{"title":"Diurnal Fluctuations of Arsenic Concentrations and Physiochemical Parameters along the Jemez River, New Mexico","authors":"L. Garcia, Daryl J. Williams, E. Martinez","doi":"10.56577/sm-2013.87","DOIUrl":"https://doi.org/10.56577/sm-2013.87","url":null,"abstract":"Snow pack dominated rivers and streams across the Southwestern United States have been feeling the effects of global climate change, which mainly include increasing temperatures and decreasing amounts of precipitation, especially precipitation in the form of snow. Over the past 50 years the Jemez River regions has experienced a 2oF increase in ambient air temperature, as well as a 40% decrease in stream discharge. Spanning roughly 129 km and contributing more than 50,000,000 cubic meters of water to the Rio Grande River annually, the Jemez River is the largest tributary to the Middle Rio Grande Basin. Further complicating matters, the surrounding geology of the Jemez River is of volcanic origin which is responsible for the many hydrothermal springs and seeps in the area, which allow for","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"6 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121196708","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
P. Longmire, M. Dale, K. Granzow, D. Carlson, Benjamin Wear, Jerzy Kulis, G. Perkins, M. Rearick
{"title":"Hydrochemistry of Lava Tube Spring and the Rio Grande, Taos County, New Mexico","authors":"P. Longmire, M. Dale, K. Granzow, D. Carlson, Benjamin Wear, Jerzy Kulis, G. Perkins, M. Rearick","doi":"10.56577/sm-2013.46","DOIUrl":"https://doi.org/10.56577/sm-2013.46","url":null,"abstract":"","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"22 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126235030","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Proterozoic Zoned Intrusive Suites: Determining the Surficial Relationships and Emplacement Mechanisms of the Burro Mountain Intrusive Suite","authors":"S. Gaynor, J. Amato","doi":"10.56577/sm-2013.82","DOIUrl":"https://doi.org/10.56577/sm-2013.82","url":null,"abstract":"","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"2 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122661863","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Structural control of warm springs in the Hillsboro-Lake Valley area","authors":"S. Kelley, Mussie Tewelde, J. Witcher, M. Person","doi":"10.56577/sm-2013.69","DOIUrl":"https://doi.org/10.56577/sm-2013.69","url":null,"abstract":"","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"114 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128131631","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Campanian Ammonites and Other Molluscs from the Pictured Cliffs Sandstone, Sandoval County, New Mexico","authors":"P. Sealey, Charles A. Turner, S. Lucas","doi":"10.56577/sm-2013.17","DOIUrl":"https://doi.org/10.56577/sm-2013.17","url":null,"abstract":"","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"67 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121462255","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Acquiring and Georeferencing Coal Mine Maps: San Juan Basin, NM","authors":"Gretchen K. Hoffman, Maureen Wilks","doi":"10.56577/sm-2013.9","DOIUrl":"https://doi.org/10.56577/sm-2013.9","url":null,"abstract":"","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"47 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133189420","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Reesidites minimus from the Juana Lopez Member of the Mancos Shale, Sandoval County, New Mexico: a Very Rare Ammonite in North America","authors":"P. Sealey, S. Lucas","doi":"10.56577/sm-2013.6","DOIUrl":"https://doi.org/10.56577/sm-2013.6","url":null,"abstract":"","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130775555","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Vertebrate Body Fossils From The Upper Pennsylvanian (Lower Wolfcampian) Bursum Formation, East Of Socorro, New Mexico","authors":"T. L. Suazo, A. Cantrell, S. Lucas","doi":"10.56577/sm-2013.38","DOIUrl":"https://doi.org/10.56577/sm-2013.38","url":null,"abstract":"The Upper Pennsylvanian (lower Wolfcampian) Bursum Formation east of Socorro, New Mexico, has been interpreted as the transition between underlying Upper Pennsylvanian shallow marine carbonate-dominated deposits and overlying Lower Permian continental red beds of the Abo Formation. Composed of interbedded marine carbonates and nonmarine red beds, exposures of the Bursum Formation produce a diverse assemblage of vertebrate body fossils. These include teeth of the dipnoan Sagenodus; teeth of the chondrychthians Deltodus, Hybodus, Acrodus and Petalodus; a partial clavicle of the temnospondyl amphibian Eryops; diadectid jaw fragments; a bolosaur? jaw fragment; a partial embolomere centrum; and various cranial and postcranial elements of the sphenacodontid eupelycosaur Sphenacodon. Vertebrate-body-fossil-producing beds in the Bursum Formation east of Socorro are stratigraphically high in the formation, occurring in the uppermost 5-10 meters. Facies that yield fossil bone vary from fluvially-deposited mudrocks and sandstones to marine-influenced carbonate conglomerates, with the majority of the fossil bones recovered from the latter. Despite the Bursum Formation being older and having a greater abundance of marine sediments than the Abo Formation, both units produce a tetrapod fauna that includes diadectids and eryopids and that is sphenacodontid dominated. However, the relatively numerous and diverse marine shark’s teeth from the Bursum differentiate its vertebrate fauna from that of the Abo Formation. The similarity of tetrapod taxa recovered from the Bursum and Abo formations east of Socorro shows that, despite changes from a mixed marine/nonmarine environment to a fully terrestrial environment, many taxa persisted from the Late Pennsylvanian into the Early Permian.","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"56 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134334043","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pavel Vakhlamov, L. Crossey, C. Dahm, V. Acu??a, A. Ali
{"title":"Evaluating Solute Sources in the Upper Gila River, NM","authors":"Pavel Vakhlamov, L. Crossey, C. Dahm, V. Acu??a, A. Ali","doi":"10.56577/sm-2013.86","DOIUrl":"https://doi.org/10.56577/sm-2013.86","url":null,"abstract":"","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"28 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"132900562","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"A Major Landslide involving an Inverted Paleochannel in Sierra County, New Mexico","authors":"Gérald, Lindsey","doi":"10.56577/sm-2013.5","DOIUrl":"https://doi.org/10.56577/sm-2013.5","url":null,"abstract":"A landslide that probably dates to the end of the Pleistocene has been found adjacent to the the New Mexico Spaceport. The feature consists of three subparallel segments partitioned by southeast trending drainages, covering an area about 8 km wide and 10 km long. It lies just off Sierra County road A013 and Apache Gap road near the entrance to the spaceport site. The head of the slide deposits consist of a northeast trending truncated paleochannel forming an inverted topographic ridge. The best view of the slide are satellite photos that show the offset of the paleochannel and the transverse ridges and swales pattern comprising the bulk of the slide body. The head of the slide is partly underlain by the Cretaceous Crevasse Canyon Formation and the Tertiary Love Ranch Formation. The slide plane is approximated as the unconformable contact between these two formations and likely facilitated by a clay stratum near the base of the the Tertiary deposits. The paleochannel deposits, with some rounded intrusive rock boulders with sizes up to 1.5 meters diameter, indicate a very high flow rate. A series of northwest trending faults have acted as shear zones separating and truncating the landslide segments. The western segment has been washed away leaving only trace evidence of the slide body. A low slide plane angle of less than one percent suggests a seismic trigger.","PeriodicalId":363585,"journal":{"name":"Proceedings Volume: \"Hydrology and History of the Rio Grande\", New Mexico Geological Society, 2013 Annual Spring Meeting","volume":"25 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2013-04-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115844876","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}