Every named stream in the Adirondack Park — the feeder waters that line the High Peaks valleys and fill the ponds.
Ragged Lake Outlet drains Ragged Lake northwest toward the Saranac River system — a short, shallow run through mixed forest and wetland typical of the mid-elevation drainages around Saranac Lake. The stream itself sees little attention: no maintained trail follows it, no fishing pressure to speak of, and the corridor offers none of the gradient or pool structure that pulls anglers or paddlers off the main routes. It's the kind of outlet that exists primarily as a dot on the topo map and a brief crossing if you're bushwhacking between Ragged Lake and the larger watershed to the west. If you're at Ragged Lake itself, you're there for the lake — not the outlet.
Rainer Brook is a tributary stream in the Raquette Lake watershed — one of dozens of small feeder brooks that drain into the broader drainage system without much individual documentation in the angling or paddling literature. No species data on file, which likely means it's either too small to hold meaningful trout populations or it simply hasn't been surveyed in recent decades. These unmapped tributaries often serve as seasonal spawning corridors or overflow channels during spring runoff, visible from a canoe route or a backcountry bushwhack but rarely destinations in themselves. Worth noting on a map if you're studying watershed connectivity, but not a water you'd plan a trip around.
Raquette Brook flows through the southern Adirondacks near Indian Lake — part of the broader Raquette River watershed that drains a significant portion of the central Park. The stream sees limited angler attention and no formal DEC stocking records, though native brook trout are likely present in the headwater tributaries if the gradient and canopy are right. Access details are sparse; this is working forest and private inholding country, where stream corridors aren't always marked or maintained for public use. If you're looking for Raquette Brook specifically, confirm access and boundaries with the Indian Lake town office or a local outfitter before you bushwhack.
Ray Brook runs through the hamlet of Ray Brook just off NY-86 west of Lake Placid — the same Ray Brook known for the federal correctional facility and the DEC regional headquarters, not wilderness solitude. The stream drains north from the low hills between the Saranac Lakes and connects to the Saranac River system, quiet water moving through mixed hardwoods and old state land. No formal access points or fishing pressure to speak of — this is a working landscape, not a trailhead. If you're looking for named brook trout water in the Keene corridor, you're better off on the Johns Brook or Slide Brook drainages to the east.
Ray Brook cuts through the hamlet of Ray Brook between Saranac Lake and Lake Placid — a small tributary stream most people cross on NY-86 without stopping. The name appears on maps more for the federal correctional facility and the DEC regional headquarters than for the water itself, which runs narrow and shallow through mixed forest and roadside culverts. It's not a destination fishery or a paddling route — more a named drainage in a region dense with better-known options. If you're looking for moving water in this corridor, the Saranac River system (north) or the Chubb River (south toward Lake Placid) are the more deliberate choices.
Raymond Brook runs through the Old Forge area — one of dozens of small tributaries feeding the Fulton Chain system and the broader Moose River watershed. No formal fish stocking records on file, but the stream likely holds native brook trout in its upper reaches if flow and temperature hold through summer. Without maintained trail access or a known put-in, Raymond Brook is one of those named waters that exists more for watershed mapping than recreation — a connector rather than a destination. If you're poking around Old Forge backcountry by bushwhack or exploring the drainage by canoe, it's there; otherwise, the Fulton Chain lakes pull the attention.
Reall Creek threads through the Old Forge area with minimal fanfare — a tributary stream that appears on topographic maps but carries no fishing reports, no trail register, and no parking-lot folklore. The name survives in DEC records and on USGS quads, but the creek itself remains one of those named waters that exists more in the cadastral record than in paddler or angler memory. Most Old Forge visitors pass within a mile of it without knowing it's there, en route to the Fulton Chain or the Moose River corridor. If you're assembling a completist map of every named flow in the region, Reall Creek earns its dot — but don't expect a pull-off or a put-in.
Red River flows through the Raquette Lake watershed — a minor tributary in a region defined by big water and historical Great Camps, though this particular stream keeps a low profile in the drainage network. No fish data on file, no formal access points documented, and the name itself suggests either an iron-tannin stain common to Adirondack feeder streams or a cartographer's placeholder that stuck. If you're poking around the Raquette Lake backcountry and cross it, you're likely bushwhacking or paddling one of the connecting routes between the major ponds — it's navigational context, not a destination.
