Normal view MARC view ISBD view

Cintaẏasi.

By:

Śarmā, Śaiḷa

Material type: Text

TextPublication details: [1962]Description: 103 p. 18 cmLOC classification:

AC125.O7 S3

Tags from this library: No tags from this library for this title. Log in to add tags.

Average rating: 0.0 (0 votes)

No physical items for this record

In Oriya.

There are no comments on this title.

to post a comment.

Back to results

1 The limestone resources and the lime industry in Ohio,
by Orton, Edward,
2 Corals from the coral limestone of Lion Creek, Stanwell, near Rockhampton,
by Etheridge, Robert,
3 A report on the limestones and cement materials of north Georgia,
by Maynard, Thomas Poole,
4 Kalkstensforekomster i Kristianiafeltet,
by Holtedahl, Olaf,
5 Limestone road materials of Wisconsin,
by Hotchkiss, William Otis,
6 The Catamaran and Strathblane coal fields and coal and limestone at Ida Bay, Southern Tasmania /
by Twelvetrees, W. H.
7 The geology and economic value of the Wapanucka limestone of Oklahoma.
by Wallis, B. Franklin
8 A report on the limestones and marls of the coastal plain of Georgia,
by Brantly, John Edward,
9 Preliminary report on the marls and limestone of Mississippi,
by Logan, William Newton,
10 Limestones and marls of North Carolina,
by Loughlin, G. F.
11 Analyses de calcareos.
by Brazil.
12 Limestones and marls of Wisconsin
by Steidtmann, Edward,
13 The limestone resources of Nyasaland,
by Dixey, F.
14 Summary report on the building limestones of the Russelville district,
by Jones, Walter Bryan,
15 Insoluble residue studies of Mississippian limestone in Indiana,
by Martin, Henry Garrett.
16 Études géologiques sur les calcaires de Bekrit et de Timhadit (Moyen Atlas)
by Pia, Julius,
17 Canadian limestone for building purposes,
by Goudge, Monson Fraser,
18 Marbles and limestones of Connecticut,
by Moore, Fred Holmsley,
19 A summary of the uses of limestone and dolomite,
by Lamar, J. E.
20 A southeastern limestone facies of lower Cambrian dolomite in Wythe and Carroll Counties, Virginia,
by Stose, George Willis,