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U.S. Geological Survey Scientific Investigations Map最新文献

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Bathymetric map and surface area and capacity table for Beaver Lake near Rogers, Arkansas, 2018 2018年阿肯色州罗杰斯附近海狸湖的水深图、表面积和容量表
Q4 Earth and Planetary Sciences Pub Date : 2019-01-01 DOI: 10.3133/sim3445
R. Huizinga, Jarrett T. Ellis, J. Sharpe, Jessica Z. LeRoy, Joseph M. Richards
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引用次数: 0
Geostatistical estimation of the bottom altitude and thickness of the Mississippi River Valley alluvial aquifer 密西西比河流域冲积含水层底部高度和厚度的地质统计学估计
Q4 Earth and Planetary Sciences Pub Date : 2019-01-01 DOI: 10.3133/SIM3426
L. Torak, Jaime A. Painter
Painter, J.A., and Westerman, D.A., 2018, Mississippi Alluvial Plain extent, November 2017: U.S. Geological Survey data release, accessed February 22, 2018, https://doi.org/10.5066/F70R9NMJ. Reba, M.L., Massey, J.H., Adviento-Borbe, M.A., Leslie, D., Yaeger, M.A., Anders, M., and Farris, J., 2017, Aquifer depletion in the Lower Mississippi River Basin: Challenges and solutions: Journal of Contemporary Water Research and Education, v. 162, no. 1, p. 128–139, accessed August 9, 2018, at https://doi.org/10.1111/j.1936-704X.2017.03264.x.
Painter, j.a.和Westerman, d.a., 2018,密西西比冲积平原范围,2017年11月:美国地质调查局数据发布,2018年2月22日访问,https://doi.org/10.5066/F70R9NMJ。Reba, M.L, Massey, J.H, adviendo - borbe, M.A, Leslie, D, yeeger, M.A, Anders, M, and Farris, J., 2017,下游密西西比河流域含水层枯竭:挑战与解决方案:当代水研究与教育,vol . 32, no. 32。1,第128-139页,2018年8月9日访问https://doi.org/10.1111/j.1936-704X.2017.03264.x。
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引用次数: 3
Structure contour and overburden maps of the Niobrara interval of the Upper Cretaceous Cody Shale in the Wind River Basin, Wyoming 怀俄明州风河盆地上白垩统科迪页岩Niobrara段构造等高线及覆盖层图
Q4 Earth and Planetary Sciences Pub Date : 2019-01-01 DOI: 10.3133/sim3427
T. Finn
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引用次数: 0
Potentiometric surface of groundwater-level altitudes near the planned Highway 270 bypass, east of Hot Springs, Arkansas, July–August 2017 2017年7月至8月,阿肯色州温泉市东部,计划中的270号高速公路旁路附近的地下水位高度电位表
Q4 Earth and Planetary Sciences Pub Date : 2019-01-01 DOI: 10.3133/sim3444
Anna M. Nottmeier, P. Hays
The Ouachita Mountains aquifer system potentiometricsurface map is one component of the Hot Springs Bypass Groundwater Monitoring Project. The potentiometric-surface map provides a baseline assessment of shallow groundwater levels and flow directions before the construction of the Arkansas Department of Transportation planned extension of the Highway 270 bypass, east of Hot Springs, Arkansas. The map provides data regarding status of groundwater levels and potential effects on the recharge area in the Hot Springs National Park and to groundwater that supplies water to domestic users near the Highway 270 bypass. Groundwater levels from 66 wells were measured in July–August 2017. Fifty nine of the 66 groundwaterlevel altitudes measured, along with select surface-water features and springs, were used to construct the Ouachita Mountains aquifer system potentiometric-surface map. The potentiometric surface, a two-dimensional representation, shows groundwater-level altitudes ranging from a maximum of 766 ft above the North American Vertical Datum of 1988 (NAVD 88) to a minimum of 443 ft NAVD 88. The spring altitudes on the potentiometric-surface map range from 534 ft to 927 ft above NAVD 88. The study area, located in the Ouachita Mountains physiographic section of the Ouachita physiographic province, comprises narrow valleys and high ridges of Stanley Shale, Hot Springs Sandstone, Arkansas Novaculite, Missouri Mountain-Polk Creek Shale, and Bigfork Chert. The highest groundwater-level altitudes observed were in the Hot Springs Sandstone, Arkansas Novaculite, and Missouri Mountain-Polk Creek Shale. The springs discharge in outcrop areas of the Stanley Shale, Bigfork Chert, and Arkansas novaculite. The planned Highway 270 bypass will cut across ridges and valleys comprising these formations and, very importantly, across areas with elevations above 660 ft above NAVD 88 that define the hot springs recharge zone. This potentiometric-surface map defines the status of the shallow groundwater potentiometric surface near the Highway 270 bypass prior to initiation of construction activities. A postconstruction potentiometric map is planned. It must be noted that shallow groundwater levels are also subject to climatic effects including changes in amount and timing of precipitation and changes in temperature.
