
NPS photo by Barabara Cellarius.
Geology and Stratigraphy of the Central Alaska I&M Network
The Central Alaska Inventory & Monitoring Network (CAKN) consists of three NPS units in south-central, east-central, and southeastern Alaska: Denali National Park and Preserve (DENA), Wrangell-St. Elias National Park and Preserve (WRST), and Yukon-Charley Rivers National Preserve (YUCH). It is important to note that Wrangell-St. Elias belongs to both the CAKN and the Southeast Alaska Inventory & Monitoring Network (SEAN). The SEAN monitors about 193 km (120 mi) of WRST coastline and the outer coast of Glacier Bay. It is difficult for the CAKN to address park vital signs south of the Bagley ice field and there is an ecological contrast to the rest of the network making it a better fit with SEAN.
The geologic history of the parks of the CAKN is complex and subject to evolving scientific interpretations (Santucci et al. 2011). Southern Alaska lies along a tectonically active continental margin that records convergence between the North American continental plate and the Pacific oceanic plate. The tall mountain ranges, volcanoes and other features are evidence of the geologic history along the continental margin and plate boundary. The geology of this geographic area, particularly DENA and WRST, is dominated by a series of terranes accreted during the latter half of the Mesozoic Era (Christeson et al. 2010; see Geologic Time Scale). Accreted terranes are large assemblages of rocks that originally formed elsewhere, were subsequently transported by plate tectonic processes, and ultimately collided with and accreted onto a different plate, in this case North America. Rocks deposited after the terrane accretion, referred to as “post-accretionary rocks”, are also exposed in the parks.
YUCH is geographically located further from the continental margin than DENA and WRST, and so consequently the park is less heavily influenced by terrane accretion. Rocks within the northeastern portion of YUCH are further from the western continental margin and were not impacted by the tectonic events along the plate boundary. The Tintina Fault divides YUCH into two distinct geologic areas: one northeast and one southwest of the fault. The area southwest of the Tintina Fault consists of a complex sequence of igneous rocks and metamorphosed sedimentary rocks. These rocks were probably metamorphosed and juxtaposed against the western margin of North America when several small microplates (or terranes) collided during the Mesozoic. Northeast of the Tintina Fault, the northeast corner of YUCH consists of a sequence of un-metamorphosed Precambrian and Paleozoic passive margin (non-volcanic continental margin characterized by carbonate, shale [mudstone], and sandstone rocks) rocks that represents the westernmost extension of the Paleozoic North American continent. The northeastern portion of YUCH is one of the rare locations in North America where such an extensive geologic history is preserved, spanning from the Precambrian to the Cenozoic. The northwest corner of YUCH, lying north of the Tintina Fault and separated to the east from the northeast corner by a northeast-trending belt of Cretaceous flysch (forming the Kandik Basin), represents a poorly understood collage of accreted terranes. The Yukon River and its tributaries cut through these ancient sedimentary rocks, exposing a remarkable record of the floral and faunal history of east-central Alaska (Santucci et al. 2011).
A Brief Geologic History
A few examples of events and Network resources in each geologic time period are highlighted below, from youngest to oldest.
The Cenozoic rocks of the CAKN parks represent non-accretionary units.
At DENA, the uppermost Cantwell Formation may extend into the Paleocene. Rocks of the Usibelli Group are mapped in DENA and are Eocene through Miocene in age. Finally, the Nenana Gravel is a Miocene and Pliocene unit.
The Cenozoic geology of WRST consists of a sequence of sedimentary, metamorphic, and igneous rocks, some of which are part of the Yakutat Terrane. The Yakutat Terrane is the last of the seven terranes in WRST. There are periods of volcanism at WRST which date to the latest Oligocene or earliest Miocene. These volcanic sequences are mapped in the Wrangell Volcanic Field.
Unnamed rocks of Cretaceous to Cenozoic are present in YUCH.
The Mesozoic geology of CAKN parks includes both accretionary and post-accretionary rocks.
