98 BULLETIN 94, UNITED STATES NATIONAL MUSEUM. 



A fine-grained, light gray, chondritic stone' with pyrrhotite and 

 metallic particles visible to the unaided eye. Stone traversed by fine 

 dark veins. 



References.— K. von Schreiberg, Gilbert's Ann. Phys., vol. 30, 

 1808. O. Biichner, Die Meteoriten in Sammlungen, 1863, p. 26. 



LLANO DEL INCA, 35 LEAGUES SOUTHEAST OF TOLTAL, ATACAMA, CHILE. No. 156. 



Stony-iron, M. Weight, 66 grams, from a mass weighing 3,145 

 grams found in 1888. 



LODHRAN, PUNJAUB, EAST INDIA. No. 481. 



Stone, Lo. Fragments from interior weighing 17.52 grams. Fell 

 October 1, 1868. Is of interest on account of its granular and friable 

 nature and the unusual crystallographic development of the olivine 

 and bronzite. The mineral composition, as determined by Tscher- 

 mak, is : 



Per cent. 



Nickel-iron 32. 5 



Olivine 28.9 



Bronzite with some chroniite and anortliite 31.2 



Pyrrhotite 7. 4 



100. 00 



Reference.— Q. Tschermak, Sitz. Alcad. Wiss. Wien, vol. 61, 1870, 

 p. 465. 



LONG ISLAND, PHILLIPS COUNTY, KANSAS. No. 211. 



Stone, Cia. Weight, 1,893 grams; in three pieces, (A) weighing 

 493 grams, having a slickensided surface, later smoothed to a smooth 

 brown crust; (B) weighing 159 grams; and (C) weighing 1,241 

 grams. All have surfaces much oxidized and in places encrusted 

 with calcium carbonate. Date of fall unknown; found in 1891. 

 Original weight some 936 kilograms, of which the larger portion, 

 in many pieces, is in the collections of the Field Columbian Museum. 

 Described by Weinschenk as a dark green stone showing metallic 

 iron, with crystalline structure (rarely chondritic) plainly evident 

 to the unaided eye. The mineral composition is given as olivine and 

 bronzite, sometimes the one and sometimes the other prevailing, 

 rarely a monoclinic pyroxene (diallage), pyrrhotite, cliromite, and 

 metallic iron. Analysis by H. W. Nichols yielded: 



uv.iii; 



