Serpentine River is a waterway on the Seward Peninsula in the U.S. state of Alaska. It debouches at Shishmaref Inlet from the southeast. It was explored and named in 1900 by the prospector Charles McLennan. [1]
A waterway is any navigable body of water. Broad distinctions are useful to avoid ambiguity, and disambiguation will be of varying importance depending on the nuance of the equivalent word in other languages. A first distinction is necessary between maritime shipping routes and waterways used by inland water craft. Maritime shipping routes cross oceans and seas, and some lakes, where navigability is assumed, and no engineering is required, except to provide the draft for deep-sea shipping to approach seaports (channels), or to provide a short cut across an isthmus; this is the function of ship canals. Dredged channels in the sea are not usually described as waterways. There is an exception to this initial distinction, essentially for legal purposes, see under international waters.
The Seward Peninsula is a large peninsula on the western coast of the U.S. state of Alaska. It projects about 320 kilometers (200 mi) into the Bering Sea between Norton Sound, the Bering Strait, the Chukchi Sea, and Kotzebue Sound, just below the Arctic Circle. The entire peninsula is about 330 kilometers (210 mi) long and 145 km (90 mi)-225 km (140 mi) wide. Like Seward, Alaska, it was named after William H. Seward, the United States Secretary of State who fought for the U.S. purchase of Alaska.
In the United States, a state is a constituent political entity, of which there are currently 50. Bound together in a political union, each state holds governmental jurisdiction over a separate and defined geographic territory and shares its sovereignty with the federal government. Due to this shared sovereignty, Americans are citizens both of the federal republic and of the state in which they reside. State citizenship and residency are flexible, and no government approval is required to move between states, except for persons restricted by certain types of court orders. Four states use the term commonwealth rather than state in their full official names.
Heading near Midnight Mountain, about 35 miles (56 km) from Shishmaref Inlet, it flows into that inlet by a very sinuous course, from which character it receives its name. The bed rock of the Serpentine River Basin above the coastal gravel belt consists of dark graphitic and feldspathic mica-schists, which form Midnight Mountain, and of crystalline limestones and mica-schists of the Kugruk group. The relations of the dark schists to the limestones were not determined, though they are regarded as belonging to the Kugruk series. In the vicinity of the hot springs these dark schists have been intruded by extensive granite masses, forming a large area of granite. This granite outcrops in needles and pinnacles, produced by weathering along a double set of joints. [2]
The Schlitz and Reindeer creeks flow northwestward into Serpentine River. Bryan Creek rises to the east of Kougarok Mountain and flows northeastward into Serpentine River. Quartz Creek is the name applied to the headwaters of the South Fork of Serpentine River. [3]
The river was first explored and named by Charles McLennan, who, with dog team and Eskimo assistants, made a trip into the region from Shishmaref Inlet in May, 1900. McLennan was probably the first European to reach the hot springs on Spring Creek, a tributary of this river. He staked a number of claims along this creek, and prepared a map of the region, a copy of which was received in Washington in March, 1901. In September, 1901, there was a small settlement at the hot springs. Gold was found on a number of the tributaries of the middle fork of this river, and in September 1901, a number of miners were preparing to winter in the neighborhood, the principal settlement being at the hot springs. [2]
The Bering Land Bridge National Preserve is one of the most remote United States national park areas, located on the Seward Peninsula. The National Preserve protects a remnant of the Bering Land Bridge that connected Asia with North America more than 13,000 years ago during the Pleistocene ice age. The majority of this land bridge now lies beneath the waters of the Chukchi and Bering Seas. During the glacial epoch this bridge was a migration route for people, animals, and plants whenever ocean levels fell enough to expose the land bridge. Archeologists disagree whether it was across this Bering Land Bridge, also called Beringia, that humans first migrated from Asia to populate the Americas, or whether it was via a coastal route.
The Koyuk River is a river on the Seward Peninsula of western Alaska, in the United States. The river originates in the interior of the peninsula, at the Lost Jim Lava Flow of the Bering Land Bridge National Preserve, where it flows southeast towards the mouth of Norton Bay on Norton Sound. The native village of Koyuk is located at its mouth. The two major tributaries are the Peace and Salmon rivers; other tributaries include Dime and Sweepstakes.
