LATE QUATERNARY GEOMORPHIC HISTORY OF LOWER HIGHLAND CREEK, WIND CAVE NATIONAL PARK, SOUTH DAKOTA

1996 ◽  
Vol 17 (5) ◽  
pp. 446-464 ◽  
Author(s):  
Glen G. Fredlund
Author(s):  
David Harwood ◽  
Kyle Thompson

Eight in-service teachers and two instructors engaged in an inquiry-based geology field course from June 14 to 29, 2014 through Wyoming, South Dakota, and Nebraska. This team of learners spent three days in mid-June working in the Grand Teton National Park area. The UW-NPS facilities provide an excellent opportunity for participants to discover the natural history of the Teton Range, as well as close-out a few projects while sitting in a real chair, at a real table, a welcome change from our usual campground setting.


Author(s):  
Cathy Barnosky

The late-Quaternary vegetation history of the northern Rocky Mountains has thus far been inferred largely from isolated records. These data suggest that conifer forests were established early in postglacial time and were little modified thereafter. The similarity of early postglacial vegetation to modern communities over broad areas gives rise to two hypotheses: (1) that glacial refugia were close to the ice margin, and (2) that vegetation soon colonized the deglaciated areas and has been only subtly affected by climatic perturbations since that time. It is the goal of this project to test these two hypotheses in the region of Grand Teton National Park.


Author(s):  
Cathy Barnosky

The objectives of this project, now in its second year, have not changed significantly from that of the proposal. Prior to this study, the late-Quaternary vegetation history of the northern Rocky Mountains had been inferred largely from isolated pollen records. These data suggested that conifer forests were established early in postglacial time and were little modified thereafter. The similarity of past vegetation to modern communities over a broad area gives rise to two hypothesis: (1) glacial refugia were c1ose to the ice margin, and (2) vegetation soon colonized the deglaciated areas and has been only subtly affected by climatic perturbations since that time. It is the goal of this project to test these hypotheses in the region of Grand Teton National Park.


2000 ◽  
Vol 30 (3) ◽  
pp. 474-476 ◽  
Author(s):  
LUIZ JOSÉ TOMAZELLI ◽  
SÉRGIO REBELLO DILLENBURG ◽  
JORGE ALBERTO VILLWOCK

Author(s):  
Terence Young ◽  
Alan MacEachern ◽  
Lary Dilsaver

This essay explores the evolving international relationship of the two national park agencies that in 1968 began to offer joint training classes for protected-area managers from around the world. Within the British settler societies that dominated nineteenth century park-making, the United States’ National Park Service (NPS) and Canada’s National Parks Branch were the most closely linked and most frequently cooperative. Contrary to campfire myths and nationalist narratives, however, the relationship was not a one-way flow of information and motivation from the US to Canada. Indeed, the latter boasted a park bureaucracy before the NPS was established. The relationship of the two nations’ park leaders in the half century leading up to 1968 demonstrates the complexity of defining the influences on park management and its diffusion from one country to another.


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