Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Tecuamburro Volcano, Guatemala geothermal gradient core hole drilling, operations, and preliminary results

Conference ·
OSTI ID:7179136
; ; ;  [1];  [2]; ;  [3];  [4]
  1. Los Alamos National Lab., NM (USA)
  2. Geological Survey, Flagstaff, AZ (USA)
  3. Swissboring Overseas Corp. Ltd., Guatemala City (Guatemala)
  4. Unidad de Desarrollo Geotermico, Guatemala City (Guatemala). Inst. Nacional de Electrificacion
A geothermal gradient core hole (TCB-1) was drilled to a depth of 700+ m at the Tecuamburro geothermal site, Guatemala during February and March, 1990. The core hole is located low on the northern flank of the Tecuamburro Volcano complex. Preliminary analysis of cores (>98% core recovery) indicates that the hydrothermal system may be centered in the 4-km-diameter Chupadero Crater, which has been proposed as the source of pyroxene pumice deposits in the Tecuamburro area. TCB-1 is located 300 m south of a 300-m-diameter phreatic crater, Laguna Ixpaco; the core hole penetrates the thin edge of a tuff ring surrounding Ixpaco and zones of hydrothermal brecciation within the upper 150 m may be related to the phreatic blast, dated at 2,910 {sup 14}C years. At the time of this writing, the unequilibrated temperature at a depth of 570m was 180{degree}C. Data on fracturing, permeability, hydrothermal alteration, and temperature will be presented. 3 refs., 3 figs.
Research Organization:
Los Alamos National Lab., NM (USA)
Sponsoring Organization:
AID
DOE Contract Number:
W-7405-ENG-36
OSTI ID:
7179136
Report Number(s):
LA-UR-90-932; CONF-900823--6; ON: DE90008929
Country of Publication:
United States
Language:
English