The Kugruk River is a stream, 60 miles (97 km) long, in the northwestern part of the U.S. state of Alaska. It is the largest tributary of the Kuzitrin River. It begins near Imuruk Lake on the Seward Peninsula and flows generally north to Kugruk Lagoon, at Kotzebue Sound on the Chukchi Sea. The river enters the lagoon 5.5 miles (8.9 km) southeast of Cape Deceit in the Northwest Arctic Borough.
The Fish River is a waterway in the U.S. state of Alaska. The 47-mile-long (76 km) river rises in the Bendeleben Mountains and flows south to Golovnin Lagoon, before emptying into Golovnin Bay, Norton Sound, and the Bering Sea. The basin formed by the Fish River is known for its placer gold deposits, and in particular, the Niukluk River and its tributaries; production from this tributary valley is reported to be more than from any other place in the region. A galena mine existed 40 miles (64 km) from the sea, worked on occasion by a San Francisco corporation with a few hundred tons of ore taken to the city for smelting and refining for silver. Walter Curran Mendenhall found obscure fossils on Fish River at White Mountain.
The Tubutulik River is a waterway in the U.S. state of Alaska. The 25-mile (40 km) long river is situated on the Seward Peninsula. It flows southeastwards to the Kwiniuk Inlet at the northwestern end of Norton Bay, 25 miles (40 km) southwest of Koyuk in the Bering Sea. Its Inuit name was reported as "Tubuktulik" in 1849 by Capt. Mikhail Dmitrievich Tebenkov of the Imperial Russian Navy. Exploration for placer gold occurred in the Council district area where the river valley is located, and in 1898, mining commenced. The production was substantial and ranked second only to that of Nome.
The Bendeleben (/ˈbɛn.dəˌleɪ.bɨn/) Mountains are a mountain range on the heart of the Seward Peninsula in Nome Census Area, Alaska, United States. This range forms a major divide between drainage basins draining into the Pacific Ocean and the Arctic Ocean. The tallest peak, Mount Bendeleben is 3,730 feet (1,140 m) at the summit, and is located on the west end. Bits of the range go into the Bering Land Bridge National Preserve, but most of the peaks remain unclaimed. The Tubutulik River flows in the area.
Cape Nome is a headland on the Seward Peninsula in the U.S. state of Alaska. It is situated on the northern shore of Norton Sound, 15 miles (24 km) to the east of Nome also on Norton Sound. It is delimited by the Norton Sound to the south, Hastings Creek on the west, a lagoon on the east and an estuary formed by the Flambeau River and the Eldorado River. From the sea shore, Cape Nome extends inland by about 4 miles (6.4 km), connected by road with Nome.
Candle Creek is a western tributary of the Kiwalik River, located on the Seward Peninsula of the U.S. state of Alaska. The unincorporated community of Candle is less than a mile away, while the village of Kiwalik is about 13 miles (21 km) away. The creek's name is attributed to the resemblance of the trees on the banks of the creek to candles when they are covered with snow. With the discovery of gold in 1901, Candle Creek's reputation as a top gold-yielding site was fixed.
Eldorado River is a waterway on the Seward Peninsula]] in the U.S. state of Alaska. It is situated 14 miles (23 km) west of Solomon. This river has its source within a few miles of Salmon Lake, from which it is separated by a low divide. It flows southeast through a broad gravel-filled valley for 30 miles (48 km) to Flambeau River before emptying into Safety Sound. Its headwaters reach the limestones of the Nome series and much of its course lies in a chlorite-albite-schist belt. The Eldorado River provides a southerly drainage into the Bering Sea.
Bonanza River is a waterway on the Seward Peninsula in the U.S. state of Alaska. The headwaters lie close to Venetia Creek and the Koksuktapaga River. It flows southeast for 25 miles (40 km) before reaching Safety Sound, as do the Flambeau and Eldorado Rivers, and then through Safety Inlet to Norton Sound. The village of Solomon is approximately 2 miles (3.2 km) away. Across the divide of West Creek, in the Bonanza River drainage, and lying above the West Creek schists, is a series of green chloride schists and sills of greenstone; these chloritic schists are the prevailing rocks of the divide between Eldorado and Bonanza rivers. In its general character, it is similar to the Eldorado River. Also called Bonanza Cal, later maps indicate California Creek to be a principal tributary of Bonanza River. According to Alfred Hulse Brooks, the Eskimo name is Ki-ul-uk.
