1843
DOI: 10.5962/bhl.title.44618
|View full text |Cite
|
Sign up to set email alerts
|

Report on the commencement and progress of the Agricultural survey of South-Carolina, for 1843

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
1
0

Year Published

1959
1959
2019
2019

Publication Types

Select...
1
1

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(2 citation statements)
references
References 0 publications
0
1
0
Order By: Relevance
“…This often highly indurated, typically gray limestone was named "the Santee white limestone" by Charles Lyell, who, in the company of Edmund Ravenel in 1842, correctly determined that oysters he observed in outcrops near Eutaw Springs along the bank of the Santee River in Orangeburg County (now submerged) were of Eocene age (Lyell, 1845). Referred to as the "Great Carolina beds" by Ruffin (1843), the "Santee beds" by Tuomey (1848), and the "Santee marl" by Sloan (1908), it was Cooke (1936) who designated the exposures at Eutaw Springs as the type section of his Santee Limestone (Banks, 1977). The unit is widespread in the subsurface of the SC Coastal Plain, although normally exposed only in deep commercial quarries, such as those at the Martin Marietta Berkeley and Orangeburg quarries near Cross, SC.…”
Section: Ectoganus Gliriformis Lobdelli Fisherichthys Folmerimentioning
confidence: 99%
“…This often highly indurated, typically gray limestone was named "the Santee white limestone" by Charles Lyell, who, in the company of Edmund Ravenel in 1842, correctly determined that oysters he observed in outcrops near Eutaw Springs along the bank of the Santee River in Orangeburg County (now submerged) were of Eocene age (Lyell, 1845). Referred to as the "Great Carolina beds" by Ruffin (1843), the "Santee beds" by Tuomey (1848), and the "Santee marl" by Sloan (1908), it was Cooke (1936) who designated the exposures at Eutaw Springs as the type section of his Santee Limestone (Banks, 1977). The unit is widespread in the subsurface of the SC Coastal Plain, although normally exposed only in deep commercial quarries, such as those at the Martin Marietta Berkeley and Orangeburg quarries near Cross, SC.…”
Section: Ectoganus Gliriformis Lobdelli Fisherichthys Folmerimentioning
confidence: 99%
“…Results of work begun by Lardner Vanuxem were published hi 1826. Edmund Ruffin (1843) continued the survey which culminated in 1848 with the first State geologic map, prepared by Michael Tuomey. A later map was made by Earle Sloan (1907Sloan ( , 1908 who gave an extensive list of mineral and fossil localities.…”
Section: Introductionmentioning
confidence: 99%