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Academic literature on the topic 'Rock Springs District'

Author: Grafiati

Published: 4 June 2021

Last updated: 28 July 2025

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Journal articles on the topic "Rock Springs District"

1

Tuyu, Krisman. "Groundwater Conditions and Springs Potency for Domestic Requirement in Klaten and Banggai Kepulauan Regency, Indonesia." IOP Conference Series: Earth and Environmental Science 1233, no. 1 (2023): 012060. http://dx.doi.org/10.1088/1755-1315/1233/1/012060.

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Abstract At present, sustainable management of water resources has become a major issue for the world community. In water management efforts, potency assessment becomes an important thing. The purpose of this study is to analyze the availability of ground water and water from springs both qualitatively and quantitatively and evaluate their potency for domestic. To determine the groundwater conditions in the research area, a qualitative descriptive analysis was carried out based on geological and hydrogeological data. To determine the potency of the springs, a quantitative descriptive analysis

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Pongoh, Oliver, Donny Royke Wenas, and Theresje Mandang. "STUDI KARAKTERISTIK BATUAN MANIFESTASI PANAS BUMI DI SEKITAR GUNUNG TAMPUSU." Jurnal FisTa : Fisika dan Terapannya 1, no. 2 (2020): 67–72. http://dx.doi.org/10.53682/fista.v1i2.93.

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North Sulawesi is one of the provinces in Indonesia which has many active volcanoes. Mount Tampusu is an area that has geothermal prospects characterized by geothermal manifestations on the surface, namely hot springs that can contribute to or influence the surrounding rocks making altered rocks within the scope of hot spring manifestations. This study aims to identify the mineral composition and type of alteration rock in the geothermal manifestation area around Mount Tampusu at the study site using SEM-EDX and FTIR methods to determine hydrothermal minerals present in these rocks. The result

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3

Karubaba, Andrew, Irwan Iskandar, and Syafrizal. "HYDROGEOCHEMICAL AND STABLE ISOTOPE ANALYSIS OF KEBAR HOT SPRINGS MANOKWARI DISTRICT, WEST PAPUA PROVINCE." INTAN Jurnal Penelitian Tambang 6, no. 2 (2023): 54–64. http://dx.doi.org/10.56139/intan.v6i2.189.

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In simple terms, geothermal classification is determined according to reservoir equilibrium, fluid type, and temperature. Based on the reservoir temperature, geothermal systems are separated into two different systems: dynamic system (convection) and static system (conduction). This system structure is also affected by topography which is further specified as a high-temperature fluid reservoir. The relationship between the characteristics of the hot springs and geothermal potential is instructive to be analyzed. The objective of the analysis is to determine critical parameters: The chemical co

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4

Thapa, Ram Singh, Rajan Subedi, Jayesh Desai, Moti Lal Rijal, Krishna Raj Tiwari, and Pem Narayan Kandel. "Identifying potential recharge areas of mountain springs through hydrogeological mapping." Banko Janakari 33, no. 1 (2023): 3–15. http://dx.doi.org/10.3126/banko.v33i1.55463.

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Springs are the primary source of water for the people inhabiting in the hills and mountain regions of Nepal. Climate variability, climate change, land use change and management factors together with various human activities including haphazard infrastructure development like urbanization and road construction over the recharge area are responsible for drying up of springs in the hills and mountains, especially in the mid-hill region of Nepal. This study attempts to identify the potential recharge zones of the springs within the four catchments viz. Banlekh and Shikharpur of Baitadi and Doti d

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5

Mulyadi, Eddy, and Arif Munandar. "Characteristics of Geology, Geochemistry, Geophysics in Assessing the Geothermal Potential of the Bonjol Region, Pasaman, West." International Journal of Science and Society 5, no. 2 (2023): 293–303. http://dx.doi.org/10.54783/ijsoc.v5i2.694.

