Tubal Cain mine

Mount Worthington is a 6,938-foot (2,115-metre) elevation double-summit mountain located in the eastern Olympic Mountains in Jefferson County of Washington state. It is set within Buckhorn Wilderness, on land managed by the Olympic National Forest. The nearest neighbor is Iron Mountain, 0.76 mi (1.22 km) to the southwest, and the nearest higher peak is Buckhorn Mountain, 1.3 mi (2.1 km) to the southwest. Precipitation runoff from Mount Worthington drains south into the Big Quilcene River, or north into Copper Creek which is a tributary of the Dungeness River. This mountain was first known as Copper Peak, but was renamed by Jack Christensen for the William J. Worthington family, pioneers of nearby Quilcene. Copper was mined in the Tubal Cain mine at the northern base of this mountain in the early 1900s. In the same vicinity of the abandoned mine are the remains of a modified B-17 plane that crashed on January 19, 1952, when returning from a search-and-rescue mission.

Welch Peaks is a 6,110-foot (1,862-metre) mountain in the eastern Olympic Mountains in Jefferson County of Washington state, United States. It is set within Buckhorn Wilderness, on land managed by the Olympic National Forest. The nearest higher neighbor is Mount Townsend, 1.2 mi (1.9 km) to the north, and Mount Worthington rises 2.1 mi (3.4 km) to the southwest. Precipitation runoff from Welch Peaks drains into tributaries of the Big Quilcene River, and Silver Creek which is a tributary of the Dungeness River. Topographic relief is significant as the summit rises 3,100 feet (945 m) above Townsend Creek in approximately one mile. The mountain's toponym was officially adopted in 1963 by the U.S. Board on Geographic Names.

Mount Townsend is a mountain in the U.S state of Washington located within the Buckhorn Wilderness near Quilcene.

The Buckhorn Wilderness is a 44,319-acre (17,935 ha) mountainous wilderness area on the northeastern Olympic Peninsula in Washington, USA. Named after Buckhorn Mountain (6,988 ft or 2,130 m), the wilderness abuts the eastern boundary of Olympic National Park which includes nearby Mount Constance (7,756 ft or 2,364 m), Inner Constance (7,667 ft or 2,337 m), Warrior Peak (7,320 ft or 2,230 m), and Mount Deception (7,788 ft or 2,374 m).

Tyler Peak is a 6,364 feet (1,940 m) mountain summit located in Clallam County of Washington state, United States. It is situated in the northeastern Olympic Mountains, near the northern end of Gray Wolf Ridge, and is set within Buckhorn Wilderness, on land managed by the Olympic National Forest. The next highest neighbor is Mt. Baldy, two miles to the west. Precipitation runoff from Tyler Peak drains into tributaries of the Dungeness River, and topographic relief is significant as the east aspect rises 4,350 feet (1,330 m) above the river in approximately 1.5 miles (2.4 km). Old-growth forests of Douglas fir, western hemlock, and western redcedar grow on the lower slopes surrounding the peak. Like the nearby town of Sequim 12 miles (19 km) to the north, Tyler Peak lies in the rain shadow of the Olympic Mountains. This landform's toponym has been officially adopted by the U.S. Board on Geographic Names.

Warrior Peak is a 7,320+ ft (2,230+ m) double summit mountain located in Olympic National Park and Jefferson County of Washington state. Warrior is the 11th-highest peak in the Olympic Mountains. The southeast summit is the slightly higher of the two summits, the northwest peak is estimated at 7,285 feet elevation. Precipitation runoff from the west side of the mountain drains into Home Creek, a tributary of the Dungeness River, whereas the east side drains into Tunnel Creek which is a tributary of the Big Quilcene River. Warrior Peak is easy to identify from Seattle, since it appears as the first prominent peak immediately north of Mount Constance, which is the dominant peak on the skyline. Warrior's nearest higher peak is Mount Constance, 0.8 mi (1.3 km) to the south-southeast. The first ascent of the mountain was made in 1945 by Fred Beckey, who solo climbed both summits, and named the mountain.

