PENNSYLVANIA COUNCIL of
PROFESSIONAL GEOLOGISTS
 

Hydrostructural Geology: The Geology within Hydrogeology (405 mins.)

  • August 18, 2020
  • 8:00 AM - 4:30 PM
  • Regional Learning Alliance, Cranberry Township, PA
  • 22

Registration

  • Member registration closes August 10 or when sold out.
  • Non-member registration closes July 30 or when sold out. If you'd like to save $100 off the cost of enrollment, return to home page and Join PCPG.

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Regional Learning Alliance*
850 Cranberry Woods Drive    DIRECTIONS
Cranberry Twp., PA

*Host facility's Health & Safety Protocols.

PCPG seminars quickly sell out. To confirm your seat, use our secure web enrollment and a credit card.

8:00: Registration Opens
8:30 - 4:30:  Seminar, with breaks/lunch provided.

Instructor

Thomas D. Gillespie P.G., Sr. Professional Geologist
Gilmore & Associates, Inc.

Download Agenda/Bio


Professional Development Conversion Formulas
DE, SC 60 mins. = 1 CEU
PA 50 mins. = 1 PDH 

Level:  Advanced

Overview: Unlike the mental imagery geologists construct of groundwater flow through a porous medium, investigators in fractured rock aquifers must first visualize the three-dimensional network of water-conducting planes before considering how the spacing, orientation and interconnection of those planes control and constrain gravity-driven flow. Complicating that visualization even further, it is usually the case that none of the sets of intersecting, non-randomly-oriented planes are aligned parallel to the prevailing hydraulic gradient.

     Combining a refresher on the concepts and methods of structural geology with quantitative analysis of groundwater flow within and between discrete, connected flow pathways, this full day, hands-on course provides the tools of both visualization and quantification of gravity-driven flow in three-dimensional space. Including a complete review of the methods of planar structural analysis, the course explores: structurally-controlled deflection of contaminant plumes; the effects of the scale of observation on aquifer heterogeneity and anisotropy; migration of separate phase liquids and gases; and groundwater flow within structural domains of differing, yet overlapping, scales of observation from individual fractures to wells, sites, through study areas and regional flow systems.

Pennsylvania Council of Professional Geologists
116 Forest Drive, Camp Hill, Pennsylvania 17011



 
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