PPT-Geology of the San Juan Basin, New Mexico

Matthew Dixon Emil Johnson Is coal bearing bedrock formation Formerly known as the callop formation The Dalton Sandstone unit NonMarine Unit Crevasse Canyon Late Jurassic 865 thickness. email pdggeopccal3vsnlnetin In the Lower Gondwana succession of the Jharia basin of eastern India the Barren Measures Formation is characterized by the cyclic disposition of 64257negrained lacustrine deposits and relatively coarsegrained 64258uvial San Juan-. Pagosa. Springs(PSPC2). Upper (11000-12644). Middle (8500-11000). Lower (7198-8500). San Juan-. Pagosa. Springs(PSPC2). In reality the 3 areas (upper, middle and lower) are represented (simulated) by only 3 points. Basin and Range. Climate. Very hot. Hottest temperature was in 1934 at 116 degrees. Dry climate. Few streams. Rain Shadow effect. Air travels east over the Pacific Ocean gathers moisture and then when it reaches the Sierra Nevada Mountains suck most of the moisture out of the air. The air that gets to New Mexico holds very little moisture which causes our hot dry climate. “Comparing the air of cities to the air of deserts and arid lands is like comparing waters that are befouled and turbid to waters that are fine and pure. In the city, because of the height of its buildings, the narrowness of its streets, and all that pours forth from its inhabitants and their superfluities…the air becomes stagnant, turbid, thick, misty, and foggy…If there is no choice in this matter, for we have grown up in the cities and have become accustomed to them, you should…select from the cities one of open horizons…endeavor at least to dwell at the outskirts of the city…”. Naming Conventions, Birth Certificates, and Immunization Records. Sonja Williams. Migrant Education Program. NCDPI. Understanding Hispanic Naming Conventions. Words to know. Nombres. =First names. Example: . de . Guadalupe/. Our . Lady . of Guadalupe. The Aztecs. The Aztecs ruled most of Central America in 1500. Empire was known as Mesoamerica; extended from the Gulf of Mexico to the Pacific Ocean. Moctezuma. EnergyPlex. Conference – Hobbs, New Mexico. Jeff Bennett, President and General Manager – New Mexico Delaware Basin. Occidental Petroleum Overview. Occidental in the Permian Basin/Highlights. Permian Basin Highlights. Estanlislao. Andrés Lucero. Thursday, November 5, 2015. La . Cosecha. 2015 Albuquerque, New Mexico. Stanley Andres Lucero. 1. I am a Manito, a . genízaro. , a coyote, a Spanish American with deep roots in New Mexico with both Native American and European ancestors. As I traced my ancestors, I also learned about the places where they settled including: . Pagosa. Springs(PSPC2). Upper (11000-12644). Middle (8500-11000). Lower (7198-8500). San Juan-. Pagosa. Springs(PSPC2). In reality the 3 areas (upper, middle and lower) are represented (simulated) by only 3 points. Spanish Exploration in Texas The Search for Gold, God, and Glory Mr. Wayne E. Davidson M.Ed. Da Vinci School for Science and the Arts The Arrival of Spain in Texa s Earliest Expeditions Cabeza de Alteration and Geochemistry of Clinkers in the San Juan Basin, New Mexico. Devlon R. Shaver. 1. , Virginia T. McLemore. 2. , and Evan J. Owen. 2. 1. Department of Mineral Engineering, New Mexico Institute of Mining and Technology, Socorro, New Mexico 87801. Episyenites. in Southern New Mexico. By Adam Smith. Episyenites. Hypothesis: . Episyenites result of fenitization from fluids related to . Cambro. -Ordovician alkaline magmatism . 525-457 . Ma in . NM and CO. Climate. Very hot. Hottest temperature was in 1934 at 116 degrees. Dry climate. Few streams. Rain Shadow effect. Air travels east over the Pacific Ocean gathers moisture and then when it reaches the Sierra Nevada Mountains suck most of the moisture out of the air. The air that gets to New Mexico holds very little moisture which causes our hot dry climate. OLUWOLE A. OYEDEJI . PRESENTATION OUTLINE. Sedimentary Basins. Location. Dahomey. OR Benin . Basin . –Origin and . Morphology. Geology . of . Ogun. . state. Economic Geology. Geotourism. sites.