| UNIDENTIFIED MINERALS ASSOCIATED WITH ZEOLITES EBURRU STATION HYDROTHERMAL LOCALITY | |
![]() 5-7-86 No. 88 5KV APER200 x1000 by CMN |
THIS TABLE LOOKS BEST WHEN VIEWED USING INTERNET EXPLORER. MAGNIFICATION FIGURES ARE FOR THE ORIGINAL SEMs, NOT FOR THE IMAGES YOU SEE ON YOUR COMPUTER SCREEN. I WILL BE ADDING SCALE BARS WHEN I HAVE TIME TO DO THE CALCULATIONS. Rosettes White. In cloumn-like structures on flat blades of an unidentified zeolite, possibly heulandite. |
![]() 4-9-86 No. 68 5KV APER200 x48.5 by CMN |
Fiberous Tufts White. Needles covered with platy structures to form fiberous looking tufts; on chabazite. |
![]() 4-9-86 No. 69 5KV APER200 x194 by CMN |
Fiberous Tufts White. Needles covered with platy structures to form fiberous looking tufts; on chabazite. |
![]() 5-14-86 No. 98 5KV APER200 x50 by CMN |
Fiberous Tufts White. Needles (?) covered with platy structures to form fiberous looking tufts growing on chabazite. See SEMs below for details. |
![]() 5-14-86 No. 100 5KV APER200 x500 by CMN |
Fiberous Tufts White. Needles (?) covered with platy structures to form fiberous looking tufts growing on chabazite. |
![]() 5-14-86 No. 101 5KV APER200 x500 by CMN |
Fiberous Tufts White. Needles (?) covered with platy structures to form fiberous looking tufts growing on chabazite. |
![]() 5-14-86 No. 103 5KV APER200 x2000 by CMN |
Fiberous Tufts White. Needles (?) covered with platy structures to form fiberous looking tufts growing on chabazite. |
![]() 5-14-86 No. 102 5KV APER200 x2000 by CMN |
Fiberous Tufts White. Needles (?) covered with platy structures to form fiberous looking tufts growing on chabazite. |
![]() 4 -2-86 No. 37 5KV APER200 x2000 by CMN |
Coated Needles White. Needles (?) covered with interconnectes spheres of unknonwn mineral. |
![]() 4 -2-86 No. 38 5KV APER200 x2000 by CMN |
Fiberous Tufts White. Needles (?) covered with unidentified amorphous coating, on chabazite. |
![]() 5-7-93 No. 2000 5KV APER200 x2000 by CMN |
Fiberous mat Pale ivory. Underlying bosses and domes of pale blue clay mineral covered by dense mat of fiberous crystals. Cracks probably from shrinkage of underlying clay mineral. |