沃希托山含水层系统电位面图是温泉旁路地下水监测工程的组成部分之一。在阿肯色州交通部计划扩建270号高速公路绕行路段(位于阿肯色州温泉市以东)之前,这张电位测量地表图提供了浅层地下水位和水流方向的基线评估。该地图提供了有关地下水位状况的数据,以及对温泉国家公园补给区和270号高速公路旁道附近家庭用水的地下水的潜在影响。2017年7月至8月测量了66口井的地下水位。测量的66个地下水位高度中的59个,以及选择的地表水特征和泉水,被用来构建Ouachita山脉含水层系统的电位-地表图。势能面是一种二维表示,显示了地下水位高度,从1988年北美垂直基准面(NAVD 88)上方766英尺的最大值到NAVD 88上方443英尺的最小值。电位计表面图上的弹簧高度范围为NAVD 88以上534英尺至927英尺。研究区位于瓦希塔省的瓦希塔山脉地理区域,包括斯坦利页岩、温泉砂岩、阿肯色Novaculite、密苏里山-波尔克溪页岩和Bigfork燧石的狭窄山谷和高脊。观察到的最高地下水位高度是在温泉砂岩、阿肯色Novaculite和密苏里山-波尔克溪页岩。泉水在斯坦利页岩、大叉燧石和阿肯色岩浆岩的露头区域流出。计划中的270号高速公路旁路将穿过由这些地层组成的山脊和山谷,非常重要的是,穿过NAVD 88以上海拔660英尺以上的地区,这些地区定义了温泉补给区。这张电位表图定义了270号高速公路旁路附近浅层地下水电位表在施工活动开始之前的状态。绘制施工后电位图。必须指出,浅层地下水位也受气候影响,包括降水数量和时间的变化以及温度的变化。
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引用次数: 1
Extent of the Last Glacial Maximum (Tioga) glaciation in Yosemite National Park and vicinity, California 加州约塞米蒂国家公园和附近地区末次冰期高峰(梯奥加)冰川的范围
Q4 Earth and Planetary Sciences Pub Date : 2019-01-01 DOI: 10.3133/SIM3414
C. Wahrhaftig, G. Stock, R. McCracken, P. Sasnett, A. Cyr
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引用次数: 6
Geologic map of the northern Harrat Rahat volcanic field, Kingdom of Saudi Arabia 沙特阿拉伯王国哈拉特拉哈特火山区北部地质图
Q4 Earth and Planetary Sciences Pub Date : 2019-01-01 DOI: 10.3133/sim3428
D. Downs, J. Robinson, M. Stelten, D. Champion, H. Dietterich, T. Sisson, H. Zahran, K. Hassan, J. Shawali
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引用次数: 9
Geologic map of the Ferncliff and Louisa quadrangles, Louisa, Fluvanna, and Goochland Counties, Virginia 弗恩克利夫和路易莎四合院的地质图,路易莎,弗鲁瓦纳和古奇兰县,弗吉尼亚州
Q4 Earth and Planetary Sciences Pub Date : 2019-01-01 DOI: 10.3133/sim3429
W. Burton, R. W. Harrison, H. Malenda, F. Pazzaglia, E. Crider
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引用次数: 1
Stratigraphic and structural relations in trench exposures and geomorphology at the Big Burn, Lily Lake, and Lester Ranch sites, Bear River Fault Zone, Utah and Wyoming 在大Burn,莉莉湖和莱斯特牧场遗址,熊河断裂带,犹他州和怀俄明州的地层学和构造关系的海沟暴露和地貌
Q4 Earth and Planetary Sciences Pub Date : 2019-01-01 DOI: 10.3133/sim3430
S. Hecker, C. DuRoss, D. P. Schwartz, F. Cinti, R. Civico, W. Lund, A. Hiscock, M. W. West, Tarka Wilcox, A. R. Stoller
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引用次数: 1
Estimated 2016 groundwater level and drawdown from predevelopment to 2016 in the Santa Fe Group Aquifer System in the Albuquerque Area, Central New Mexico 新墨西哥州中部Albuquerque地区Santa Fe Group含水层系统2016年预估的地下水位和从开发前到2016年的下降
Q4 Earth and Planetary Sciences Pub Date : 2019-01-01 DOI: 10.3133/SIM3433
A. Galanter, L. Curry
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引用次数: 4
Geologic map of the Poncha Pass area, Chaffee, Fremont, and Saguache Counties, Colorado 蓬查山口地区,查菲,弗里蒙特和萨瓜奇县,科罗拉多州的地质图
Q4 Earth and Planetary Sciences Pub Date : 2019-01-01 DOI: 10.3133/sim3436
S. Minor, J. Caine, C. A. Ruleman, C. Fridrich, Christine F. Chan, T. Brandt, C. Holm-Denoma, L. Morgan, M. Cosca, V. Grauch
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引用次数: 2
期刊
U.S. Geological Survey Scientific Investigations Map
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