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The purpose of this study was to determine the Characteristics of Geology, Geochemistry, Geophysics in Assessing the Geothermal Potential of the Bonjol Region, Pasaman, West Sumatra. The Bonjol geothermal area is included in the Bonjol District, Pasaman Regency, West Sumatra Province. The rocks in the study area can be divided into 13 rock units, namely two sedimentary rock units, 10 volcanic rock units, and one surface sediment unit, while geothermal manifestations in the research area are scattered in the central part which is dominated by the emergence of hot springs in Padang Baru, Takis R

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6

Chen, Z., X. Zhou, J. Du, et al. "Hydrochemical characteristics of hot spring waters in the Kangding district related to the Lushan <i>M</i><sub>S</sub> = 7.0 earthquake in Sichuan, China." Natural Hazards and Earth System Sciences 15, no. 6 (2015): 1149–56. http://dx.doi.org/10.5194/nhess-15-1149-2015.

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Abstract. Hydrogeochemistry of 10 hot springs in the Kangding district was investigated by analyzing cation and anion concentrations in the spring water. The water samples were collected in the 5 days after the Lushan MS = 7.0 earthquake, which occurred on 20 April 2013. The spring waters are classified into seven chemical types based on their hydrochemical compositions. Compared with hydrochemical data before the Lushan earthquake, concentrations of Ca2+, HCO3- and total dissolved solid (TDS) in water samples from the Guanding, Erdaoqiao, Gonghe, Erhaoying, Tianwanhe and Caoke springs signifi

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7

Khawajah, Mohammad A., Ahmad A. Al-Taani, Abeer I. Al-Zoubi, and Abeer A. Al-Hamad. "GIS and Water Quality Index Based to Assess Spring Water Quality, A Case Study of Bani Kinanah District, Irbid, Northwestern Jordan." Indonesian Journal on Geoscience 10, no. 3 (2023): 393–405. http://dx.doi.org/10.17014/ijog.10.3.393-405.

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Springs in northwestern Jordan are significant sources of freshwater for local communities. The reliance on springs to fulfill the growing demands for water has been intensified in the past decade, following the decline in rainwater due to climate change. Thirty water samples were collected from springs located in Bani Kinanah District, northwest Jordan, and tested for various water quality parameters, including pH, EC, TDS, Na+, Ca+2, Mg+2, K+, Cl-, F-, SO4-2, NO3-, TH, TA, Fe, Mn, Pb, and Zn. The results show that most water quality variables fall within the acceptable limits for drinking wa

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8

Arifin, M. Fauzi, Hendra Fachri, and Busthan Azikin. "Geochemical Analysis of Hot Springs in Massepe, Tellu Limpoe Sidenreng Rappang Regency, South Sulawesi Province, Indonesia." International Journal of Islamic Education, Research and Multiculturalism (IJIERM) 5, no. 2 (2023): 314–31. http://dx.doi.org/10.47006/ijierm.v5i2.223.

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Location of the study is administratively located in the District Tellu Limpoe, Sidenreng Rappang Regency in South Sulawesi Province. Geographically located at coordinate 119°47'00" – 119°49'00" east longitude and 04°00'00"– 04°02’00" latitude. This study aims to determine the geological conditions and geochemical, it is hot spring types, and subsurface temperature of the geothermal Massepe area Sidenreng Rappang district of South Sulawesi Province. Methods of research are conducted in the form of data collection methods and methods of geological and geochemical laboratory analysis. The geomor

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Bhutia, Namgyal Tshewang, and Malavika Sinha. "Geo-physical attributes of Shushunia’s aquifer, Chhatna block, Bankura district, West Bengal, India." Landscape & Environment 17, no. 2 (2023): 1–11. http://dx.doi.org/10.21120/le/17/2/1.

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Shushunia hill lies in a transitional zone of the South Singbhum Mobile Craton and northern Gondwana formation. The Shushunia hill appears like a porcupine peak and it has structural similarity to the Eastern Ghat. The Shushunia hill zone is an example of a contact spring. In the foothill zone, two perennial springs are observed. The study purely deals with its aquifer and water quality. Based on the present rock strata and the nature of the contact aquifer, its early condition has been assumed. The discharge of the confined aquifers occurs by leakage. The water temperature depicts the springs

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10

Chen, Zhi, Jianguo Du, Xiaocheng Zhou, et al. "Hydrochemistry of the Hot Springs in Western Sichuan Province Related to the WenchuanMS8.0 Earthquake." Scientific World Journal 2014 (2014): 1–13. http://dx.doi.org/10.1155/2014/901432.

