discharging a potential pollutant, or is causing in
stream impacts due to modifications of flow. Possible examples:
Leaking barrel, Refrigerator,
Tires, etc. This does not include general litter (e.g. paper products).
- Industrial Point Sources: There is reasonably
clear evidence that an upstream industrial point source has contributed
pollutants.
- Municipal Point Sources: There is reasonably
clear evidence that an upstream municipal point source has contributed
pollutants.
- Natural Sources: There is reasonably
clear evidence that natural sources are contributing pollutants.
Possible examples: streambank erosion, pollen, foam, etc.
- Source(s) Unknown: If you see an impact
but are unable to clearly identify any likely sources.
Additional Comments
Any observations about the site that were not covered elsewhere on the survey form should be recorded in this section.
Macroinvertebrate Collection Stream Conditions
- Average Water Depth: Average
depth of stream during data collection.
- Is substrate covered with excessive silt:
Record whether there is an excessive amount of silt covering
substrate.
- Substrate Embeddedness in Riffles: What
percentage of substrate embeddedness in riffles.
- Did you observe any fish or wildlife:
Note any fish and wildlife seen in the stream.
Macroinvertebrate Collection
- Check all habitats that were sampled:
Identify all habitats that were sampled at the site during data
collection.
- Did you see any live crayfish: Were any
live crafish found at site.
- Did you see any large clams: Were any
large clams found at site.
Identification and Assessment
- Group 1 - 3: Next to each taxa record if rare (R = 1-10) or common (C = 11 or more) in
stream. Leave blank if no members of taxa were recorded.
- Rate your confidence in these identifications:
How confident are you in the identifications.
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