FOR    THE    YEARS    1901-1905,   INCLUSIVE.  119 
Fairbanks  (Harold  W.) — Continued. 
4.  Lake  Chelan,  Washington. 
Abstract:  Science,  new  ser.,  vol.  15,  pp.  412-413,  1902. 
Describes  physiographic  changes  which  have  taken  place  in  this  region. 
5.  The  physiography  of  southern  Arizona  and  New  Mexico. 
Abstract:  Eng.  <t  Mg.  Jour.,  vol.  75,  p.  154,  1903;  Jour.  Geol.,  vol.  11,  pp.  97-99,  1903. 
6.  Gypsum  deposits  in  California. 
U.  S.  Geol.  Surv.,  Bull.  no.  223,  pp.  119-123,  1  pi.,  1904. 
'  Describes  character,  occurrence,  and  geologic  relations  of  the  gypsum  deposits  of  California. 
7.  San  Luis  folio,  California. 
U.  S.  Geol.  Surv.,  Geol.  Atlas  of  U.  S.,  folio  no.  101,  1904. 
Describes  topography  and  drainage,  climate  and  vegetation,  the  character,  occurrence,  and 
relations  of  Juratrias  (?),  Cretaceous,  and  Tertiary  sedimentary  rocks  and  included  igneous 
rocks,  the  geologic  structure  and  history  of  the  area,  the  development  of  the  physiographic 
features,  and  the  economic  resources  and  soils. 
Fairchild  (Herman  Le  Roy). 
1.  Beach  structure  in  Medina  sandstone. 
Am.  Geol.,  vol.  28,  pp.  9-14,  3  pis.,  1901. 
Discusses  the  evidences  indicating  the  origin  of  the  ripple  marks  i  the  Medina  sandstone  of 
New  York. 
2.  Pleistocene  geology  of  western  New  York,  report  of  progress  for  1900. 
N.  Y.  State  Mus.,  54th  Ann.  Rept.,  vol.  1,  pp.  rl03-rl39,  33  pis.,  1902. 
Discusses  the  occurrence  and  deformation  of  the  Iroquois  shoreline  and  gives  results  of  recent 
studies  in  the  Syracuse-Oneida  and  Cattaraugus-Chautauqua  districts. 
3.  Elements  of  geology:  a  text-book  for  colleges  and  the  general  reader  by  Joseph 
Le  Conte.     Revised  and  partly  rewritten  by  Herman  Le  Roy  Fairchild. 
See  Le  Conte  (Joseph),  4. 
4.  Latest  and  lowest  pre-lroquois  channels  between  Syracuse  and  Rome. 
N.  Y.  State  Mus.,  55th  Ann.  Rept,,  pp.  r31-rl7,  25  pis.,  1903. 
Describes  the  occurrence  and  formation  of  river  channels  formed  during  the  Glacial  period 
in  central  New  York. 
5.  Direction  of  pre- Glacial  stream  flow  in  central  New  York. 
Am.  Geol.,  vol.  33,  pp.  43-45,  1904. 
6.  Geology  under  the  new  hypothesis  of  earth  origin. 
Am.  Geol.,  vol.  33,  pp.  94-116,  1904. 
Compares  the  sufficiency  of  the  nebular  and  planetesimal  hypotheses  and  discusses  the  expla- 
nation given  by  the  latter  of  the  origin  of  the  atmosphere  and  ocean,  volcanic  phenomena, 
deposits  of  hydrocarbons,  ores,  salt,  and  gypsum,  climate  in  geologic  time,  glaciation, 
erustal  movements,  and  life  on  the  earth. 
7.  Geology  under  the  planetesimal  hypothesis  of  earth  origin. 
Geol.  Soc.  Am.,  Bull.,  vol.  15,  pp.  243-266,  1904. 
See  preceding  entry.  Includes  discussion  by  Edward  H.  Kraus,  Willis  T.  Lee,  Israel  C.  Rus- 
sell, and  Frederick  W.  Sardeson. 
8.  Glacial  waters  from  Oneida  to  Little  Falls  [New  York]. 
N.  Y.  State  Mus.,  56th  Ann.  Rept.,  vol.  1,  and  N.  Y.  State  Geol.,  22d  Rept.,  pp.  rl7-r41,  26  pis. 
1904. 
Describes  the  position  and  extent  of  waters  along  the  ice  front,  and  the  drainage  at  different 
stages  of  the  Glacial  epoch  in  north  central  New  York,  as  determined  from  the  occurrence, 
character,  etc.,  of  Glacial  deposits. 
9.  Glacial  drainage  in  central  western  New  York. 
Abstract:  Geol.  Soc.  Am.,  Bull.,  vol.  14,  p.  553,  1904. 
10.  Evidences  of  slight  glacial  erosion  in  western  New  York. 
Abstract:  Sci.  Am.  Suppl.,  vol.  57,  p.  23447,  1904. 
11.  Ice  erosion  theory  a  fallacy. 
Geol.  Soc.  Am.,  Bull.,  vol.  16,  pp.  13-74,  12  pis.,  6  figs.,  1905. 
Discusses  the  character  of  glacial  erosion  and  presents  evidence  to  show  that  deep  valleys  and 
the  finger  lakes  of  New  York  could  not  have  been  produced  by  erosion. 