Red River runs through the Raquette Lake township in the central Adirondacks — a stream that feeds the broader Raquette River watershed but lacks the angler traffic or documented fish data of its better-known cousins. The name suggests historical logging-era use (red pine rafts, tannin-stained water, or simple surveyor's convention), but specific access points and put-in details are sparse in contemporary records. If you're poking around Raquette Lake proper and see a tributary inlet worth exploring, this is likely it — bring a topo map and expect to bushwhack.
Red River flows through the central Adirondacks near Old Forge — a modest stream that threads through lowland forest and wetland before feeding into the Moose River drainage. It's the kind of water that shows up on the DEC atlas but not in guidebooks: no put-in parking, no trail register, no lean-to a quarter-mile in. The corridor is mostly private land and state forest patchwork, so access is limited and informal — more of a local fishing or bushwhacking reference than a planned destination. If you're poking around the Old Forge backcountry by canoe or on foot, you'll cross it; otherwise, it stays off the list.
Redwater Brook flows through the Tupper Lake region with minimal public documentation — no fish surveys on file, no maintained trail access noted in DEC records, and a drainage pattern that suggests private land or remote state forest without established recreation infrastructure. The name hints at tannin-stained water, common in streams draining wetland and softwood forest, but without access intel or angler reports the brook remains more of a blue line on the map than a known destination. Streams like this often surface in old logging roads or bushwhack routes, worth noting if you're stitching together a longer backcountry route but not a standalone target. Check county tax maps and DEC easement layers before assuming access.
Reservoir Outlet is the discharge stream from Great Sacandaga Lake — engineered flow controlled by the Conklingville Dam at the northeast end of the reservoir, feeding into the Sacandaga River proper as it runs north toward the Hudson. The dam itself dates to 1930, built to regulate downstream flooding and generate hydropower, which means the outlet's character shifts with seasonal drawdowns and release schedules rather than natural hydrology. Not a destination water — more infrastructure than fishery — but it marks the transition point where a 29-mile reservoir becomes a moving river again. Parking and access at the dam site off Conklingville Road in Day.
Risedorph Stream is one of the smaller tributaries feeding the Great Sacandaga Lake system — likely a seasonal flow corridor given the absence of fisheries data and named access points in the DEC records. Streams like this tend to run high during snowmelt and after heavy rain, then drop to intermittent pools by midsummer, serving more as drainage channels than paddling or fishing destinations. The Great Sacandaga basin contains dozens of these unnamed and lightly-documented feeder streams, most of which see more use from deer and beaver than from anglers. If you're exploring the shoreline by boat, expect marshy inlet zones rather than defined banks.
Roaring Branch drains a steep wooded draw in the Lake George Wild Forest — one of dozens of small tributary streams that feed the lake's eastern shore, most unnamed and overlooked in favor of the bigger water downstream. The name suggests seasonal high flow, likely off snowmelt or heavy rain, and points to the kind of whitewater character that gave half the streams in the Park their working names in the logging era. No fish data on record, no formal trails — this is connector hydrology, not destination water. If you're bushwhacking ridges above the lake and cross a loud stream in spring, there's a decent chance you've found it.
Roaring Brook drains the eastern slopes of the High Peaks, carving down from the col between Hedgehog and Noonmark before joining the Ausable near Keene Valley — one of the principal feeder streams for the East Branch watershed. The name delivers: this is a high-gradient stream, loud in spring runoff, audible from NY-73 through most of May. Multiple trails cross or parallel sections of the brook on the approach to Round Mountain, Dix, and the Great Range, but there's no designated fishing access and the gradient keeps most anglers pointed toward the Ausable itself. If you're day-hiking out of Keene Valley in April, you're fording Roaring Brook — plan for wet boots.
