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Bill Hirt photoDepartment of Biological and Physical Sciences
College of the Siskiyous
800 College Avenue
Weed, California 96094

Office: Science 217 (7-217)

Office hours: MWF 10:00-10:50 AM, TTh 11:00-11:50 AM, and by appointment

E-mail: hirt@siskiyous.edu

Office phone: 530·938·5255

Lab phone: 530·938·5157

 

Fall 2015 Academic Schedule


Monday
Tuesday
Wednesday
Thursday
Friday
Saturday
8:00-8:50 AM  

ENVS 1002
SCI-120

  ENVS 1002
SCI-120
   
       
9:00-9:50 AM        
       
10:00-10:50 AM office
hour
office
hour
office
hour
 
 
11:00-11:50 AM
ASTR 1110
SCI-216
office
hour
ASTR 1110
SCI-216
office
hour
ASTR 1110
SCI-216
 
 
12:00-12:50 PM GEOL 1210
SCI-216
  GEOL 1210
SCI-216
  GEOL 1210
SCI-216
 
     
1:00-1:50 PM     GEOL 1210
lab
SCI-216
     
         
2:00-2:50 PM          
         
3:00-3:50 PM     GEOL 1110
CCC Confer
   
       
4:00-4:50 PM          
         
6:30-9:30PM; 2, 4-Sep
7:00AM-5:00PM; 5-Sep
    GEOL 0800
SCI-216
  GEOL 0800
SCI-216
GEOL 0800
field
6:30-9:30PM; 16, 18-Sep
7:00AM-5:00PM; 19-Sep
    GEOL 0810
SCI-216
  GEOL 0810
SCI-216
GEOL 0810
field

Scholarship

I began my study of Earth science at Santa Monica College, and went on to earn my degrees in geology from UC Los Angeles and UC Santa Barbara. Since earning my Ph.D. I have continued to study how felsic (silica-rich) magmas form, accumulate in Earth's crust and change composition as they cool, crystallize, and interact with other magmas.

Although I have studied some very hot felsic lavas in Idaho that are related to the Yellowstone hotspot (Hirt, 2002), most of my work has been has been directed towards understanding the development of a suite of felsic magmas that accumulated deep underground in California's Sierra Nevada about 85 million years ago. The compositions and textures of rocks in the Mount Whitney Intrusive Suite suggest that Earth's crust warmed as the intrusion grew and that this warming enabled magma near the center of the body to stay molten long enough for crystals and melt to separate on a large scale and form a compositionally-stratified magma reservoir (Hirt, 2007).

Campus and Community Service

On campus during the 2015-2016 academic year I will serve as an at-large member of the Academic Senate's Executive Committee and as the chair of the Equivalency Committee. Off campus, I will continue to serve as a board member of the Shasta Valley Resource Conservation District.