'Columbia river basalt group' diaporamas de présentation

Lecture 5 Tectonic Landforms

Lecture 5 Tectonic Landforms. Landforms that result from crustal movements Landforms with little erosion so "their shape defines a fractured or deformed surface" Bloom. Escarpment or "scarp". Tectonic Scarp: steep slope from differential movement of surface. Basaltic Lava Flows.

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Hydrologic Conditions in the Palouse Aquifer

Hydrologic Conditions in the Palouse Aquifer. Dale R. Ralston Professor Emeritus of Hydrogeology University of Idaho. Outline of talk. Introduction Ground water management concepts Description of the Palouse aquifer Well development and water level decline

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OUTLINE

Groundwater Recharge, Storage, and Discharge mechanisms of the Colombia Plateau Regional Aquifer System (CPRAS). OUTLINE. ORGANIZATION OF PRESENTATION Introduction/Setup Purpose Location Geology Hydrogeologic Setup Mechanisms/Analysis Recharge to aquifer Storage in aquifer

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Chapter 15: Continental Flood Basalts

Chapter 15: Continental Flood Basalts. Large Igneous Provinces (LIPs) Oceanic plateaus Some rifts Continental flood basalts (CFBs). Figure 15-1. Columbia River Basalts at Hat Point, Snake River area. Cover of Geol. Soc. Amer Special Paper 239. Photo courtesy Steve Reidel.

365 views • 17 slides

Ch 173-218 WAC Underground Injection Control Program Rule Revision

Ch 173-218 WAC Underground Injection Control Program Rule Revision. Geologic Sequestration of Carbon Dioxide. Washington Climate Change Legislation: ESSB 6001. Passed in April 2007 Requires Ecology and EFSEC to develop rules for the Geologic Sequestration of Carbon Dioxide.

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Acknowledgments

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Weather in eastern W ashington

Weather in eastern W ashington. By Billy hunter. Washington has four unique seasons with four different weather patterns.

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