506 University Geological Survey of Kansas. 
A BIBLIOGRAPHY OF PUBLICATIONS ON THE MINERALS OF 
THE DISTRICT, WITH BRIEF ABSTRACTS. 
1. 18738-’74. Description of the Ores and Associated Min- 
erals, being chapter XXIII of Report of Geological Survey 
of Missouri, pp. 886-399 ; A. Schmidt and A. Leonard. Men- 
tions the following minerals: Galena, cerussite, pyromorphite, 
blende, calamine, smithsonite, zinc bloom, pyrites, limonite, 
dolomite, calcite, quartz, and bitumen. 
2. 1877. Geological Survey of Missouri, Industrial Report 
on Lead, Zinc, and Iron, pp. 9-25, 105-109; Chas. P. Will- 
iams. Gives the following list of minerals: Galena, pyro- 
morphite, anglesite, cerussite, hydrozincite, and goslarite 
(in solution in mine waters). 
3. 1881. Notes on Kansas Minerals, Trans. Kan. Acad. 
Sci., VIII, pp. 25, 26; Erasmus Haworth. Reports the fol- 
lowing minerals from the vicinity of Galena, Kan.: Chalco- 
pyrite, greenockite, and anglesite. 
4. 1882. Notes on the Minerals of Missouri, St. Louis 
Acad. of Sci., IV, pp. 401-413; A. V. Leonard. Lists the 
following minerals as occurring in the district: Galena, 
cerussite, pyromorphite, anglesite, sphalerite, smithsonite, 
hydrozincite, calamine, buratite, greenockite, pyrite, mar- 
casite, dolomite, calcite, aragonite, and bitumen. 
5. 1884. A Contribution to the Geology of the Lead and 
Zine Mining District of Cherokee County, Kansas; Hrasmus 
Haworth; printed by the author, Oskaloosa, Iowa, June, 
1884. Reports the following minerals from Cherokee county, 
Kansas: Galena, anglesite, cerussite, sphalerite, smithsonite, 
hydrozincite, calamine, goslarite, pyrite, marcasite, melan- 
terite, calcite, dolomite, barite, greenockite, chalcopyrite, 
quartz, azurite, and limonite. 
6. 1890. The Zinciferous Clays of Southwest Missouri, 
and a Theory as to the Growth of the Calamine of that Sec- 
tion, Amer. Jour. Sci., XXXIX (3), pp. 38-42; W. H. 
Seamon. Gives analyses of ‘‘tallow-clays,’’ which show 
variable, though often large percentages of zinc oxide, some 
containing as high as fifty-four per cent. ‘‘From the rela- 