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Hydrogeochemistry of 32 hot springs in the western Sichuan Province after the WenchuanMS8.0 earthquake was investigated by analyzing the concentrations of cation and anion and the isotopic compositions of hydrogen and oxygen. The water samples of the hot springs were collected four times from June 2008 to April 2010. Hydrogeochemical data indicated the water samples can be classified into 9 chemical types. Values ofδD andδ18O indicated that the spring waters were mainly derived from meteoric precipitation and affected by water-rock interaction and mixture of deep fluids. Concentrations of K+an

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Books on the topic "Rock Springs District"

1

Engineering, Nelson. Westside/Rock Springs water supply project. Nelson Engineering, 1998.

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2

United States. Bureau of Land Management. Rock Springs District., ed. Final Rock Springs wilderness environmental impact statement for the Rock Springs District (Fremont, Lincoln, Sublette, and Sweetwater Counties). The District, 1990.

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United States. Bureau of Land Management. Rock Springs District. Final Rock Springs wilderness environmental impact statement for the Rock Springs District (Fremont, Lincoln, Sublette, and Sweetwater Counties). The District, 1990.

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United States. Bureau of Land Management. Rock Springs District. Revised draft, wilderness environmental impact statement for the Rock Springs District, Wyoming (Fremont, Lincoln, Sublette and Sweetwater counties, Wyoming). The District, 1988.

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5

United States. Bureau of Land Management. Record of decision for the Kemmerer resource management plan and rangeland program summary document, Kemmerer Resource Area, Rock Springs District, Lincoln, Sweetwater, and Uinta counties, Wyoming. U.S. Dept. of the Interior, Bureau of Land Management, Kemmerer Resource Area, 1986.

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6

Final Rock Springs wilderness environmental impact statement for the Rock Springs District (Fremont, Lincoln, Sublette, and Sweetwater Counties). The District, 1990.

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7

Final Rock Springs wilderness environmental impact statement for the Rock Springs District (Fremont, Lincoln, Sublette, and Sweetwater Counties). The District, 1990.

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Book chapters on the topic "Rock Springs District"

1

Sims, P. K. "Central City and Idaho Springs districts, Front Range, Colorado." In Mineral Deposits and Geology of Central Colorado: Red Rocks Park to Cripple Creek, Colorado July 2–8, 1989. American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft129p0015.

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2

Petrov, Oleg, Edward Prasolov, Sergey Sergeev, and Yury Pushkarev. "Isotope Correlations in Rocks and Ores of Major Intrusions in the Norilsk District." In Springer Geology. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-05216-4_7.

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3

Varade, Abhay M., Y. D. Khare, Mukesh Sakhare, et al. "Investigation of Lineaments for Identification of Deeper Aquifer Zones in Hard Rock Terrain: A Case Study of WRWB-2 Watershed from Nagpur District, Central India." In Springer Hydrogeology. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-62397-5_14.

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4

Bethke, Craig M. "Hydrothermal Fluids." In Geochemical Reaction Modeling. Oxford University Press, 1996. http://dx.doi.org/10.1093/oso/9780195094756.003.0020.

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Hydrothermal fluids, hot groundwaters that circulate within the Earth’s crust, play central roles in many geological processes, including the genesis of a broad variety of ore deposits, the chemical alteration of rocks and sediments, and the origin of hot springs and geothermal fields. Many studies have been devoted to modeling how hydrothermal fluids react chemically as they encounter wall rocks, cool, boil, and mix with other fluids. Such modeling proliferated in part because hydrothermal fluids are highly reactive and because the reaction products are commonly well preserved, readily studie

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5

Krahulec, Kenneth A. "History and Production of the West Mountain (Bingham) Mining District, Utah." In Geology and Ore Deposits of the Oquirrh and Wasatch Mountains, Utah. Society of Economic Geologists, 1998. http://dx.doi.org/10.5382/gb.29.15.

