Yellowstone National Park preserves this high-altitude landscape of hydrothermal activity and alpine summits. The northern interior of the park is defined by significant elevations, including the peak of Mt Holmes and the nearby Trilobite Point. These features are connected by a network of backcountry routes, most notably the Mount Holmes-Winter Creek Trail and the Grizzly Lake Trail, which facilitate movement through the drainage basins of Indian Cr and Winter Cr. The presence of Riverside Geyser highlights the thermal features typical of this volcanic region, while Grizzly Lake serves as a prominent water body within the drainages of Straight Cr and Obsidian Cr. This survey illustrates the protected wilderness character of the Gallatin Range, showing how the terrain transitions from the high ridges of Antler Peak and Dome Mtn down into the creek valleys that feed the larger river systems of the park.
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This is the sole edition of this map. No revisions or reprints were ever made.
1885 · Gallatin
USGS Topo · 1:125,000
1885 · Gallatin
USGS Topo · 1:125,000
1901 · Gallatin
USGS Topo · 1:125,000
1908 · Gallatin
USGS Topo · 1:125,000
1911 · Gallatin
USGS Topo · 1:125,000
1955 · Ashton
USGS Topo · 1:250,000
1958 · Ashton
USGS Topo · 1:250,000
1958 · Madison Junction
USGS Topo · 1:62,500
1958 · Mount Holmes
USGS Topo · 1:62,500
1958 · Norris Junction
USGS Topo · 1:62,500