High-resolution digital elevation dataset for Crater Lake National Park and vicinity, Oregon, based on LiDAR survey of August-September 2010 and bathymetric survey of July 2000

Data Series ◽  
10.3133/ds716 ◽  
2012 ◽  
Author(s):  
Joel E. Robinson
Keyword(s):  
High Resolution ◽  
National Park ◽  
Crater Lake ◽  
Bathymetric Survey ◽  
Crater Lake National Park ◽  
Digital Elevation

scholarly journals A Long-Term Watershed-Scale Partnership to Restore Bull Trout Across Federal, State, Private, and Historic Tribal Land Near Crater Lake National Park, Oregon

Fisheries ◽  
2018 ◽  
Vol 43 (4) ◽  
pp. 183-193 ◽  
Author(s):  
M. W. Buktenica ◽  
D. K. Hering ◽  
N. Scott ◽  
C. Lambert ◽  
J. McKee ◽  
...  
Keyword(s):  
National Park ◽  
Crater Lake ◽  
Federal State ◽  
Bull Trout ◽  
Watershed Scale ◽  
Crater Lake National Park ◽  
Tribal Land

Crater Lake National Park: A History

2003 ◽  
Vol 8 (4) ◽  
pp. 693
Author(s):  
Marguerite S. Shaffer ◽  
Rick Harmon
Keyword(s):  
National Park ◽  
Crater Lake ◽  
Crater Lake National Park

scholarly journals Mapping the potential distribution of frozen ground in Tucarroya (Monte Perdido Massif, the Pyrenees)

2020 ◽  
Vol 46 (2) ◽  
pp. 395-411 ◽  
Author(s):  
E. Serrano ◽  
A. Pisabarro ◽  
J.I. López-Moreno ◽  
M. Gómez-Lende ◽  
R. Martín-Moreno ◽  
...  
Keyword(s):  
High Resolution ◽  
National Park ◽  
Potential Distribution ◽  
Temperature Data ◽  
Predictor Variables ◽  
Snow Pack ◽  
Frozen Ground ◽  
Digital Elevation ◽  
Elevation Model ◽  
Ground Potential

This paper shows the creation of a map of frozen ground potential for the Tucarroya valley in Ordesa National Park. To create this map, it was necessary to combine the identified landforms associated to the presence of frozen ground by fieldwork, ground temperature data continuously recorded during two years by automatic loggers, a Basal Temperature of Snow (BTS) survey, and predictor variables derived from a high resolution Digital Elevation Model (DEM). Four environments have been differentiated: unfrozen ground, seasonal frozen ground, possible permafrost and probable permafrost. The map confirms a very limited variety and extension of permafrost, above 2700 m a.s.l. on gentle and shadowed slopes. Seasonal frozen ground is the most common thermal regime, as it can be developed above 2500 m a.s.l. Snow-pack duration and thickness tightly control the duration of frozen ground and the freezing-thawing cycles. Frost activity and unfrozen ground is restricted from 2570 to 2750 m a.s.l.

Under trees and water at Crater Lake National Park, Oregon

2012 ◽  
Author(s):  
Joel E. Robinson ◽  
Charles R. Bacon ◽  
Chris Wayne
Keyword(s):  
National Park ◽  
Crater Lake ◽  
Crater Lake National Park
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