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Campgrounds open and space available, but reservations no longer accepted.
As of 9.3.2012, winter reservations no longer accepted (via reserveamerica.com; 1-800-444-7275) for Jed Smith, Mill Creek, and Elk Prairie campgrounds. This does NOT mean that sites are unavail. All sites avail. first-come, first-served basis until May. More »
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Miners Ridge and Ossagon backcountry camps closed indefinitely.
Backpacker sites avail. during summer only at Gold Bluffs Beach Campground (8 sites avail.; free permit req'd; $5 fee paid on site) and year-round at Elk Prairie Campground (hiker/biker sites avail., first-come, first-served; $5 fee paid on site). More »
Natural Features & Ecosystems
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Geologic Setting The North Coast region, which includes RNSP and the adjacent offshore area, is the most seismically active region in the United States. As a result of frequent earthquakes, rapid uplift rates have led to landslides, actively braiding and shifting rivers, and rapid coastal erosion. The reason for all this activity is the geologic setting of the North Coast region. Three tectonic plates (thin pieces of the Earth's crust which float above the mantle) known as the North American, the Pacific, and the Gorda contact each other at the Mendocino triple junction. This junction lies offshore near Cape Mendocino, which is about 100 miles (160 km) southwest of RNSP. Each of these plates slide against each other as they slowly move in opposing directions. Movement may be as much as two or three inches (5-6 cm) a year. Many times, this movement comes in the form of earthquakes, when built-up energy is released along fault lines that border the plates. Although the majority of these earthquakes are too small to be noticed, larger quakes are not uncommon. In the 1990s, at least nine magnitude 6.0-plus earthquakes jolted the North Coast. This amount of large quakes was higher than in any other decade within the last century. Most of these quakes occurred offshore, resulting in one death and major financial losses. Because the Gorda plate is subducting beneath the North American plate, there is the possibility of a "great earthquake" occurring in the future. Scientists believe that the two plates are partially locked together along a contact known as the Cascadia subduction zone. The frozen boundary between the two plates is called the megathrust. The megathrust is broken from time to time, but usually along small parts of the fault, resulting in small quakes. However, if a larger part is broken, a magnitude 8.0-plus quake is possible. |
Gold Bluffs Beach along Davison Road
Lynne Mager
Earthquakes Studies have shown that the last great subduction zone earthquake took place 300 years ago. Intervals between such quakes are in the hundreds of years, so predicting the next one is difficult. But research suggests that eventually such a quake will occur. Disastrous effects are possible when visiting the redwood region; be prepared by following these precautions:
Rocks Most of RNSP is underlain by rocks of the Franciscan asemblage, which is primarily composed of sandstones and mudstones. This rock unit is best seen along the coast from Enderts Beach to the mouth of Redwood Creek and in road cuts on the way to the Tall Trees Grove trailhead. Much of the Franciscan assemblage consists of rock that has been sheared and lifted from the ocean floor as a result of the plate action along the Cascadia subduction zone. |
Tsunami logo NPS Tsunami Tsunamis have killed in the past. They are always a possible threat in the seismically active North Coast region, however, destructive tsunamis are rare and shouldn't ruin your visit to the beach. In the event that you do find yourself near the coast when an earthquake hits, be aware of the following guidelines:
Klamath River mouth NPS Rivers and Streams The three large river systems within the park — the Smith River, the Klamath River, and Redwood Creek — have cut deep gorges through the forest and mountainous terrain. Redwood Creek follows the Grogan Fault northwest, with many small tributaries. The Klamath River, the largest in the North Coast region, provides important habitat for wildlife along its banks and in its estuary. The Smith River is also important for wildlife and has been named a Wild and Scenic River. Stream flow depends on the amount of rainfall in the parks. The rainy season usually stretches from October through April, but the Smith and Klamath rivers also receive water from snowmelt in the mountains to the east. Warm rains combined with snowmelt have caused floods, including the large flood of December 1964 which caused the highest record peak flow on Redwood Creek. Though there are no natural ponds or lakes in the parks; there are lagoons and marshes, results of oceanic and tectonic processes. Also within the parks' boundaries are the estuaries at the mouths of the Klamath River and Redwood Creek. These estuaries provide several uses for humans and wildlife: a transition and nursery area for fish, valuable habitat for fresh and saltwater species, recreational area for park visitors and nearby communities, and a supply of water for farming and ranching. Salmon and steelhead populations were severely diminished by past logging activities within Redwood Creek's watershed. Increased sediment loads as a result of increased erosion has altered the habitat of Redwood Creek. Today, these fish are attempting to maintain their presence in the creek, but very few of these fish are able to adapt to the ecological imbalance. 
Steller's sea lions NPS Ocean Despite the extreme nature of fierce ocean winds, pounding waves, and geologic instability, visitors will find this pristine coastline an enchanting, unexpected part of the RNSP experience. Intertidal Zone: A splash zone above the high tide line receives the powerful shock of pounding waves. Inhabitants here are more attuned to life on land than on sea, but they are at the same time transitional. Tidepools: Beaches: Seastacks: 
Historic Dolason barn in Dolason Prairie along the Bald Hills Road. The Lyons family raised award-winning sheep for 100 years, starting in the 1850s. Prairies For thousands of years, American Indians routinely set fires in the prairies to keep them free of encroaching trees, to make the land more productive, and to attract elk, which were an important food source. The regularity of fire in the prairies has limited what kind of trees grew there. Oaks gained a foothold in places and big-leaf maples thrived along stream courses, but for the most part, fires killed tree seedlings before they had a chance to take hold and turn grassland into forest. In more recent times, the suppression of fire has resulted in the spread of Douglas-fir, a species well suited for growing in hot, dry places like the Bald Hills. The open grasslands have dwindled, now replaced by fir forests. Today, park staff is again using fire to maintain the oak woodlands, grasses, and other native plants found in this diminishing natural community. Fire not only helps preserve the natural values of these grassy expanses, but the cultural values as well. Values represented by the historic barns, relict stands of oak, and the openness of the land itself. Explore the biodiversity of the Klamath Network, which includes Redwood National and State Parks, Lassen Volcanic National Park, Crater Lake National Park, Oregon Caves National Monument, Whiskeytown National Recreation Area, and Lava Beds National Monument. 
The Klamath Region covers northern California and southern Oregon including the above parks.
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Did You Know?
While oceans contain most of Earth's carbon, about half stored on land in Redwood National and State Parks is in soils. The amount of carbon in the upper two meters of soil alone is ~14 million metric tons. That's equal to 1% of total U.S. emission in a year!