Roaring Brook drains east toward Lake George through a wooded fold in the southeastern corner of the Park — one of dozens of small tributaries feeding the lake from the surrounding ridges. The stream picks up volume in spring melt and after heavy rain, but by midsummer it's more trickle than roar in most sections. No formal access or trail infrastructure, and the surrounding terrain is a mix of private land and undeveloped forest, so this is a water you encounter rather than seek out. If you're bushwhacking or exploring old woods roads in the southern Lake George basin, you'll cross it eventually.
Roaring Brook is one of several streams by that name in the Adirondacks — this one draining north through Keene toward the Ausable, fed by spring runoff and year-round seeps from the eastern High Peaks watershed. The name suggests gradient and volume in the right season; by late summer most Adirondack "roaring" brooks are ankle-deep rock gardens. No fish data on record, which often means thin water, short season, or both. If you're hiking in the Keene corridor and cross a swift, cold stream marked Roaring Brook on the map, you're likely looking at snowmelt highway — not a fishing or swimming destination, but the kind of water that reminds you how the mountains work.
Roaring Brook drains north through the Tupper Lake region — one of dozens of tributaries feeding the Raquette River watershed in this stretch of the northwestern Adirondacks. The name suggests rapids or a steep pitch through a rocky channel, typical of the transition zones where Adirondack headwaters drop off the higher ground toward the St. Lawrence drainage. Without formal fish surveys or maintained access, it's a waterway that threads through private timber and state land in the quieter corners of the park — the kind of stream you cross on logging roads or encounter while bushwhacking between better-known destinations. Check DEC public land maps if you're planning to explore off-trail in this drainage.
Roaring Brook flows through the Indian Lake town corridor — one of several small tributaries in the central Adirondacks that carries snowmelt and summer rain down from the ridgelines into the Cedar River or Hudson drainage. The name suggests steep gradient and noisy spring runoff, though without recorded fishery data or maintained access points, this is likely a bushwhack proposition for anglers or a crossing for backcountry skiers working the high country between trail systems. The Indian Lake region holds dozens of these named brooks and feeder streams — most appear on the DEC quad maps but few see regular foot traffic outside hunting season. Worth noting if you're plotting cross-country routes or studying watershed flow for a paddling trip downstream.
Roaring Brook drains north from the High Peaks Wilderness toward the Chubb River and Saranac Lake system — one of several dozen named streams threading the Lake Placid region, most of them unmarked on highway signage and known primarily to bushwhackers and brook trout anglers working upstream from documented access points. The name suggests gradient and volume during spring melt; by late July most Adirondack "roaring" brooks drop to a trickle or a chain of pools depending on canopy and bedrock. Without listed fish data or formal trail access, this is a water that lives in DEC records and on USGS quads — visible from the map, harder to pin down on the ground.
Robbs Creek is a quiet tributary in the Speculator drainage — the kind of small stream that shows up on USGS quads but rarely in trail guides or fish surveys. No state-documented stocking or species records, though small Adirondack feeder streams in this watershed typically hold wild brook trout if the gradient and temperature hold. Access details are sparse; most traffic comes from locals who know the old logging roads or from paddlers working the bigger connecting waters downstream. If you're passing through Speculator and see a bridge crossing on a back road, that's often your best look.
Robinson Brook drains the high country between Keene and the Ausable valleys — one of dozens of unnamed or little-known feeder streams that quietly gather snowmelt and deliver it downslope to larger drainages. No maintained trail follows it, no lean-to marks its banks, and it doesn't appear on most recreation maps, which makes it typical of the Park's network of minor tributaries: ecologically critical, hydrologically productive, and entirely off the radar for anyone not consulting a USGS quad. If you're bushwhacking between ridges in this region and hear moving water, it's likely Robinson Brook or one of its upstream forks.
Rock Cut Brook runs through the Keene valley watershed — a small tributary system feeding into the East Branch of the Ausable, tucked somewhere in the network of seasonal streams that drain the slopes between the High Peaks corridor and the valley floor. No public access data on file, no stocked fish, no trail intersections that make it onto the standard maps. It's the kind of water that shows up on USGS quads but not in guidebooks — a reference point for property lines and old logging roads, more useful to surveyors than to hikers. If you're bushwhacking the ridgelines above Keene, you've probably crossed it without knowing its name.
