Ohio Journal of Science: Volume 46, Issue 6 (November, 1946)

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https://kb.osu.edu/handle/1811/1028

Front Matter
p. 0
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The Teays River
Ver Steeg, Karl pp. 297-307
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Variations in the Bird Populations of Ohio and Nearby States
Moseley, Edwin L. pp. 308-322
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Laboratory Tests Showing the Effect of DDT on Several Important Parasitic Insects
Peterson, Alvah pp. 323-326
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The Lifting Effect of Quicksand
Smith, Ernest Rice pp. 327-328
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Check List of Ohio Leafhoppers (Homoptera: Cicadellidae)
Osborn, Herbert; Knull, Dorothy Johnson pp. 329-336
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Notes on Nymphs of the Dragonfly Genus Helocordulia Needham
Wright, Mike pp. 337-339
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A New Species of Cyclocoelum (A Trematode) from the Eastern Solitary Sandpiper
Zeliff, C. Courson pp. 340-342
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Index to Volume XLVI
pp. 343-344
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Back Matter
p. 999
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Back Matter
(1946-11)
Index to Volume XLVI
(1946-11)
A New Species of Cyclocoelum (A Trematode) from the Eastern Solitary Sandpiper
(1946-11) Zeliff, C. Courson
Notes on Nymphs of the Dragonfly Genus Helocordulia Needham
(1946-11) Wright, Mike
Check List of Ohio Leafhoppers (Homoptera: Cicadellidae)
(1946-11) Osborn, Herbert; Knull, Dorothy Johnson
The Lifting Effect of Quicksand
(1946-11) Smith, Ernest Rice
Laboratory Tests Showing the Effect of DDT on Several Important Parasitic Insects
(1946-11) Peterson, Alvah
Variations in the Bird Populations of Ohio and Nearby States
(1946-11) Moseley, Edwin L.
The Teays River
(1946-11) Ver Steeg, Karl
The course of the Teays River, a large Tertiary stream, including the present Kanawha and New Rivers and their tributaries, has been traced from its source in the Piedmont region, westward to the Illinois River. This stream, more than 800 miles long, crossed the entire Appalachian region, passing through the abandoned valley, from a point near St. Albans to Huntington, West Virginia. From Chillicothe, Ohio, the buried valley of the Teays has been traced, by means of well records, in a westerly direction across Ohio, Indiana and Illinois to the_ Mississippi. The Teays River was a mature stream and drained a maturely dissected region. An early glacier, Kansan or pre-Kansan, dammed its westerly course in Ohio, ponding the waters, forming lake-like expanses in southeastern Ohio. In the ponded areas, slack-water deposits were laid down. The broad valley of the Teays (Kanawha-New) River was an avenue for the migration of plant life from the Piedmont region to southeastern Ohio.
Front Matter
(1946-11)

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