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Volume
7, Number 4,
May 1961:
The
F.B. and Rena G. Ross
Natural History Reservation
Text-only version

ISSUE
HOME PAGE
ABOUT
THIS ISSUE
IN THIS
ISSUE
- Introduction
- History of the
Area
- Description
of the Area
- Aerial Photograph
- Accumulation of Field
Data
- Weather
- Conservation
Practices
- Animals of the
Reservation
- Nature Trail
- Cover Picture
- Ross Message
SLIDESHOW
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images in this issue.
This
page was last modified:
February 24, 2008
This
page was originally posted:
June
14, 2005
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The
F.B. and Rena G. Ross Natural History Reservation
by
John Breukelman, Thomas A. Eddy and Emily L. Hartman


Figure
17
Nature
Trail
Many
days would be required for a visitor to see and learn the
complex interrelationships of habitats, plants, and animals
on the Reservation. He might study for weeks its many acres
of upland prairie and associated wooded ravines, thickets,
and aquatic habitats.
Not
many visitors can spend days or weeks, so a nature trail
is being established to enable the interested student to
see representative communities of plants and animals found
on the prairie of eastern Kansas. An hour or two spent on
this trail is enough for a brief glimpse of the life on
the vast prairie.
The
nature trail leads to eight stations on the prairie which
represent rather distinct assemblages of living things.
The communities, named after the dominant plants that occur
in the selected areas, are shown on the aerial photo on
page 9.
If you
are planning a visit, write the Ross Natural History Reservation
Committee, Department of Biology, Kansas State Teachers
College, Emporia, Kansas, asking for an application form
for a guided field trip. All field trips within the Reservation
are supervised by personnel of the Department of Biology.
Anyone
interested in a more technical description of the natural
history and geology of the area may receive a copy of The
F.B. and Rena G. Ross Natural History Reservation, by
Emily L. Hartman. This was published as Volume 8, Number
4, of The Emporia State Research Studies, June 1960;
it may be obtained by writing Thomas A. Eddy, Department
of Biology, Kansas State Teachers College, Emporia, Kansas.
Surface
evaporation is recorded at intervals by measuring the change
in water level over a given period of time, usually not
less than 24 hours.

Figure
18

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Cover Picture
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