Rock Pond Brook drains northeast out of the Rock Pond drainage in the Paradox Lake Wild Forest — a small tributary system in terrain that sees more hunting traffic than through-hikers. The stream runs through mixed hardwood and hemlock corridors typical of the mid-elevation eastern Adirondacks, eventually feeding into the larger Paradox Lake watershed. No formal trailhead or maintained path follows the brook itself; access is via old logging roads and bushwhack from the Paradox Lake area. Species data isn't on record, but beaver activity and brook trout habitat are the safe assumptions in these quiet eastern drainages.
Roger Brook feeds the network of streams threading through the Saranac Lake watershed — one of dozens of named tributaries that remain largely invisible to the map-following public but known to locals who fish the backcountry beaver meadows or paddle the Saranac chain in low water. No official access data, no fish surveys on record, no trailhead on file — the kind of water that exists mostly as a blue line on DEC maps and a name in the GNIS database. These brooks often hold wild brookies in their headwater pockets, but Roger Brook's specific character — whether it's a seasonal trickle or a year-round feeder, whether it drains a hillside or connects two ponds — remains undocumented in public records. Worth noting if you stumble across it; not worth planning a trip around unless you already know the country.
Rooster Comb Brook drains the northeast shoulder of Rooster Comb Mountain in Keene — a small, steep tributary that feeds into the Johns Brook watershed before making its way to the East Branch of the Ausable. The brook cuts through a mix of hardwood and conifer on a relatively short run, gaining elevation quickly in the upper reaches and likely running high only during spring melt and heavy rain. It's named for the mountain above it, which forms part of the Great Range horseshoe visible from the Johns Brook Valley. This is backcountry drainage — no road crossings, no fishing pressure, no named campsites — more likely encountered as ambient sound on a bushwhack than as a destination in itself.
Round Lake Stream connects Round Lake to the Raquette River drainage north of Tupper Lake — a small tributary water in working forest country, logged and regrown, with none of the High Peaks foot traffic. The stream moves through low-gradient wetland and mixed hardwood before emptying into the main flow; expect beaver work, blown-down timber, and the kind of paddling or bushwhacking that requires a tolerance for ambiguity. No established access points or marked trails — this is private timberland interspersed with Forest Preserve, so topo and parcel maps are non-negotiable if you're planning a visit. If you're fishing the Raquette or exploring the Round Lake area by canoe, the stream mouth is worth noting as a secondary put-in or a place to glass for waterfowl in spring and fall.
Round Pond Brook drains the high country south of Indian Lake village — a small tributary system feeding into the Cedar River drainage, tucked into the west-central backcountry where named streams outnumber maintained trails. No fish stocking records, no formal access points, and no lean-tos within the immediate watershed; this is working forest and remote wetland, the kind of water that appears on a USGS quad but rarely sees foot traffic outside hunting season. If you're headed into this zone, you're navigating by compass and contour lines, not trail signs. The brook itself is likely intermittent in summer, fast and cold during snowmelt.
Round Pond Brook drains east from Round Pond in the Town of Indian Lake — a backcountry drainage in the central Adirondacks where named streams often connect modest ponds to larger watersheds with little fanfare and less foot traffic. No fish data on record, no maintained trail system flagged to the brook itself, and the kind of obscurity that keeps it off both the hatchery truck routes and the weekend itinerary. If you're bushwhacking the drainage or working a topo sheet between Round Pond and the Cedar River corridor, you'll cross it — otherwise it stays a blue line on the map. Check DEC wetland and wild forest classifications before planning any access.
Rowland Hollow Creek feeds into the Great Sacandaga Lake basin — one of dozens of small tributaries draining the rolling terrain south and west of the reservoir. No fish data on record, no maintained trails, no lean-tos — this is the kind of Adirondack water that exists on the DEC list and the USGS map but not in the hiking guide or the fishing report. If you're exploring the southern Adirondack fringe by truck or canoe, you'll cross creeks like this on forest roads or find their mouths tucked into coves along the Sacandaga shoreline. Worth knowing it has a name; not worth planning a trip around it unless you're already there.
