Document 15635991

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Presentation Outline
• Meet Our Team
• The Tools We Used
• The Peeper Pond
• In the Field
• The River and
Beach
• Lookout Point
• In the Woods
• Big Bedrock
Paul
Elissa
Jessie
Katherine
Jenny
Andrea
Gill
Brendyl
Ann
Kim
Ellen
Angela
Alex
Mike
James
Jason
Tripod with Auto-level
Stadia Rod (Surveying Rod)
Conductivity Meter
Velocity Meter
pH Tester
Munsell Soil
Chart
Spades
Tarp
Shovels
And Now
Let’s Hit the
Trail….
Our Tasks
Measure
the
Measure
the
Percent
Take
a
GPS
reading
Measure
Measure
Air
pH
and
Level
Water
of
Conductivity
of
the
Saturation
of
and Locate Our
Temperatures
theWater
Water
Dissolved
in
Position onOxygen
the Map
the Water
Measuring Air and Water
Temperature
Our Results on Monday July 2, 2001:
Air Temperature 16˚c
Water Temperature 19˚c
Measuring the pH
Level of the Water
Our Results on Monday July 2, 2001:
pH of Water - 7.5
pH
of Milk
= 6.6
of Grapefruit
= 3.4 = 3.3
pH ofpH
Mellow
Yellow
Soda
Measuring the
Conductivity of the Water
Conductivity of
Conductivity
of Milk=
Soda=
4.65uS
0.51uS
Conductivity
of Grapefruit=
2.52uS
Our Results on Monday July 2, 2001:
Conductivity of the Water 165uS
Measuring the Percent
Saturation of Dissolved
Oxygen in the Water
Our Results on Monday July 2, 2001:
66% Saturation
Take a GPS Reading and
Locate it on the Map
Our Results on Monday July 2, 2001:
Position: 18T 0659877
UTM 4912466
What can we learn about this
field from the soil pit?
Use of
plows
evident in
the A-layer
Evidence
of
vegetation
Rocks and sand at
the bottom of the
pit indicate that
this land was once
part of the
Huntington River
Clean-Up Time!
BMI stands for...
Benthic - Bottom-Dwelling
Macro - Large
Invertebrates - Spineless Creatures
Collecting Samples
What We Found
Stonefly
Mayfly
Also:
Caddisflies
Midge
Dragonflies
Aquatic Worms
Boulders
• Brought here by The
Glacier
• Very difficult for the
river to move
• They are Shaped by
the river
River Terraces
• Flat and Long
• Separated by steep
slopes
• Sand and gravel not
far below the soil
Lookout point provides you with a
view of two very basic characteristics
of a river; a cut bank and a point bar.
A Cut Bank is on the outside of a river
bend.
A Point Bar is located on the inside of a river
bend.
Bedrock is the solid rock that is under
gravel, soil, and other material.
It is exposed on the Earth’s surface
through a combination of faulting
and erosion.
Folds in the bedrock are caused by
pressure, heat, and stress.
Foliation
• Strike Measurements
• Dip Measurements
And
everyone
else
who
Christine
Paul,
The
Katherine
Allison
Private
State
Elissa,
of
AllAnd
of
our
Families
And
all
of
the
other
Also
Of
course
helped
to
make
this
Contributors
Vermont
and
Friends
staff
members
Jessiepossible
experience
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