| Plate | Photo Description | 
| 1 | (a) 
- (d) — Fully developed uranium halos in mica (biotite) | 
| 2 | (a) - (d) — 
210Po halos in mica (biotite); (a) — 
also with a 218Po halo | 
| 3 | (a) - (d) — 
214Po halos in mica (biotite) | 
| 4 | (a) - (d) — 
218Po halos in mica (biotite) | 
| 5 | (a, b & d) — Elliptical (compressed) 
210Po halos in coalified wood; 
(c) — Dual 210Po halo in coalified wood | 
| 6 | Uranium halos in fluorite in different stages of development:
(a)	- (b) — Embryonic; 
(c) - (d) — Fully developed; 
(e) — Overexposed, first-stage 
reversal; (f) - (g) — 
Overexposed, second-stage reversal; (h) — 
Overexposed, third-stage 
reversal | 
| 7 | (a) - (h) — 210Po halos in fluorite | 
| 8 | (a) - (h) — 
218Po halos in fluorite; (c) — center darkened 
by electron microbeam analysis | 
| 9 | (a) — 218Po halos in mica (biotite); 
(b) — Spectacle halo 
in biotite; (c) - (d) — 
214Po halos in biotite | 
| 10 | (a) — Overlapping 210Po halos in biotite, using phase contrast;
(b)	and (d) — Thorium halo and 
giant halo in Madagascan mica;
(c)	— Dwarf halos in Ytterby mica; 
(e) - (f) — 
Assortment of different
polonium halo types in biotite; (g) — 214Po halos in biotite;
(h)	— A 210Po and a 214Po halo in biotite | 
| 11 | (a) — Biotite crystal from Murray Bay, Canada; (b) — Po halo 
containing specimens of granite from New Hampshire, the dark areas are biotite crystals; 
(c) — Zircon crystals extracted from granite drill cores taken from a depth of about 
15,000 ft.; (d) — Rhyolite from 1,683.3 ft. (specimen obtained from 
J. Eichelberger, Sandia National Labs) |