EXPLANATION OF PLATE I.
MAGNIFIED SECTIONS OF VESUVIAN MINERALS.
Fig. 1. Section of leucite crystal from the lava of 1868, with fluid cavities. Mag., 350 diams.
" 2, 3, 4, and 5. Sections of nepheline crystals from the lava of 1767, 1834, and 1854.
" 6. Section of sodalite crystal from the lava of 1794, with belonites and crystals of magnetite enclosed.
" 7, 8, 9. Crystals of leucite with microliths and cavities darkened by magnetite dust; also, containing crystals of magnetite.
" 10. Group of leucite crystals of irregular form from the lava of 1855, congregated around a nucleus of crystals of plagioclase and magnetite.
[Illustration: Plate II.]
EXPLANATION OF PLATE II.
MAGNIFIED SECTIONS OF VESUVIAN MINERALS.
Fig. 1. Section of augite crystal from the lava of 1794, with numerous gas cells and delicately banded walls. The interior contains two long prisms, probably of apatite.
" 2. Crystal of augite with banded walls, and indented by leucite crystals, from the lava of 1794. Mag., 40 diams.
" 3, 4, 5. Sections of augite crystals from the lavas of 1794 and 1820.
" 6. Group of augite crystals from the lava of 1835.
" 7. Ditto from the lava of 1822, with encluded mica-flake (_a_) and portion of the glass paste, or ground-mass, of the rock (_b_), containing microliths and grains of magnetite.
Fig. 8. Two crystals of olivine from the lava of 1855; they are intersected on one side by the plane of the thin section, and are remarkable for showing lines of gas cells, and bands of growth sometimes cellular. Mag., 40 diams.
" 9. Section of rock-crystal (quartz), with double terminal pyramids, from the lava of 1850.
" 10. Twin crystal of sanidine from the lava of 1858. Mag., 40 diams.
" 11, 12, 13. Sections of plagioclase crystals (probably labradorite) from the lava of 1855. Mag., 100 diams.
" 14. Section of olivine crystal from the lava of 1631--imperfectly formed. Mag., 30 diams.
" 15. Section of mica-flake from the lava of 1822. Mag., 30 diams.
[Illustration: Plate III.]
EXPLANATION OF PLATE III.
MAGNIFIED SECTIONS OF VOLCANIC ROCKS.
1. Diorite dyke, traversing Assynt limestone, North Highlands.
2. Basalt from upper beds, near Giant's Causeway, County Antrim.
3. Hornblende-hypersthene-augite Andesite, from Pichupichu, Andes.
4. Augite-Andesite from Pichupichu, Andes.
5. Olivine dolerite, with hornblende and biotite, Madagascar.
6. Leucite basalt, with mellilite, Capo di Bove, Italy.
[Illustration: Plate IV.]
EXPLANATION OF PLATE IV.
MAGNIFIED SECTIONS OF VOLCANIC ROCKS.
1. Vesuvian lava, glass paste with numerous crystals of leucite; others of augite and nepheline porphyritically developed; also small grains of magnetite.
2. Vesuvian lava, glass paste with numerous crystals of leucite; others of olivine, hornblende, and sanidine, porphyritically developed; small grains of magnetite.
3. Trachyte from Hungary; felsitic paste with crystals of hornblende and sanidine, and a little magnetite.
4. Gabbro, from Carlingford Hill, Ireland, consisting of anorthite, augite, a little olivine, and magnetite.
5. Dolerite, from old volcanic neck, Scalot Hill, near Lame, consisting of labradorite, augite, olivine, and magnetite.
6. Dolerite, Ballintoy, County Antrim, showing ophetic structure, consisting of augite, labradorite, and magnetite.
[1] Mr. S. Allport has discovered this in the rock called the "Wolf Rock" off the coast of Cornwall. The most important work on basalt is that by F. Zirkel, _Unters. uber mikros. Zusammensetzung und Structur der Basaltgesteine_. Bonn (1870).
[2] Zirkel, _Die mikroskopische Beschaffenheit der Mineralien und Gesteine_, p. 153. Leipsig (1873).
[3] Zirkel, _Petrog._, i. 578; B. von Cotta, p. 178 (Eng. Trans.).