Every named river in the Adirondack Park — the Hudson, the Moose, the Raquette, the Sacandaga, and the rivers that drain the High Peaks.
Newcomb River drains the southwestern corner of the High Peaks Wilderness — a dark-water flow that runs north from the outlet of Lake Harris through a forested corridor before joining the Hudson River near the hamlet of Newcomb. The river sees light paddling traffic in the spring when flows are up, but it's mostly a thoroughfare for anglers working the pools and riffles between the lake and the confluence. The shoreline is state land for most of its length, with access tied to the back roads and informal pull-offs that skirt the flow rather than any maintained trailhead. It's quiet water in a working corner of the park — more transit than destination.
Newcomb River drains northeast out of Harris Lake and Rich Lake, flowing roughly parallel to NY-28N through the town of Newcomb before joining the Hudson River near the hamlet. It's a quiet, meandering run through mixed hardwood and conifer — more of a working drainage than a destination river, though paddlers occasionally float sections in high water during spring runoff. The river corridor is undeveloped for most of its length, passing through a mix of state land and private forest holdings. Access is limited to road crossings and informal put-ins where the highway comes close to the water.
The North Branch Black River cuts through the western Adirondack plateau above Old Forge, draining a network of beaver ponds and wetlands before converging with the main stem near Forestport. It's a remote headwater system — no road crossings, no state campgrounds, no named put-ins — which means it stays quiet even when the Moose River and Fulton Chain are stacked with boats. The corridor holds brook trout, but access is bushwhack or private-land negotiation; most paddlers and anglers work the mainstem downstream where the DEC manages public easements. If you're scouting this stretch, start with the DEC Region 6 office in Watertown for current easement maps and flow conditions.
The North Branch Grasse River drains a broad, low-lying swath of forest northeast of Tupper Lake — classic north-country water that braids through alder thickets and beaver meadows before converging with the Middle Branch near the town of Childwold. It's working river country, not trail-accessed wilderness: most paddlers who know it launch from roadside pull-offs along county routes or from private camp roads, often during high water in spring or after heavy rain. The fishing record is sparse, but the drainage holds the usual suspects — brookies in the headwater tributaries, pickerel and panfish in the slower pools. This is low-profile Adirondack water: no lean-tos, no parking lots, no crowds.
The North Branch Grasse River drains northwest out of the central Adirondacks through a mix of private timberland and state forest — it's a working woods waterway, not a recreation corridor. The river feeds the main stem of the Grasse River west of the park boundary, eventually joining the St. Lawrence watershed; access is scattered and undeveloped, mostly via logging roads and informal put-ins where the branch crosses through Forest Preserve parcels. This isn't paddling-guide country — it's a drainage you cross on the way to something else, or fish if you know a local with permission on a good stretch. No formal boat launches, no DEC signage, no species surveys in the record.
The North Branch Great Chazy River drains a broad swath of northeastern Franklin County before joining its other tributaries near the Canadian border — a quieter watershed than the crowded High Peaks corridor to the south, but part of the same lake-and-river matrix that defines the northern Adirondacks. The drainage runs through working forestland and old farmsteads; access is typically roadside where Route 374 and smaller county roads cross the flow. No established put-ins or marked trails in the common hiking sense — this is explorer territory, better suited to anglers willing to bushwhack or paddlers scouting their own lines in spring. Check DEC regs for the Great Chazy basin; some tributaries have seasonal trout closures.
The North Branch Moose River drains west from the Moose River Plains Wild Forest toward Old Forge — a backcountry waterway that sees more hunters and paddlers than hikers, threading through mixed hardwood and wetland corridors in one of the park's quieter corners. Access typically requires forest roads or longer paddles from established put-ins along the main Moose River system; this isn't a roadside stop. The watershed connects to the broader Moose River network — a region defined by remote ponds, old logging routes, and fall moose sightings that justify the name. Fish data is sparse, but the system historically held brook trout in its cleaner tributaries.
