Geothermal Gradient Drilling and Measurements Ascension Island, South Atlantic Ocean

This technical report on the Phase II geothermal exploration of Ascension Island documents the data collected during thermal gradient drilling and the subsequent thermal and fluid chemical investigations. It also documents the completion of the Phase II exploration strategy which was proposed at the...

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Main Authors: Sibbett, B. S., Nielson, D. L., Adams, M. C.
Other Authors: United States. Department of Energy.
Format: Report
Language:English
Published: Geothermal Energy Program (U.S.) 1984
Subjects:
Online Access:https://doi.org/10.2172/893457
https://digital.library.unt.edu/ark:/67531/metadc882822/
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author Sibbett, B. S.
Nielson, D. L.
Adams, M. C.
author2 United States. Department of Energy.
author_facet Sibbett, B. S.
Nielson, D. L.
Adams, M. C.
author_sort Sibbett, B. S.
collection University of North Texas: UNT Digital Library
description This technical report on the Phase II geothermal exploration of Ascension Island documents the data collected during thermal gradient drilling and the subsequent thermal and fluid chemical investigations. It also documents the completion of the Phase II exploration strategy which was proposed at the end of the Phase I--Preliminary Examination of Ascension Island. The thermal gradient drilling resulted in seven holes which range from 206 to 1750 ft (53-533 m) deep, with a cumulative footage of 6563 ft (2000 m). The drilling procedure and the problems encountered during the drilling have been explained in detail to provide information valuable for any subsequent drilling program on the island. In addition, the subsurface geology encountered in the holes has been documented and, where possible, correlated with other holes or the geology mapped on the surface of the island. Temperatures measured in the holes reach a maximum of 130 F (54.4 C) at 1285 ft (391.7 m) in hole GH-6. When the temperatures of all holes are plotted against elevation, the holes can be classed into three distinct groups, those which have no thermal manifestations, those with definite geothermal affinities, and one hole which is intermediate between the other two. From consideration of this information, it is clear that the highest geothermal potential on the island is in the Donkey Flat area extending beneath Middleton Ridge, and in the Cricket Valley area. Because of the greater drilling depths and the remote nature of the Cricket Valley area, it is recommended that future exploration concentrate in the area around Middleton Ridge.
format Report
genre South Atlantic Ocean
genre_facet South Atlantic Ocean
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op_doi https://doi.org/10.2172/893457
op_relation rep-no: DOE/ID/12079-117
rep-no: ESL No.-134
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https://digital.library.unt.edu/ark:/67531/metadc882822/
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spelling ftunivnotexas:info:ark/67531/metadc882822 2025-01-17T00:50:04+00:00 Geothermal Gradient Drilling and Measurements Ascension Island, South Atlantic Ocean Sibbett, B. S. Nielson, D. L. Adams, M. C. United States. Department of Energy. 1984-07-01 Text https://doi.org/10.2172/893457 https://digital.library.unt.edu/ark:/67531/metadc882822/ English eng Geothermal Energy Program (U.S.) rep-no: DOE/ID/12079-117 rep-no: ESL No.-134 doi:10.2172/893457 osti: 893457 https://digital.library.unt.edu/ark:/67531/metadc882822/ ark: ark:/67531/metadc882822 Geothermal Exploration Atlantic Ocean 15 Geothermal Energy Geology Geothermal Legacy Exploration Drilling Burros Temperature Gradients Geothermal Legacy Islands Geothermal Gradients Report 1984 ftunivnotexas https://doi.org/10.2172/893457 2019-06-15T22:07:52Z This technical report on the Phase II geothermal exploration of Ascension Island documents the data collected during thermal gradient drilling and the subsequent thermal and fluid chemical investigations. It also documents the completion of the Phase II exploration strategy which was proposed at the end of the Phase I--Preliminary Examination of Ascension Island. The thermal gradient drilling resulted in seven holes which range from 206 to 1750 ft (53-533 m) deep, with a cumulative footage of 6563 ft (2000 m). The drilling procedure and the problems encountered during the drilling have been explained in detail to provide information valuable for any subsequent drilling program on the island. In addition, the subsurface geology encountered in the holes has been documented and, where possible, correlated with other holes or the geology mapped on the surface of the island. Temperatures measured in the holes reach a maximum of 130 F (54.4 C) at 1285 ft (391.7 m) in hole GH-6. When the temperatures of all holes are plotted against elevation, the holes can be classed into three distinct groups, those which have no thermal manifestations, those with definite geothermal affinities, and one hole which is intermediate between the other two. From consideration of this information, it is clear that the highest geothermal potential on the island is in the Donkey Flat area extending beneath Middleton Ridge, and in the Cricket Valley area. Because of the greater drilling depths and the remote nature of the Cricket Valley area, it is recommended that future exploration concentrate in the area around Middleton Ridge. Report South Atlantic Ocean University of North Texas: UNT Digital Library
spellingShingle Geothermal Exploration
Atlantic Ocean
15 Geothermal Energy
Geology
Geothermal Legacy
Exploration
Drilling
Burros
Temperature Gradients Geothermal Legacy
Islands
Geothermal Gradients
Sibbett, B. S.
Nielson, D. L.
Adams, M. C.
Geothermal Gradient Drilling and Measurements Ascension Island, South Atlantic Ocean
title Geothermal Gradient Drilling and Measurements Ascension Island, South Atlantic Ocean
title_full Geothermal Gradient Drilling and Measurements Ascension Island, South Atlantic Ocean
title_fullStr Geothermal Gradient Drilling and Measurements Ascension Island, South Atlantic Ocean
title_full_unstemmed Geothermal Gradient Drilling and Measurements Ascension Island, South Atlantic Ocean
title_short Geothermal Gradient Drilling and Measurements Ascension Island, South Atlantic Ocean
title_sort geothermal gradient drilling and measurements ascension island, south atlantic ocean
topic Geothermal Exploration
Atlantic Ocean
15 Geothermal Energy
Geology
Geothermal Legacy
Exploration
Drilling
Burros
Temperature Gradients Geothermal Legacy
Islands
Geothermal Gradients
topic_facet Geothermal Exploration
Atlantic Ocean
15 Geothermal Energy
Geology
Geothermal Legacy
Exploration
Drilling
Burros
Temperature Gradients Geothermal Legacy
Islands
Geothermal Gradients
url https://doi.org/10.2172/893457
https://digital.library.unt.edu/ark:/67531/metadc882822/