Metalline
Mining Company
News
Release: For immediate release May 4, 2000
Additional
results from the oxide zinc mineralization, Sierra Mojada Project
Coeur d’Alene, Idaho – Metalline is pleased to
announce additional results of tonnage and grade calculations from channel
samples collected from the white zinc zone of the San Salvador mine.
Merlin Bingham, the
President of Metalline Mining Company, stated “that in addition to being
impressed by the quality and distribution of the channel samples throughout the
known white zinc zone (the existing workings), the zinc grade is exceptional,
only 3 mines in the world have grades greater than 15% zinc, according to the
International Zinc Association”. He
also expressed Metalline’s
satisfaction with North Limited as their Joint Venture partner, the high
quality of the work and with the aggressive program that is being conducted to
continue to develop an oxide zinc reserve at Sierra Mojada.
Multiple horizons of oxide zinc mineralization occur
in the San Salvador, Encantada and Fronteriza mines. There are two distinctive types of mineralization, one designated
the red zinc mantos which have been mined in all three mines and one designated
the white zinc zone which, to date, is known only in the San Salvador
mine.
The white zinc occurs vertically below the red zinc
on the 5 and 6 levels of the San Salvador.
The red zinc occurs on the 3 and 4 levels. The white zinc was discovered by Mineros Nortenos, relatively
recently during their mining operations in the three mines, which has spanned
in excess of 40 years. The red zinc is
brightly colored red and yellow and consists of iron oxide minerals,
smithsonite (zinc carbonate) and hemimorphite (zinc silicate) in limestone and
dolomite. The white zinc consists of
smithsonite and hemimorphite in limestone and calcareous shale and without the
iron oxide minerals has a grey to white color.
Since January, in excess
of an additional 1000 channel samples have been collected during mapping and
sampling of the 3 mines, 667 of these were collected in the white zinc zone of
the San Salvador mine. The channel
samples were added to the Gemcom database and a volume was created for the
sampling in the white zinc zone. The
results of grade and tonnage calculation for all channel and drill hole
samples within this volume is 7.3 million tonnes that
average 20.52% zinc. The
sampled volume is 400 meters in an east-west direction, 50 to 175 meters in a
north-south direction and 20 to 75 meters vertically. This volume represents the known extent of the white zinc. The calculation represents the sampling in
this volume of rock at the present time.
While the distribution of samples throughout the volume is impressive,
sampling is limited to the existing workings.
In order to bring the white zinc zone to a resource and eventually a
reserve will require additional drilling to sample between the existing
workings and to extend and define the limits of mineralization. This work indicates that significant tonnes
and grade can be developed in the white zinc.
The white zinc system can geologically be inferred to continue to the east
under the red zinc for at least the 1500 meters of the red zinc in the three
mines and it may be present throughout the 5 kilometers of the known oxide
mineralization of the district.
In Metalline’s news release
dated January 18, 2000, Metalline announced grade and tonnage calculation
results from the red zinc manto system of 2.1
million tonnes that average 13.86% zinc. A re-calculation, using the new
data, for the red zinc is currently in progress and will be announced when
completed.