Mount Constance is a peak in the Olympic Mountains of Washington and the third highest in the range. It is the most visually prominent peak on Seattle's western skyline. Despite being almost as tall as the ice-clad Mount Olympus to the west, Mount Constance has little in the way of glaciers and permanent snow because the eastern, and particularly this northeastern, portion of the Olympics receives far less precipitation. However the narrow and steep Crystal Glacier still exists on the mountain's north face, shaded by the bulk of the main peak and with a small lake at its terminus. In addition, the treeline is higher here than mountains to the west, also hinting at the drier alpine conditions. By virtue of its position at the eastern edge of the Olympics, Mount Constance also enjoys spectacular vertical relief. For example, it rises over 6,900 feet (2,100 m) above the Dosewallips River to the south in only 3 horizontal miles (4.8 km). It is also only 12 miles (20 km) from the tidewater of Hood Canal. The summit of Mount Constance lies on the boundary between Olympic National Park and Buckhorn Wilderness. The Constance massif includes Mount Constance, Inner Constance, the twin peaks of Warrior to the north, as well as numerous subsidiary summits on rocky southern ridges enclosing the cirque basin that contains Lake Constance.

Inner Constance is a summit of the Olympic Mountains and is located in Jefferson County of Washington state. It is located near the eastern edge of Olympic National Park on the Olympic Peninsula. At 7,670 feet (2,338 m), Inner Constance is the fifth-highest peak of the Olympic Mountains, after Mount Olympus, Mount Deception, Mount Constance, and Mount Johnson. Its nearest higher neighbor is Mount Constance, 0.9 mi (1.4 km) to the east. Within this nearly mile-wide separation resides a deep glacially carved canyon called "Avalanche Canyon". Precipitation runoff on the north side of the peak drains into tributaries of the Dungeness River, whereas the south side drains into tributaries of the Dosewallips River.

Mount Zion is a 4,278-foot (1,304 m) peak in the Olympic National Forest. The peak is located 9.5 miles (15.3 km) northwest of Quilcene, and near Lords Lake and Bon Jon Pass. Billed as one of the easier hikes in the Olympics, Zion offers a 1,340-foot (410 m) elevation gain in just under 2 miles (3.2 km).

Gray Wolf Ridge is a spur of the northeastern Olympic Mountains in Washington's Olympic Peninsula. Arcing northeast from the Mount Deception - Needles - Mount Clark - Mount Walkinshaw massif, Gray Wolf Ridge is covered by alpine and subalpine forests up to the timberline, leaving the upper elevations of the ridge's six rocky peaks vegetated only by fragile alpine meadows. The ridge and its component mountains are markedly steep, as is its primary access route, the Maynard Burn Trail (#816) of Olympic National Forest. The higher, western segment of Gray Wolf Ridge lies within the boundary of Olympic National Park. Gray Wolf Mountain, at 7,218 feet (2,200 m) above sea level, is the ridge's highest summit. It was first climbed by Leigh B. Lint in 1928. Other distinct peaks include '7076' (7076), Baldy (6797), Tyler Peak (6364), and Maynard Peak (5065), which forms the northeastern terminus of Gray Wolf Ridge. Gray Wolf River runs through the valley-bottom to the Ridge's north; Royal Creek and the Dungeness River flow through the valley along the Ridge's east and south. Gray Wolf Ridge is the highest point of Clallam County.

The Gray Wolf River is a river of the Olympic Peninsula in Washington. It is a tributary of the Dungeness River. It heads near Gray Wolf Pass and drains the west slope of The Needles.

Mount Jupiter is a 5,711-foot (1,741-meter) mountain summit in the Olympic Mountains and is located in Jefferson County of Washington state. It is situated in The Brothers Wilderness on land managed by Olympic National Forest. Mount Jupiter is easy to identify from Seattle, since it appears as the prominent peak between The Brothers and Mount Constance. Precipitation runoff from the north side of the mountain drains into the Dosewallips River, whereas the south side drains into the Duckabush River. Topographic relief is significant as the summit rises 5,100 feet (1,554 meters) above the Duckabush Valley in 1.5 miles (2.4 km). The Jupiter name was applied by the Seattle Press Expedition in an effort to link the peak with the Greco-Roman mythological names associated with Mount Olympus. Jupiter was a Roman god on Olympus. The mountain's toponym has been officially adopted by the United States Board on Geographic Names.