Brooks Mountain is the highest peak in the York Mountains range on the Seward Peninsula in the U.S. state of Alaska. It is located in the central part of the Teller Quadrangle, about 25 miles (40 km) east of Cape Prince of Wales. It has an elevation of 2,918 feet (889 m). It has tin ore deposits, and high-grade uranium has also been found in the form of zeunerite.
Ear Mountain is an isolated mountain located on the Seward Peninsula in the U.S. state of Alaska. The mountain, with an elevation of 2,329 feet (710 m), has a belt of Cretaceous tin "granites." Though the mountain is located in an area long known for its tin deposits, it was only in 1953 and 1954 during a survey by the US Bureau of Mines that tin deposits were confirmed to be on Ear Mountain.
Cape Mountain is located 3 miles (4.8 km) southeast of Cape Prince of Wales on the Seward Peninsula in the U.S. state of Alaska. It was named by the surveyor, Alfred Hulse Brooks, in 1900.
Bluestone River is a waterway located on the Seward Peninsula in the U.S. state of Alaska. A tributary of the Tuksuk Channel from the south, Bluestone is a north-flowing stream situated 11 miles (18 km) southeast of Teller. It was named in 1900 by Edward Chester Barnard, topographer of the United States Geological Survey.
Grantley Harbor is a waterway located at the bay of Port Clarence, Alaska, on the Seward Peninsula in the U.S. state of Alaska. The inner harbor at the entrance to the northeast corner of the bay was named after Lord Grantley.
Nuluk River is a waterway on the Seward Peninsula in the U.S. state of Alaska. It enters the Ikpek Lagoon 40 miles (64 km) northeast of Cape Prince of Wales. It heads in the high mountains made up of the Port Clarence limestone about 35 miles south of the Arctic Ocean. For 15 miles (24 km) from its head, the river occupies a canyon, varying from 100–1,000 feet (30–305 m) in depth, cut in Silurian limestones. Fossils have been reported about the head of the river. Northward along its course, the character of the bed rock changes, and calcareous mica-schists are noted. The Silurian limestones dip toward the schists, and near the contact with them, are very highly folded. The coastal plain gravel extends inland farther along the Nuluk River than it does on the other rivers of this region.
Arctic River is a waterway in the U.S. state of Alaska. Situated on the northwestern portion of Seward Peninsula, it rises south of Ear Mountain. It is about 25 miles (40 km) long, and flows into the west side of Shishmaref Inlet. Southeast of Ear Mountain, the course of this river is in a broad basin containing a number of small lakes. Below this basin, the river has cut a well-defined canyon. Viewed from the surrounding hills, the basin appears to be an old lake bed. A broad, flat divide, which has what appears to be an abandoned river channel across it, separates this basin from the drainage of the Kugruk River of the Arctic region. Many of the tributaries of Arctic River were staked by gold miners.
American River is a waterway in the U.S. state of Alaska. Situated on the northwestern portion of Seward Peninsula, it is the eastern and larger fork of the Agiapuk River. It joins the Agiapuk River in a broad, gravel-filled basin, and for 20 miles (32 km) up, is characterized by a wide flood plain and a meandering course. It receives a number of large tributaries from the east, which also have wide floodplains developed in their lower parts. The important tributaries are Portage Creek, Budd Creek, and Igloo Creek, while smaller tributaries are Burke, Gold Run, Dome, and Camp creeks. All of these tributaries received some attention from gold prospectors. The river is easily navigable for small boats for several miles above the mouth of Portage Creek, and the region can also be reached from Teller. Gold had been discovered in the region in September 1901, and a number of the streams were known to be gold-bearing to some extent.
Mary River is a waterway in the U.S. state of Alaska. Situated on the northwestern portion of Seward Peninsula, it was included in the Agiapuk River mining district.
Imuruk Lake is the largest body of fresh water in Seward Peninsula in the U.S. state of Alaska. It measures 31 square miles and has a drainage basin of 102 square miles, It lies on top of a lava plateau at an elevation of 960 feet. The drainage basin is relatively flat, as the maximum elevation, it is only about 1,600 feet. A low gap in the divide between the lake and the head of the right fork of Goodhope River rises only a few feet above the lake. The Fairhaven Ditch takes practically all its water from the lake. Serpentine Hot Springs flow to the Serpentine River, 47 miles northwest of Imuruk Lake.
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Coordinates: 66°08′54″N165°32′24″W / 66.14833°N 165.54°W

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