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NARROW
Format
Article Type
Journal
Publisher
Section
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
-
Africa
-
East Africa
-
Ethiopia (1)
-
Ethiopian Rift (1)
-
Kenya
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Kenya Rift valley (5)
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Lake Magadi (1)
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-
Lake Natron (1)
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Malawi (1)
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Tanzania
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Olduvai Gorge (1)
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Zambia (2)
-
-
East African Lakes
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Lake Kariba (1)
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Lake Magadi (1)
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Lake Natron (1)
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East African Rift (2)
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Gregory Rift (1)
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North Africa
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Algeria
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Guelma Algeria (1)
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Egypt
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Kharga Oasis (1)
-
-
-
Southern Africa
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Barberton greenstone belt (2)
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Karoo Basin (2)
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South Africa
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Eastern Cape Province South Africa (1)
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Gauteng South Africa (1)
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KwaZulu-Natal South Africa (1)
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Transvaal region (1)
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Western Cape Province South Africa (1)
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Zimbabwe (1)
-
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West Africa
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Adamawa (1)
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Benue Valley (1)
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Cameroon (1)
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Nigeria
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Jos Plateau (1)
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Niger Delta (1)
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-
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Altiplano (3)
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Anglesey (1)
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Arctic Ocean (1)
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Arctic region
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Greenland (1)
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Russian Arctic (1)
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Svalbard
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Spitsbergen (1)
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Asia
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Altai Mountains
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Gorny Altai (1)
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Mongolian Altai (1)
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Altai Russian Federation
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Gorny Altai (1)
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Altai-Sayan region (1)
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Anadyr Basin (1)
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Arabian Peninsula
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Oman (3)
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Baikal region (2)
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Baikal rift zone (6)
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Buryat Russian Federation (4)
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Central Asia (1)
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Chukotka Russian Federation
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Chukchi Peninsula (1)
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Far East
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China
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Altyn Tagh Fault (1)
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Gansu China
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Hexi Corridor (1)
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Guangdong China (2)
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Inner Mongolia China (1)
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Longmenshan (1)
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Qilian Mountains (1)
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Xianshuihe fault zone (1)
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Xizang China (5)
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Yunnan China
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Tengchong (2)
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Japan
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Hokkaido (4)
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Honshu
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Gumma Japan (1)
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Kanto Plain (1)
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Matsushiro Japan (1)
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Nagano Japan (1)
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Tamagawa (1)
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Kyushu
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Sakura-jima (1)
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Kumamoto Japan
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Aso (1)
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Mongolia
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Mongolian Altai (1)
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Taiwan (2)
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Himalayas
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Garhwal Himalayas (3)
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Indian Peninsula
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India
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Cauvery Basin (1)
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Ghats
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Northeastern India
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Rajasthan India
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Uttarakhand India
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Jammu and Kashmir
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Nepal (3)
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Irkutsk Russian Federation (1)
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Kamchatka Russian Federation
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Kamchatka Peninsula
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Uzon (1)
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Kemerovo Russian Federation (1)
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Kolyma River (1)
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Main Central Thrust (2)
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Middle East
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Dead Sea Rift (2)
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Iran
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Israel
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Jordan (2)
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Turkey
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Zagros (1)
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Novosibirsk Russian Federation (2)
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Russian Far East (1)
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Sayan
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Atlantic Ocean
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Tarawera volcanic complex (1)
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Canada
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Eastern Canada
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Newfoundland and Labrador
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Newfoundland (1)
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Ontario
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Thunder Bay (1)
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Quebec
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Anticosti Island (1)
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Nunavut
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Ellesmere Island (1)
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Sverdrup Basin (1)
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Sverdrup Islands
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Axel Heiberg Island (2)
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-
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Queen Elizabeth Islands
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Ellesmere Island (1)
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Sverdrup Basin (1)
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Sverdrup Islands
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Axel Heiberg Island (2)
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Western Canada
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Alberta
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Banff National Park (6)
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Jasper National Park (3)
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British Columbia
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Queen Charlotte Islands (1)
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Canadian Cordillera (2)
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Canadian Rocky Mountains (5)
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Manitoba (2)
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Northwest Territories (6)
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Saskatchewan (1)
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Yukon Territory (5)
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-
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Caribbean region
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West Indies
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Antilles
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Greater Antilles
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Hispaniola
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Haiti (1)
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-
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Lesser Antilles
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Montserrat Island
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Soufriere Hills (1)
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Soufriere (1)
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Trinidad and Tobago
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Bahamas (1)
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Cascade Range (4)
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Central America
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Costa Rica (1)
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Central Valley (1)
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Colorado River basin (1)
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Columbia Hills (2)
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Commonwealth of Independent States
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Kyrgyzstan (1)
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Russian Federation
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Anadyr Basin (1)
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Baikal region (2)
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Baikal rift zone (6)
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Buryat Russian Federation (4)
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Chukotka Russian Federation
-
Chukchi Peninsula (1)
-
-
Irkutsk Russian Federation (1)
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Kamchatka Russian Federation
-
Kamchatka Peninsula
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Uzon (1)
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-
-
Kemerovo Russian Federation (1)
-
Khabarovsk Russian Federation (1)
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Kolyma River (1)
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Kolyma Uplift (1)
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Krasnoyarsk Russian Federation (1)
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Lake Baikal (2)