The North Branch Moose River drains a remote stretch of working forest west of Old Forge — timber company land, gated roads, and the kind of country where you're more likely to see a logging truck than a trailhead sign. The branch feeds into the main Moose River system that eventually reaches the Black River, part of the old log-drive corridor that defined the southwestern Adirondacks through the early 20th century. Public access is limited and undefined; this is a river you find by studying topographic maps and knowing which gates open seasonally. Brook trout likely hold in the headwater tributaries, but nobody's keeping formal records.
The North Branch Moose River drains the high country west of Old Forge, flowing north through state forest land before joining the main stem of the Moose near McKeever. It's classic Adirondack headwater terrain — rocky gradient, beaver activity in the flats, and corridors thick enough with alder and blowdown that most anglers and paddlers stick to the main Moose downstream. The North Branch sees most of its traffic from hunters and snowmobilers working the network of seasonal roads that cross the drainage. Access details are sparse; if you're headed in, bring a good topo and expect to bushwhack.
The North Branch Saranac River flows west out of the High Peaks toward the village of Saranac Lake — a cold, fast water with the kind of wooded banks and boulder runs that read as classic Adirondack trout water, though no fish data is on record. The river corridor sees less foot traffic than the main stem, but the NY-86 corridor parallels much of the flow, meaning pullover access and sight-fishing opportunities for those who know where to look. It drains a wide basin north of the MacIntyre Range and eventually joins the main Saranac River downstream — part of the broader watershed that feeds the Saranac Lakes chain and, ultimately, Lake Champlain.
The North Branch Saranac River drains the northwest shoulder of the Saranac Lakes Wild Forest, running roughly parallel to NY-3 before merging with the main stem near Saranac Lake village. It's a working river — cold, fast in spring, studded with midstream boulders and pocket pools that hold brook trout through summer if you're willing to bushwhack the corridor. Access is opportunistic: bridge crossings, dirt road pull-offs, and the occasional old logging trace that dead-ends at the bank. This is not a documented paddling route or a named fishing destination — it's the kind of water you find by studying the blue line on a map and walking in with waders.
The North Branch Saranac River drains a wide swath of northern Franklin County before joining the main stem near Bloomingdale — a working river more than a destination, threading through a mix of state land and private inholdings west of the village of Saranac Lake. The upper sections run quiet and marshy through spruce lowlands; downstream it picks up current and takes on the character of a paddle route, though access points are scattered and poorly marked. This is cold-water trout habitat by designation, but specific stocking records and angler reports are thin — it fishes like a tributary system that sees more moose than pressure. Best known locally as a place you cross on the way to somewhere else.
The North Fork Boquet River drains the eastern High Peaks wilderness — a network of cold headwater tributaries that converge near Keene Valley before joining the main Boquet River and eventually feeding Lake Champlain. The river runs fast and technical through mixed hardwood and conifer forest, dropping elevation quickly off the eastern slopes of the range — more whitewater corridor than fishing destination, though brook trout hold in the deeper pockets between cascades. Access points are scattered along backcountry trails radiating from Keene Valley, but this is a river you cross more often than you paddle or fish. In spring runoff it's loud, cold, and impassable without a bridge.
North Fork East Creek drains a narrow valley system in the Paradox Lake region — a tributary network that feeds into the broader Schroon River watershed. The stream traces a cold-water corridor through mixed hardwood and hemlock stands, typical of mid-elevation waterways on the eastern flank of the Park. No public access data or fisheries records on file, which usually means either private holdings along the corridor or a routing that doesn't intersect maintained trail systems. Worth noting for watershed mapping or bushwhack planning, but not a named destination in the usual sense.
Northwest Bay Brook drains north into Northwest Bay on Lake George — a small tributary system in the Brant Lake region that threads through mixed hardwood forest and low wetland before reaching the lake's quieter northwestern arm. The stream itself is modest and largely overlooked; no formal trail access, no stocking records, and the kind of flow that depends on snowmelt and spring rain to stay fishable. Most paddlers encounter it as a feeder channel when kayaking the upper bay, where the mouth opens into a shallow delta choked with lily pads by midsummer. If brook trout are present, they're wild holdovers in the headwater stretches — but there's no data to confirm it.
