The geological formations crossed by the Syracuse and Chenango Valley Railroad

B. &ensp;.

2. Neighboring localities of same formation. 3. Rocks and minerals. 4. Fossil remains. 5. Economical products.
 * 1. Outcrops.
 * 1. Outcrops.
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C. &ensp;.

2. Neighboring localities of same formation. 3. Rocks. 4. Fossil remains. 5. Economical products.
 * 1. Outcrops.
 * 1. Outcrops.
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D. &ensp;.


 * 1. Divisions.
 * 1. Divisions.

b. Hamilton beds, proper. c. Genesee Shale. 2. Outcrops.
 * a. Marcellus Shale.
 * a. Marcellus Shale.
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b. Hamilton proper. c. Genesee. 3. Neighboring localities of same formation.
 * a. Marcellus.
 * a. Marcellus.
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b. Hamilton proper. c. Tully Limestone. d. Genesee Shale. 4. Rocks. 5. Fossil remains. 6. Economical products. E. &ensp;.
 * a. Marcellus Shale.
 * a. Marcellus Shale.
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2. Origin of deposits. 3. Natural products, timber, etc. 4. Adaptability to agricultural products. 5. Economical products. II. &ensp; HYDROGRAPHY OF MADISON AND ONONDAGA COUNTIES.
 * 1. Nature of deposits.
 * 1. Nature of deposits.
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 * A. &ensp; Drainage
 * A. &ensp; Drainage

2. Atlantic (Susquehanna) system. B. &ensp; Trend of watershed. C. &ensp; Waterfalls. D. &ensp; Lakes and ponds. E. &ensp; Mineral springs. F. &ensp; Effect of clearings on streams. III. &ensp; VALLEY FORMATIONS OF MADISON AND ONONDAGA COUNTIES.
 * 1. St. Lawrence system.
 * 1. St. Lawrence system.
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B. &ensp; Similarity to formations elsewhere. C. &ensp; Former higher level of lakes; their probable future. D. &ensp; Theory of valley formation. IV. TABLES AND LISTS.
 * A. &ensp; General trend of local valleys.
 * A. &ensp; General trend of local valleys.
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