Placer gold is found downstream of gold-bearing rock, concentrated on or near bedrock and wherever stream current slows. The U.S. Geological Survey says the best odds are in “further systematic study of known productive areas, rather than in efforts to discover unknown areas.” In practice, that means picking a known gold district, finding public or permitted water there, and reading the stream.
This guide is desk research from the USGS, the California, Utah and Washington state geological surveys, and a BLM and Forest Service panning booklet. A historic district is not a promise that a spot is open to the public or still holds gold. Land status and rules vary by state and change, so check with the land manager before you dig.
Lode gold and placer gold
The USGS describes two main deposit types. Lode deposits hold gold in the solid rock where it was deposited. Placer deposits are “concentrations of gold derived from lode deposits by erosion” that gravity has sorted into stream sediments. The USGS says the areas likely to hold valuable lode gold have been explored so thoroughly that an inexperienced prospector without ample capital “has very little chance” of finding a workable lode.
Placers are where hobby prospectors start. The USGS calls panning “the simplest, easiest, and least expensive method” of separating gold from stream sediment and “the method most commonly employed by the beginning prospector.”
Where gold settles in a stream
Gold is heavy. The USGS says gold particles “move downward during high-water periods when the entire bed load of sand, gravel, and boulders is agitated,” so they are “often concentrated on or near bedrock.” Concentrations of gold in gravel are called pay streaks.
| Spot | Why gold collects there (agency) |
|---|---|
| On or near bedrock | Gold sinks while the bed load moves in high water (USGS) |
| Bedrock crevices and pockets | They act as natural riffles (BLM/Forest Service) |
| Below rapids and falls; deep pools | Turbulent water slows and drops gold (BLM/Forest Service) |
| Downstream side of boulders | Current is deflected and slows (BLM/Forest Service) |
| Inside bends; upstream ends of point bars | Good for fine gold, renewed yearly in runoff (BLM/Forest Service) |
| Depressions in sand and gravel bars | Fine gold collects where current slackens (USGS, Utah) |
| With black sands | Heavy minerals settle with the gold (USGS) |
The USGS says prospectors in gold country look “where coarse sands and gravel have accumulated and where ‘black sands’ have concentrated.” Magnetite is the most common mineral in black sands. The booklet for Alaska’s Kenai Peninsula adds that spring, early summer and just before freeze-up are good times there because water is low and gold-bearing gravel is exposed, and it asks panners to dig only in active, unvegetated stream gravels.
Rock clues
Placer gold comes from gold-bearing rock upstream. The Utah Geological Survey says Utah’s placers “are usually associated with areas of igneous rocks” and that “finding gold is possible in any stream or river that crosses a gold-mineralized area.” The White Mountain National Forest in New Hampshire says gold there is associated with a wide variety of rock types, “granitic and volcanic rocks in particular,” along with stream gravels and glacial deposits.
Washington’s Division of Geology and Earth Resources explains that weathering frees gold and other heavy minerals from lode rock, and that in streams “heavy minerals (including gold) settle into crevices and any other depressions in the streambed and form placer deposits.”
Historic placer districts by state
The USGS publication Prospecting for Gold in the United States (1967) summarized the main placer regions. It is old, so treat it as a map of where gold has been found, not where it remains or who owns the land now. State survey notes are added where available.
