46 
IOWA ACADEMY OP SCIENCES. 
specimens were secured as a curiosity, and after being properly 
rounded, to obscure their origin, were recognized by some of 
the “old inhabitants” as genuine mad stones. Their curative 
power has yet to be tested, but in all other respects, apparently, 
their identification is complete. 
The fragments removed from the larger specimen were pre- 
served for examination and analysis. The specimen itself is 
larger than a hen’s egg, light gray in color, with darker specks 
of iron scattered through; distinctly stratified ; with no cleavage 
planes. The luster on a broken surface is resinous, on a worn 
surface more earthy. Its hardness, considered as a rock is 2i, 
but the fine powder scratches glass. It is infusible in an ordi- 
nary blowpipe flame, and powders easily after ignition. 
Under the microscope it appears to be made of flat and irreg- 
ular transparent granules about 1-500 millimeter thick, some of 
which are ten times that width, fitted loosely together so as to 
leave irregular cavities everywhere in communication with each 
other. The fragments resemble fragments of silicious infuso- 
rial shells which are found in large quantities in some parts of 
the Rocky mountains. 
The specimen after remaining some weeks in the air of a dry 
room (heated by hot air) weighed 70.77 grams. It was placed 
in distilled water, in which it floated for two or three minutes, 
boiled for some hours, and allowed to cool. After weighing it 
was hastily dried with a piece of filter paper and weighed 
again. Lastly it was dried some hours in an oven at a temper- 
ature of 100° to 150° C, cooled in a desiccator, and weighed. 
Weight in ordinary dry air 70 77 grams. 
Weight in water, saturated 39.14 grams. 
Weight in air, saturated.. 115.00 grams. 
Weight in air, dry.. 69.15 grams. 
From this data we get: 
Volume of rock in the specimen 30.01 cc. 
Volume of cavities in the specimen 45.85 cc. 
Total volume 75.86 cc. 
Specific gravity of rock 2.304 
Specific gravity of the whole 912 
Volume of water held in ordinary dry air.*. 162 cc. 
Some fragments of the stone were pulverized in an agate 
mortar, fused with sodium and potassium carbonates, and 
analyzed in the ordinary way. Before fusion the powder was 
dried at about 150°C. The results are as follows: 