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Abstract Erastus Bingham and his two sons, Thomas and Sanford, began ranching in a wooded canyon in the Oquirrh Mountains in 1848. This was a year after the Latter-day Saint (LDS) pioneers entered the Great Salt Lake Valley, then a part of Mexico (Arrington and Hansen, 1963). They were probably the first Caucasians to recognize mineralized rock in the Oquirrh Mountains and brought their discovery to LDS President Brigham Young.1 Young, however, wisely counseled the Saints to settle and farm Utah to provide the necessities of life and avoid the pursuit of precious metals: Instead of hunting gol

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6

Hayashi, Toshihiko, and Sachihiro Taguchi. "Epithermal Gold Exploration in the Iriki District, Kagoshima, Japan." In Epithermal Gold Mineralization and Modern Analogues, Kyushu, Japan. Society of Economic Geologists, 2001. http://dx.doi.org/10.5382/gb.34.07.

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Abstract The Iriki district was chosen by the Metal Mining Agency of Japan (MMAJ) as a target for epithermal gold exploration on the basis of the following criteria: the presence of steam-heated acid alteration, a gravity anomaly high, geochemical characteristics of hot spring water similar to those of water from the Hishikari gold deposit, and old mining activity. In 1994 and 1995 the MMAJ carried out exploration that included alteration mapping, geochemical and geophysical surveys, and diamond drilling. of note, several drill holes intersected gold mineralization returning approximately 6 g/

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7

Wilkerson, Gregg, and Larry Vredenburgh. "Roadside geology and mining history of the Bodie and Aurora districts, Mono County, California, and Mineral County, Nevada." In Field Excursions to the Northern Sierra Nevada of California, the Mining Districts of the Sierra Nevada, and Cretaceous and Paleocene Sediments in Maryland, USA. Geological Society of America, 2023. http://dx.doi.org/10.1130/2023.0065(04).

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ABSTRACT This field trip explores the geology and mining history of the Bodie Hills with a focus on the Bodie and Aurora mining districts. The field trip starts and ends in Bridgeport, California. Our first geologic stop is at Travertine Hot Springs, which provides an analogy for the style of mineralization observed in the Bodie and Aurora districts. We then proceed south on Highway 395 to the Bodie exit at Highway 270. At this location on Highway 395 is the placer camp of Dogtown with outcrops of till from the Sherwin glaciation. A side trip up Cinnabar Canyon exposes rocks with veinlets of c

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8

Pickthdrn, William J. "Relation of Hot-Spring Gold Mineralization to Silica-Carbonate Mercury Mineralization in the Coast Ranges, California." In Active Geothermal Systems and Gold-Mercury Deposits in the Sonoma-Clear Lake Volcanic Fields, California. Society of Economic Geologists, 1993. http://dx.doi.org/10.5382/gb.16.05.

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Abstract The discovery of the McLaughlin hot-spring type gold deposit in the old Knoxville mercury district sparked considerable interest and research into the origin and relation of mercury and epithermal gold mineralization in the California Coast Ranges Province. Silica-carbonate mercury mineralization occurs throughout the Coast Ranges, from Santa Barbara County in the south to Lake and Colusa counties in the north (Fig. 1). Since their discovery in the mid 1800’s California’s Coast Ranges mercury deposits have produced over 50% of the total production for the United States, and two of the

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9

Lexa, J., J. Štohl, and V. Konečný. "The Banská Štiavnica ore district." In Epithermal Mineralization of the Western Carpathians. Society of Economic Geologists, 1999. http://dx.doi.org/10.5382/gb.31.09.

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Abstract The Banská Štiavnica ore district is in the central zone of the largest stratovolcano in the Central Slovakia Neogene Volcanic Field, which is situated at the inner side of the Carpathian arc over the Hercynian basement with the Late Paleozoic and Mesozoic sedimentary cover. Volcanic rocks of the High-K orogenic suite are of the Badenian through Pannonian age (16.5– 8.5 Ma). Their petrogenesis is closely related to subduction of flysch belt oceanic basement underneath the advancing Carpathian arc and to back-arc extension processes. The stratovolcano includes a large caldera 20 km in

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Colopy, Cheryl. "The Garland." In Dirty, Sacred Rivers. Oxford University Press, 2012. http://dx.doi.org/10.1093/oso/9780199845019.003.0020.

