62 NATURAL HISTORY. [NORTH 
fibrous variety (which has received the name of botryolite) likewise from 
Arendal. 
Case 40 is set apart for such silicates as contain one or more borates, 
of which, however, in some cases, it is uncertain how far these may be 
considered as essential component parts. — To this order belong the 
species tourmaline and axinite. Among the red-coloured varieties 
of the former, some of which are called rubellife, the most remark¬ 
able deposited here is a specimen of uncommon form and dimensions, 
which was presented by the king of Ava to the late Colonel Symes, 
when on an embassy to that country; blue varieties of the same, some 
of them known by the name of indicoJite; a suite of modifications of 
tourmaline crvstals of tliose colours, as well as of others, such as srreen 
of various shades, among which, those from Brazil, Elba, and from 
Campolongo deserve more particular notice. Of the axinite, Wer¬ 
ner’s Thumei’stein, veiy characteristic specimens from Bourg d’Oisans, 
Norway, &c., will be found in this Table Case. 
Case 41. In this Case begins the order of the Cai’bonates — Carbonate 
of soda, %’arious localities. — Carbonate of baryta or witherite, among 
the specimens of which may be pai'ticularized the beautiful groups of 
double six-sided p}Tamids, and those of six-sided prismatic ciystals. 
— JSarytocalcite, from Alston Moor in Cumberland. — Carbonate of 
strontia, called strontianite, chiefly fr*om Strontian in Argyleshire, in 
prismatic and aciculai' cn stais, which latter liave sometimes been mis¬ 
taken for arragonite. The remaining part of this Case is occupied by 
such specimens of the mineral species called arragonite as have partly 
been found to contain a few per cent, of cai-bouate of strontia ; they 
are, however, essentially carbonates of lime, though of a different crystal 
system. Among the more intes'esting of the regular forms here deposited 
are the loose and variously grouped simple and hemitrope crvstals from 
Arragon, and from Herrengrund, in-Hungarv, Kosel, Bohemia, Sec., 
and the fine acicularly crystallized varieties, in brown iron stone, 
from liefeld, in volcanic ejections of Vesuvius, &c.: they are con¬ 
tinued in 
Case 42, in which are also placed several vei*y perfect specimens of 
the coralloidal variety of arragonite from Eisenertz in Stiria, and 
Hiittenberg in Cai'inthia, formerly called /cm, 8:c. : to the massive 
varieties of this species some of the calcareous deposits of Cai'lsbad in 
Bohemia may be referred. The remainder of the Case contains 
several striking varieties of common carbonate of lime or calcite, 
some of which have been mistaken for arragonite, and 
Cases 43 to 45. iSumerous crvstallized varieties of the same. 
Among the specimens placed in the first of these Table Cases may be 
specified those illustrative of double refraction, cleavage, supernumerary 
joints, colour, &c.; likewise the various secondary obtuse and acute rhom- 
bohedrons; among the former of which the most common, but net the least 
striking, is the inverae variety of Haiiy, so called from its being as it 
were an inversion of the primitive rhombohedron of calcareous spar; 
and the same with a considerable admixture of quartz, commonly called 
crystallized sandstone of Fontainbleau, &c. ; also many interesting and 
beautiful specimens, from the Hartz, Derbyshire, &c., of prismatic and 
pvramidal miodifications of the same substance. 
Case 45. Besides additional chiefiy prismatic modifications of ervs- 