| State or region | Placer areas the agencies name | Source |
|---|---|---|
| California | Feather, Mokelumne, American, Cosumnes, Calaveras, Yuba, Trinity rivers | USGS; CGS adds Sacramento River |
| California | Older Tertiary gravels in the same Mother Lode area | USGS |
| Alaska | Yukon River basin including Fairbanks; Nome beaches | USGS |
| Alaska | Copper River and Kuskokwim River drainages | USGS |
| Montana | Southwest: Last Chance Gulch at Helena; Alder Gulch, Madison County | USGS |
| Idaho | Boise Basin; Salmon River; Clearwater at Elk City, Pierce, Orofino | USGS |
| Idaho | Flour gold in Snake River sands, southern Idaho | USGS |
| Colorado | Fairplay district (Park County); Breckenridge (Summit County) | USGS |
| Oregon | Rogue River tributaries: Greenback and Applegate districts | USGS |
| Oregon | Blue and Wallowa Mountains streams; Sumpter; Burnt and John Day rivers | USGS |
| Washington | Columbia and Snake rivers; streams of central and northeast WA | USGS; WA DNR |
| South Dakota | Black Hills: Deadwood area; French Creek near Custer | USGS |
| Utah | Bingham Canyon; Colorado, Green and San Juan rivers | Utah GS |
| Utah | Henry, La Sal, Abajo and Tushar mountains | Utah GS |
| Arid Southwest | Intermittent streams in parts of NV, AZ, NM and southern California | USGS |
| Southern Appalachians | Eastern-slope streams in MD, VA, NC, SC, GA and AL | USGS |
| New Hampshire | Wild Ammonoosuc River and Tunnel Brook (history of gold recovery) | White Mountain NF |
A few details matter for planning. The USGS says arid-region placers lack a permanent water supply, so they need dry or semi-dry recovery methods. The Utah Geological Survey says most Utah placer gold is flour gold that “is difficult to recover,” and that Bingham Canyon’s original topography has been altered by open-pit mining. Washington’s survey map comes with a warning that many of the areas it lists are closed to the public.
Set expectations before you go
Both the USGS and the California Geological Survey say most placer deposits “have been thoroughly reworked at least twice.” The USGS estimates that fewer than 1 in 1,000 people who prospected in the western United States ever made a strike, and the California survey calls about 1 in 1,000 a conservative estimate. The Utah Geological Survey says that after more than 100 years of work, the chance of finding large concentrations in Utah’s streams is small.
That does not make a day of panning pointless. It means the realistic goal is learning to read a stream and recovering some color, not income.
How to research a specific area
- Start with the state geological survey. The Utah Geological Survey lists its placer compilations, such as UGS Circular 47 and USGS Bulletin 1357, and the California Geological Survey lists gold publications such as Gold Districts of California.
- Read the stream once you are there. Use the spots in the table above, and work the active channel.
- Confirm who manages the land. The California Geological Survey reminds prospectors that “you must always obtain permission from the owner to prospect on private property.” On a mining claim, BLM’s 2026 claims packet says “you must have permission from the current claimant” to prospect; see how mining claims work . For places set aside for the public, see recreational gold panning areas by state . Rules for pans and sluices also vary; the sluice box guide shows how much they differ by agency.
- Bring the right first tools. A pan and a classifier are enough to sample a new area; see the gold panning kits and pans guide . When something shiny shows up, check it with the gold, pyrite and mica tests .
FAQ
Where is the best place to look for gold in a creek?
Look where fast water slows down. The BLM and Forest Service booklet points to slower water below rapids and falls, deep pools, the downstream side of boulders, inside bends, the upstream ends of point bars, and bedrock crevices. The USGS adds that gold often concentrates on or near bedrock.
Can you find gold in the eastern United States?
Yes, in small amounts. The USGS says limited gold has been washed from streams on the eastern slope of the southern Appalachians, in parts of Maryland, Virginia, the Carolinas, Georgia and Alabama, and a small amount has come from placers in New England.
Is there still gold in old placer areas?
Some, but expect small amounts. The USGS and the California Geological Survey say most placer deposits have been reworked at least twice, and both say the best chances are in known productive areas.
Sources
- U.S. Geological Survey, Prospecting for Gold in the United States (1967) (publication record ) (placer regions by state, reworked placers, odds, lode prospects, panning, eastern placers, arid placers)
- U.S. Geological Survey, Gold (General Interest Publication) (lode and placer deposits, gold on or near bedrock, pay streaks, black sands)
- California Geological Survey, Note 24: Hints for Gold Prospectors (2002) (Mother Lode rivers, reworked placers, odds, private property permission, gold publications)
- Utah Geological Survey, Utah Gold (placers and igneous rocks, Utah placer areas, flour gold, publications)
- Washington Division of Geology and Earth Resources, Recreational Gold Panning (revised 2010) (how placers form, central and northeastern Washington, closed areas)
- BLM and USDA Forest Service, Gold Panning: Guide to Recreational Gold Panning on the Kenai Peninsula (2018 revision) (where to look in a stream, season, active gravels)
- White Mountain National Forest, other recreation opportunities (rock types, Wild Ammonoosuc River and Tunnel Brook)
- BLM Montana-Dakotas, Mining Claims Packet (March 12, 2026) (claimant permission)