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Lena River (1)
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Magadan Russian Federation (1)
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Novosibirsk Russian Federation (2)
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Orenburg Russian Federation (1)
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Russian Arctic (1)
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Russian Far East (1)
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Russian Pacific region (2)
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Sakhalin Russian Federation
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Kuril Islands
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Etorofu Island (1)
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Siberian Platform (1)
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Tatar Russian Federation
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Romashkino Field (1)
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Transbaikalia (1)
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Tuva Russian Federation (2)
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Yakutia Russian Federation
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Aldan River (1)
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Indigirka River (1)
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Volga-Ural region (1)
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Death Valley (2)
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East Pacific Ocean Islands
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Hawaii
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Kilauea (2)
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Mauna Loa (1)
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Europe
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Alps
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Eastern Swiss Alps (1)
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Western Alps
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Carpathians
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Central Europe
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Austria (1)
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Czech Republic
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Germany
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Hungary (1)
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Slovakia (1)
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Switzerland
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Swiss Alps
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Eastern Swiss Alps (1)
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Jutland (1)
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Orenburg Russian Federation (1)
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Southern Europe
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Croatia (1)
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Greece
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Crete (1)
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Greek Aegean Islands
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Cyclades
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Ionian Islands
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Iberian Peninsula
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Mexico
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Panamint Range (1)
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Kern County California (2)
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Mono County California
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New York
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Balcones fault zone (7)
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Utah
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iodine
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hydrogen
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nitrogen
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helium
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krypton
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oxygen
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dissolved oxygen (3)
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O-18/O-16 (85)
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Proboscidea
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Mastodontoidea (1)
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-
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Reptilia
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cyanobacteria (13)
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Invertebrata
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Ostracoda
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Podocopida
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Candona (2)
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Darwinula (2)
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-
-
-
-
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Mollusca
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Bivalvia
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Heterodonta
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Veneroida
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Cephalopoda
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Gastropoda (2)
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Protista
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Foraminifera
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Textulariina
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microfossils
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Conodonta (1)
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Plantae
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Spermatophyta
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thallophytes (13)
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Cenozoic
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Quaternary
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Tertiary
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Asmari Formation (1)
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Muddy Creek Formation (1)
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Neogene
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Miocene
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Pliocene (15)
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Paleogene
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upper Tertiary (2)
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Coal Measures (1)
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Laurentide ice sheet (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Edwards Formation (1)
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Trinity Group (1)
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Upper Cretaceous
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Franciscan Complex (1)
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Jurassic
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Navajo Sandstone (2)
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Upper Triassic
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-
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Paleozoic
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Carboniferous
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Lower Carboniferous
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Dinantian (2)
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Mississippian
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Lower Mississippian
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Burlington Limestone (1)
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Pocono Formation (1)
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Madison Group (1)
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Upper Mississippian
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Mauch Chunk Formation (1)
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Meramecian
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Saint Louis Limestone (1)
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-
-
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Namurian (2)
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Pennsylvanian
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Upper Carboniferous
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Millstone Grit (2)
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-
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Devonian
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Lower Devonian
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Old Red Sandstone (3)
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Upper Devonian
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Chemung Formation (1)
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Hampshire Formation (1)
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Knox Group (1)
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lower Paleozoic
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Conococheague Formation (1)
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Madera Formation (1)
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middle Paleozoic (1)
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Middle Ordovician
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Platteville Formation (1)
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Upper Ordovician (1)
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Permian
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Toroweap Formation (1)
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Silurian
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Lower Silurian
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Tuscarora Formation (3)
-
-
-
upper Paleozoic
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Arkansas Novaculite (1)
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-
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Precambrian
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Archean
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Gunflint Iron Formation (1)
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upper Precambrian
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Proterozoic
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igneous rocks
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Mesozoic
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Namurian (2)
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Upper Carboniferous
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
springs
MACROCOMPONENT COMPOSITION AND GENESIS OF PORE SOLUTIONS IN HYDROTHERMAL CLAYS OF THE PAUZHETKA GEOTHERMAL SYSTEM ( Southern Kamchatka ) Available to Purchase
GEOCHEMISTRY OF GROUNDWATERS AND SURFACE WATERS, AND GROUND ICE OF THE OKA PLATEAU ( Eastern Sayan, Russia ) Open Access
Catalog Replenishment Based on Statistical Method for Strong Earthquakes in the Triple Junction Area, Eastern Tibet Available to Purchase
Role of the Water–Rock System in the Formation of the Composition of Radon Water of the Tulinskoe Field (Novosibirsk) Available to Purchase
Heat Flow in the Northeastern Continental Margin of Russia Available to Purchase
The Hydrological Impact of Historical and Modern Earthquakes in Central‐Southern Italy: Data Analysis and Seismotectonic Insights Available to Purchase
Application of Multi-Near-Surface Geophysical Surveys for Geothermal Spring: A Case Study in Kon Tum Province, Vietnam Available to Purchase
Geoheritage in the making: the discovery and vulnerability of deep-sea hydrothermal vents Available to Purchase
Abstract Some significant geological sites are inaccessible. Among the most inaccessible sites are the hydrothermal vents and their associated biological communities located deep in the ocean. These prime geoheritage sites, hosting what may be the most primordial life on Earth, are vulnerable to mineral and fishing exploitation. Many lie in international waters, protected only by non-binding agreements with no clearly defined means of enforcement. The discovery of these vents in 1977 fundamentally altered scientists’ view of basic Earth processes and the extreme conditions under which life can exist. The discovery of the vents was a group effort and required technological accomplishments not available to previous generations of researchers. Often overlooked in the credits for this discovery was the persistence and determination of Kathleen Crane, a graduate student at Scripps Institution of Oceanography. Many women of her era faced significant challenges as they attempted to break into an often-unwelcoming field, marine geology. The challenges were not unique to geology; women were not welcomed in many other disciplines, both scientific and non-scientific. In spite of the obstacles, few people have made as remarkable a geoscience discovery as Dr Crane.