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Bundelkhand is a thirsty land. When I arrived there early in 2008, my skin—already parched from the dry winter air of Kathmandu and Delhi—immediately felt itchy. The cool air hit my sinuses with a prickly thud. They ached, and my eyes smarted as moisture left them. The land was an expanse of beige sand and rocks; beautiful, I thought, save for a dryness so intense it made me feel a little anxious. Most of the trees were not very tall, except for the water-thrifty “flame of the forest,” with its dark green dust-covered leaves, several inches wide. In the spring the leaves drop off and the tree’

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Conference papers on the topic "Rock Springs District"

1

Szymanski, Eugene, Michael Vanden Berg, Nathan Moodie, et al. "ASSESSING THE GEOLOGIC CARBON (CO2) SEQUESTRATION POTENTIAL OF MULTIPLE SUBSURFACE TARGETS IN THE IRON SPRINGS DISTRICT, IRON COUNTY, UTAH." In Joint 118th Annual Cordilleran/72nd Annual Rocky Mountain Section Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022cd-373696.

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Acheampong-Mensah, Abena Serwah, and Virginia T. McLemore. "Geochemistry of critical minerals in mine wastes at Hillsboro and Steeple Rock districts, New Mexico." In 2023 New Mexico Geological Society Annual Spring Meeting. New Mexico Geological Society, 2023. http://dx.doi.org/10.56577/sm-2023.2930.

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Acheampong-Mensah, Abena Serwah, Virginia T. McLemore, Nicole Hurtig, and Alexander Gysi. "Geochemistry of critical minerals in mine waste at Hillsboro and Steeple Rock districts, New Mexico." In 2024 New Mexico Geological Society Annual Spring Meeting. New Mexico Geological Society, 2024. http://dx.doi.org/10.56577/sm-2024.3009.

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4

Li, Yitian, Ingar F. Walder, and Bonnie Frey. "Evaluation of Leaching Tests on Uranium Bearing Waste Rocks From Grants Mineral District, New Mexico." In 2016 New Mexico Geological Society Annual Spring Meeting. New Mexico Geological Society, 2016. http://dx.doi.org/10.56577/sm-2016.470.

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5

Hahn, F., S. Klein, J. Güldenhaupt, T. Seidel, and T. König. "The High Temperature-Mine Thermal Energy Storage (HT-MTES) Project in Bochum, Germany." In 57th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2023. http://dx.doi.org/10.56952/arma-2023-0443.

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ABSTRACT The aim of the German HEATSTORE sub-project has been the development of a mine thermal energy storage (MTES) pilot plant for the energetic reuse of an abandoned small colliery below the premises of the Fraunhofer IEG in Bochum, Germany. In the summer 2020 three wells have been drilled into existing open mine voids from the IEG drilling site. During the winter of 2020/2021, a first MTES test operation has been carried out. The underground temperature has been recorded before, throughout and after a test operation by Distributed Temperature Sensing (DTS) as well as groundwater temperatu

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Reports on the topic "Rock Springs District"

1

Gavin, Greg, Paul Inkenbrandt, Trevor Schlossnagle, and Rebecca Molinari. Groundwater of Pahvant Valley, Millard County, Utah. Utah Geological Survey, 2024. http://dx.doi.org/10.34191/ss-173.

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Pahvant Valley, located in Millard County, Utah, encompasses 1610 square miles and includes several small towns, agricultural districts, hot springs, and biologically important wetlands, all heavily reliant on groundwater. This study, conducted by the Utah Geological Survey during 2022 and 2023, aims to define Pahvant Valley’s water recharge and discharge estimates, characterize its primary hydrogeologic units, and describe groundwater recharge and discharge areas. The research includes the collection of groundwater and surface water samples to estimate flow paths, sources of recharge and disc

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