Last updated: January 3, 2025
Article
NPS Geodiversity Atlas—Katahdin Woods and Waters National Monument, Maine

NPS Photo by Grace Kirk.
Introduction
Katahdin Woods and Waters National Monument is situated in the forestland of Maine’s North Woods on the eastern border of Baxter State Park approximately 130 km (80 mi) north of Bangor in Penobscot County. Established on August 23, 2016, in honor of the 100th anniversary of the National Park Service, the monument encompasses approximately 35,435 hectares (87,563 acres) and protects an area that was once the heart of Maine’s logging and papermaking industry. The landscape of the monument is dominated by the fluvial valleys of the East Branch of the Penobscot River, Wassataquoik Stream, and Seboeis River, and features rolling forests, mountains, wetlands, and a diverse biological community spanning three ecoregions. The forests of Katahdin Woods and Waters display the transition between northern boreal and southern broadleaf deciduous forests, providing a unique opportunity to study the effects of climate change across different ecosystems. The landscape of KAWW shares a cultural history that dates back nearly 11,000 years, inspiring Native Americans, lumberjacks, timber owners, artists, authors, scientists, recreationists, and others. (NPS Geologic Type Section Inventory, Henderson, 2022)
Geologic History and Features
Katahdin Woods and Waters' geology provides prominent evidence of large and powerful earth-changing events that have shaped the landscape as we know it today. Geologic formations throughout the monument provide striking visual evidence that marine waters covered the area in the periods immediately following the Cambrian period (over 500 million years ago). Owen Brook limestone, an outcrop of calcareous bedrock west of the East Branch containing fossil brachiopods, is of coral reef origin. Pillow lavas, near the summit of Lunksoos Mountain, were produced by underwater eruptions. Haskell Rock, the 20-foot-tall pillar in the midst of the East Branch, is conglomerate bedrock that suggests a time of dynamic transition from volcanic islands to an ocean with underwater sedimentation. In more recent geological history, glacial landforms, glacial scoured bedrock, and the lake sediments in the area, deposited only since the retreat of the last glaciers, record a history of intense change in climate that gave rise to the modern topography of the area. (NPS Foundation Document KAWW, 2016)
Fossil Resources
One of the resources mentioned in the presidential proclamation establishing the monument is fossils, making Katahdin Woods and Waters NM one of only 18 National Park System units that have paleontological resources specifically referenced in their establishing proclamation or enabling legislation.
Many kinds of fossils have been reported from Katahdin Woods and Waters NM. They are either body fossils or trace fossils of marine invertebrates. Most of the diversity comes from corals and brachiopods. In terms of abundance, crinoid columnals (pieces of the “stems” of sea lilies) are frequently found, but columnals are hard to attribute to species so we know very little about the actual kinds of crinoids that they came from. Other kinds of fossils found in the monument include sponges, bivalves, snails, trilobites, graptolites (a kind of colonial invertebrate, with tiny worm-like animals living in tubes or cups in larger structures), and invertebrate burrows. (Paleontology of KAWW, Tweet, 2022)

NPS photo by Vincent Santucci.
Regional Geology
Katahdin Woods and Waters National Monument is a part of the New England Physiographic Province and shares its geologic history and some characteristic geologic formations with a region that extends well beyond park boundaries.
-
Tweet JS, Santucci VL, Ashton I. 2022. Katahdin Woods and Waters National Monument: Paleontological resource inventory (public version). Natural Resource Report. NPS/KAWW/NRR—2022/2472. National Park Service. Fort Collins, Colorado. https://doi.org/10.36967/2294810
-
Henderson TC, Santucci VL, Connors T, Tweet JS. 2022. National Park Service geologic type section inventory: Northeast Temperate Inventory & Monitoring Network. Natural Resource Report. NPS/NETN/NRR—2022/2475. National Park Service. Fort Collins, Colorado. https://doi.org/10.36967/2294876
Related Articles
Katahdin Woods and Waters National Monument
- Type: Series
- Locations: Arches National Park, Bandelier National Monument, Big Bend National Park, Bighorn Canyon National Recreation Area, Canyon de Chelly National Monument, more »
All across the park system, scientists, rangers, and interpreters are engaged in the important work of studying, protecting, and sharing our rich fossil heritage. Park Paleontology news provides a close up look at the important work of caring for these irreplaceable resources.
- Contribute to Park Paleontology News by contacting the newsletter editor
- Learn more about Fossils & Paleontology
- Celebrate National Fossil Day with events across the nation
- Locations: Katahdin Woods and Waters National Monument
- Offices: Geologic Resources Division
Katahdin Woods and Waters National Monument preserves rocks and fossils from much of the first half of the Paleozoic Era, approximately 540 to 400 million years ago, when what is now the east coast of North America was growing with additions of small continental fragments. Fossils have been occasionally reported from the monument by scientists in the past, but this is the first time that a thorough inventory has been made of the monument’s fossils.
- Type: Series
- Locations: Agate Fossil Beds National Monument, Alibates Flint Quarries National Monument, Aniakchak National Monument & Preserve, Appalachian National Scenic Trail, Arches National Park, more »
- Locations: Alibates Flint Quarries National Monument, Big South Fork National River & Recreation Area, Bighorn Canyon National Recreation Area, Blue Ridge Parkway, Buffalo National River, more »
- Offices: Geologic Resources Division
During the Paleozoic Era (541 to 252 million years ago), fish diversified and marine organisms were very abundant. In North America, the Paleozoic is characterized by multiple advances and retreats of shallow seas and repeated continental collisions that formed the Appalachian Mountains. Common Paleozoic fossils include trilobites and cephalopods such as squid, as well as insects and ferns. The greatest mass extinction in Earth's history ended this era.
- Locations: Buffalo National River, Chesapeake & Ohio Canal National Historical Park, Chickasaw National Recreation Area, George Washington Memorial Parkway, Great Basin National Park, more »
- Offices: Geologic Resources Division
- Locations: Chesapeake & Ohio Canal National Historical Park, Chickasaw National Recreation Area, Cumberland Gap National Historical Park, Death Valley National Park, Delaware Water Gap National Recreation Area, Katahdin Woods and Waters National Monument
- Offices: Geologic Resources Division
- Type: Series
- Locations: Alibates Flint Quarries National Monument, Big South Fork National River & Recreation Area, Bighorn Canyon National Recreation Area, Buffalo National River, Canyonlands National Park, more »
During the Paleozoic Era (541 to 252 million years ago), fish diversified and marine organisms were very abundant. In North America, the Paleozoic is characterized by multiple advances and retreats of shallow seas and repeated continental collisions that formed the Appalachian Mountains. Common Paleozoic fossils include trilobites and cephalopods such as squid, as well as insects and ferns. The greatest mass extinction in Earth's history ended this era.