Rapid diagenesis and microbial biosignature degradation in spring carbonates from Crystal Geyser, Utah, U.S.A. Available to Purchase
Hydrochemical evolution and source mechanisms governing the unusual lithium and boron enrichment in salt lakes of northern Tibet Available to Purchase
Strontium isotopes and rare earth elements in terrestrial hot-spring deposits: Characterization and geothermal implications Available to Purchase
Travertine records climate-induced transformations of the Yellowstone hydrothermal system from the late Pleistocene to the present Available to Purchase
Biotic-Abiotic Radial-Acicular Crystal Fan Fabrics with Rosickýite at the Angel Springs Tufa-Travertine Deposit in Southern British Columbia Available to Purchase
Hydrology Drives Crustal Deformation and Modulates Seismicity in the Matese Massif (Italy) Available to Purchase
Water quality of the southern Tibetan Plateau: hydrogeochemical assessment of the Yarlungzangbo River Available to Purchase
Are They Everywhere? – Benthic Foraminifera From Saline Springs in Central Germany Open Access
Tectonic control of thermal springs, gas vents and travertine deposition in Bagni di San Filippo and Campiglia d’Orcia area (Monte Amiata Volcano-Geothermal area, Italy) Available to Purchase
Surface expression of Late Caledonian magmatic lithium concentration, in the Rhynie Chert, UK Open Access
Hydrology and geology of the Fernow Experimental Forest, West Virginia, USA Available to Purchase
ABSTRACT The Fernow Experimental Forest (the “Fernow”) is an 1860-ha (4600-acre) research forested watershed in Parsons, West Virginia, USA. The Fernow has been in operation since 1934 and has historically been the site of timbering and silvicultural research programs. Beginning in the 1950s, a water quality research program was established in the Fernow to assess the effects of different forestry management techniques on water quantity and quality. As a result, most peer-reviewed research from the Fernow has focused on water quality data directly related to forestry efforts with little mention of the effects of geology, hydrogeology, or climate on water resources in the Fernow. Further, the Fernow is representative of Appalachian headwater mountain watersheds and is a protected and secure research site in the greater Monongahela National Forest. This, in combination with the long-term data records from the water research program, make the Fernow an ideal location for further geologic and hydrologic investigations in forested mountain watersheds. The geology of the Fernow is dominated by moderately dipping Paleozoic-aged strata with local karst features (e.g., springs) occurring in one unit. The hydrology of the Fernow consists of intermittent and perennial streams that are reactive to seasonal weather patterns. This field guide serves as an overview of the geology and hydrology of the Fernow and surrounding region to be used as a teaching and recruitment tool to advance the geologic understanding of Allegheny Mountain headwaters.
Karst hydrogeology of the Chalk and implications for groundwater protection Open Access
Abstract The Chalk is an unusual karst aquifer with limited cave development, but extensive networks of smaller solutional conduits and fissures enabling rapid groundwater flow. Small-scale karst features (stream sinks, dolines, dissolution pipes, and springs) are common, with hundreds of stream sinks recorded. Tracer velocities from 27 connections between stream sinks and springs have median and mean velocities of 4700 and 4600 m d −1 . Tests to abstraction boreholes also demonstrate very rapid velocities of thousands of metres per day. Natural gradient tests from observation boreholes have rapid velocities of hundreds of metres per day. There is strong geological control on karst with dissolution focused on stratigraphical inception horizons. Surface karst features are concentrated near the Paleogene boundary, or where thin superficial cover occurs, but rapid groundwater flow is also common in other areas. The Chalk has higher storage and contaminant attenuation than classical karst, but recharge, storage and flow are influenced by karst. Point recharge through stream sinks, dolines, losing rivers, vertical solutional fissures, and soakaways enables rapid unsaturated zone flow. Saturated zone networks of solutional fissures and conduits create vulnerability to subsurface activities, and enable long distance transport of point source and diffuse pollutants, which may be derived from outside modelled catchment areas and source protection zones.