384 WILLIAM HERBERT HOBBS 
above the freezing-point even in the summer season, save only 
during short intervals at the termination of the fierce Antarctic 
blizzards. Furthermore, these marginal glaciers to the inland ice 
are nourished, not by inwardly and upwardly directed air currents, 
; 
is 
“9 
~ 
I Hie 
PIEDMONT EXPANDED-FOOT DENDRITIC 
TNE Sey Rte Wee 
Malaspina Glacier, Taku Glacier Early Stage 
Alaska Baltoro Gl, Himalaya Mts 
DENDRITIC RADIATING HORSE =shOB 
TYPE TYPE TYPE 
Late Stage Alpine Glaciers of 
Tasman GI.,N.Z. Glaciers Glacier Nat Fark 
GLACIER TYPES OF RECEDING FAEMICYCLE 
Progressive Withdrawal of Glacier Foot , 
Fic. 14 
as are the mountain glaciers of moderate latitudes, but by down- 
wardly and outwardly flowing currents which bring drift snow from 
the inland ice and often carry it beyond the marginal glaciers to 
be dissipated upon the surface of the sea. Separate areas of 