Within DENA the Mesozoic portions of accretionary terranes include:
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Yukon–Tanana Terrane (Triassic)
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Farewell Terrane (Triassic–Jurassic)
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Chulitna Terrane (Triassic–Jurassic)
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Windy Terrane (Triassic–Cretaceous)
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McKinley Terrane (Triassic–Cretaceous)
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Pingston Terrane (Triassic)
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West Fork Terrane (Jurassic)
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Kahiltna Assemblage (Late Jurassic–Late Cretaceous)
The Mesozoic rocks of WRST are associated with the Wrangellia Terrane and are divided into two
sections:
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Wrangellia Terrane, eastern Alaskan Range and northern Wrangell Mountains
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Wrangellia Terrane, southern Wrangell Mountains and St. Elias Mountains
Within YUCH the following Mesozoic units are mapped:
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Glenn Shale (Triassic–Early Cretaceous)
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Kandik Group (Early Cretaceous)
The Paleozoic is well-represented within DENA in a number of terranes. Many of the terranes appear to be exotic to North America and accreted onto the continent. However, there may be Paleozoic rocks in DENA that originated in North America.
Below is a list of terranes mapped in DENA:
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Dillinger Terrane (Early Ordovician–Devonian)
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McKinley Terrane (Silurian–Triassic)
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Yukon–Tanana Terrane (Devonian–Mississippian)
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Windy Terrane (Early Devonian–Late Triassic) (potentially some older units)
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Mystic Terrane (Early Devonian–Early Jurassic)
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Chulitna Terrane (Late Devonian–Early Jurassic)
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Pingston Terrane (Pennsylvanian–Triassic)
Within WRST the Paleozoic is represented by Devonian through Permian geologic units associated with terranes. The oldest Paleozoic unit is the Kaskawulsh Group in the Alexander Terrane. Below are the various terranes within WRST that have Paleozoic components:
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Alexander Terrane (Devonian–Pennsylvanian)
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Wrangellia Terrane, eastern Alaska Range and northern Wrangell Mountains (Pennsylvanian– Permian)
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Wrangellia Terrane, southern Wrangell Mountains and Saint Elias Mountains (Mississippian– Permian)
The Paleozoic rocks within YUCH span from the Cambrian through the Permian (Santucci et al. 2011). During the early and middle Paleozoic, the YUCH area was part of an ancestral platform referred to as the Yukon Shelf. The platform was situated between the Brooks Geosyncline (basin along the continental margin) to the north and the Cordilleran Geosyncline to the south. The interior of the shelf subsided during the Ordovician and Early Devonian, forming a trough (Brosgé and Dutro 1973). Paleozoic sediments were extensively eroded during the Pennsylvanian.
The Precambrian is represented in DENA and YUCH. In DENA the Wickersham Grit is a Proterozoic unit. In YUCH the Proterozoic Tindir Group includes the most ancient rocks exposed in the park (Kaufman et al. 1992).
Geology & Soils—Central Alaska Network Parks
Type Sections—Central Alaska Network

The geologic history above is excerpted from a report titled, "National Park Service geologic type section inventory: Central Alaska Inventory & Monitoring Network". Type sections are essential reference locations for the geoscientists who study geologic history and paleontology. A summary of the type sections in each park can be found at the links below.
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Denali National Park & Preserve, Alaska (contains three identified stratotypes)
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Wrangell-St. Elias National Park, Alaska (contains 25 identified stratotypes)
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Yukon-Charley Rivers National Preserve, Alaska (contains 17 identified stratotypes)
The full Network report is available in digital format from:
Please cite this publication as:
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Henderson TC, Santucci VL, Connors T, Tweet JS. 2022. National Park Service geologic type section inventory: Central Alaska Inventory & Monitoring Network. Natural Resource Report. NPS/CAKN/NRR—2022/2369. National Park Service. Fort Collins, Colorado.
NPS Stratotype Inventory
Fossil Resources—Central Alaska Network

Between 2002 and 2011, network-based paleontological resource inventories were completed for all the 32 I&M networks, and six of the earliest were completely updated between 2012 and 2016. The report linked below summarizes the paleontological resources of all park units in the Central Alaska Inventory & Monitoring Network (CAKN). The report provides geologic background and paleontological resource data for each park to support management operations, planning, and science-based decision making as required by NPS management policies and the Paleontological Resources Preservation Act (2009).
The full report is available in digital format from
Please cite this publication as:
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Santucci, V. L., R. B. Blodgett, W. P. Elder, J. S. Tweet, and J. P. Kenworthy. 2011. Paleontological resource inventory and monitoring: Central Alaska Network. Natural Resource Technical Report NPS/NRSS/NRTR—2011/510. National Park Service, Fort Collins, Colorado.
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Last updated: February 21, 2025