Executive Documents, Printed for the General Assembly of North Carolina, At the Session of ... [serial] 1852, V 1

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Barnes, upon the Tossnot, is similar to that upon the plantation of Mr. Ham, near Golds- boro'. It is the blue marl, intermixed with innumerable small bivalve shells, which have become very thoroughly de- composed. The bed is eleven feel thick, covered with a stratum of sand five feet thick.
§ 36. The deposits of marl upon the Roanoke are no less important than upon the Tau, Neuse and Cape Fear. My examinations were confined chiefly to Halifax County. The beds, considered as one formation, cons
...ist of the following members : — 1. Layers of decomposed rock — a coarse mica slate.
2. Marl loaded with fossils, five feet.
3. Marl of a green color, with only a few shells, eight to ten feet.
4. Blue clay, from ten to fifteen feet thick.
5. Reddish clay, two feet.
6. Gravel, fine and coarse, twenty feet.
7. Cray sands and loam.
The marl lies deep, and is exposed only in ravines. It is attended with much expense in raising it. Mr. Pope, of Halifax, has used it upon his plantation, and has made pre- parations for its extensive consumption, and the results have been favorable.


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