Forest HILL

California

Video

1

LOCATION

Foresthill is a rare gem nestled in the lower Sierra Foothills of Placer County, just 50 minutes east of Sacramento. Spanning approximately 1,200 hectares, the property offers a blend of gentle slopes and dramatic ridgelines with panoramic views stretching up to 50 kilometers. Its location balances tranquility and accessibility—only a short drive from iconic destinations like Lake Tahoe, Squaw Valley (site of the 1960 Winter Olympics), and Auburn’s private airport, while being adjacent to the charming unincorporated town of Foresthill.

The area enjoys a mild four-season climate and is already equipped with critical infrastructure including roadways, water from an 8.6 million m³ reservoir, electricity via an adjacent substation, and general plan approvals for residential and commercial development. Whether envisioning a high-end residential enclave, a retirement community, or a resort destination, Foresthill is a rare investment opportunity set against the backdrop of natural beauty and long-term growth.

The property is about approx. 1/10th of the size of the city of San Francisco. For those familiar with the San Francisco Peninsula, an apt description would be about approx. 3/4th the size of Hillsborough. The Foresthill property is just shy of approx. 1/6th the size of Hong Kong island. It’s about approx. 2.5 hours drive from San Francisco International Airport

Foresthill History

Forest Hill was first settled when the Forest House hotel and trading post was built after gold discoveries in 1850. The post office was established in 1859 under the name “Forest Hill”, but was changed to “Foresthill” in 1895 for reasons that are difficult to determine.

Foresthill was one of the largest towns in Placer County. By the late 1850s it boasted hotels, stores, banks, saloons, and numerous homes and other structures. The productive hard-rock mines of the area would ensure that the town remained viable for many decades.

An October, 1859 edition of the Daily Alta California provided a glowing report of conditions at Foresthill at the time: “Forest Hill is, for its size and age, as fine a village as I met in my travels. Its citizens are highly favored with good prospects, in addition to the enormous amount of gold already obtained.”

2

Foresthill

Goldmine

Foresthill has a significant gold mining legacy rooted in the California Gold Rush.

Foresthill Mining District, California holds three significant drift mines —
Baltimore , Dardanelles, and Mayflower — all cited in historic records for substantial production or remaining gravel in the Foresthill Channel. Baltimore reportedly has [2 million cubic yards of un-mined gravel. Historic yields in this channel ranged from [0.008 oz/yd3] to [0.18 oz/yd3], representing a potential in-situ value in the tens of millions to over a billion dollars at current gold prices. We are seeking qualified partners for a Phase I evaluation to confirm volume and grade, with options for [purchase or profit-sharing arrangements.

To develop this opportunity requires modern technology (a completely subterranean operation), political savvy, and financial resources.

Baltimore Mine

The Baltimore is an underground drift mine cited in the 1927 State Mineralogist report as having ~2 million cubic yards of unmined Foresthill Channel gravels. No historic production figures are recorded, but its proximity to prolific producers (New Jersey, Jenny Lind, Independent) suggests high potential. – Low-end (0.008 oz/yd3): ~16,000 oz → ~$54 million at August 2024 prices – High-end (0.18 oz/yd3): ~360,000 oz → ~$1.22 billion at August 2024 prices

Dardanelles Mine

About 3,700 feet west of the Baltimore adit, the Dardanelles was worked by both drift mining and hydraulicking. Historic production is reported at $2,000,000 (~125,000 oz at $16/oz). Remaining gravel volume is unquantified, but its explicit mention in the 1927 State Mineralogist report indicates significance.
Using a conservative 10–40% non-recovery range, the remaining potential is: – 14,000–56,000 oz → ~$48 million to ~$190 million at August 2024 prices

Mayflower Mine

Roughly 2 miles northeast of Baltimore, the Mayflower was a major Foresthill Channel producer with historic output of $1,000,000 (~62,500 oz at $16/oz). Under a 10–40% non-recovery range, remaining potential is: – 7,000–28,000 oz → ~$24 million to ~$95 million at August 2024 prices

The Baltimore and Dardanelles drift mines are cited in the 1927 State Mineralogist report for substantial unmined Foresthill Channel gravels. The Baltimore is estimated at 2,000,000 cubic yards; the Dardanelles, while unquantified, warranted specific mention. Historic yields range from 0.008 oz/yd3 (hydraulicking at Dardanelles) to 0.18 oz/yd3 (drift-mined gravels in the Foresthill Channel through both mines). At current gold prices (~$3,400/oz), that equates to $54M to $1.22B in potential in-situ value (Baltimore only).

Baltimore & Dardanelles Mines –

Gold Recovery Opportunity Foresthill Mining District, Placer County, California – Sierra Nevada Foothills

The Baltimore and Dardanelles drift mines are cited in the 1927 State Mineralogist report for substantial unmined Foresthill Channel gravels. The Baltimore is estimated at 2,000,000 cubic yards; the Dardanelles, while unquantified, warranted specific mention. Historic yields range from 0.008 oz/yd3 (hydraulicking at Dardanelles) to 0.18 oz/yd3 (drift-mined gravels in the Foresthill Channel through both mines). At current gold prices (~$3,400/oz), that equates to $54M to $1.22B in potential in-situ value (Baltimore only).

1. Executive Summary

The Baltimore and Dardanelles underground drift mines are located in the historic Foresthill Mining District of Placer County, California, within the Foresthill Tertiary Channel system. Both mines are cited in the 1927 California State Mineralogist’s Gravels of the Middle Fork of the American River.
Baltimore Mine – Estimated 2,000,000 cubic yards of unmined channel gravels.
Dardanelles Mine – Remaining gravel volume not quantified; presumed significant due to explicit mention in
the report. Historic yields in the district range from 0.008 oz/yd3 (hydraulicking at the Dardanelles) to 0.18 oz/yd3
(drift-mined gravels in the Foresthill Channel, which flows through both mines). At August 2025 gold prices (~$3,400/oz), the Baltimore alone represents a potential in-situ gross value between $54 million and $1.22 billion, depending on grade.
We are seeking a qualified mining partner to fund and execute a Phase I program to confirm gravel volume and grade, with the option to negotiate purchase or profit-sharing terms.

2. Historic Production Context

Mine Historic Production Value* Gold Price at TimeApprox. Ounces Notes
Baltimore N/A – – Estimated 2,000,000 yd3 of unmined channel gravels
Dardanelles $2,000,000 $16/oz ~125,000 oz Mix of drift mining and hydraulicking
Mayflower $1,000,000 $16/oz ~62,500 oz Located ~2 miles NE, also on Foresthill Channel
* Historical figures from state and mining district records; some are third-party historical estimates.

3. Remaining Resource Potential

Using a 10–40% non-recovery range — consistent with conservative estimates of residual gravels in similar drift mines — and applying yield assumptions for Baltimore based on historic grades*:
Baltimore – 2,000,000 yd3 at 0.008–0.18 oz/yd3 = 16,000–360,000 oz (*).
Dardanelles – ~14,000 to 56,000 oz remaining.
Mayflower – ~7,000 to 28,000 oz remaining.
– Combined Multi-Mine Potential – 37,000 to 444,000 oz.

4. Key Advantages for Modern Evaluation

1. High-Value Target – Documented unmined gravels in one of California’s most productive Tertiary channels.
2. Historic Grade Variability – From low-grade hydraulicking yields to high-grade drift-mined pay.
3. Infrastructure Access – Road network, grid power, and water resources in place for rapid mobilization.
4. Potentially Preserved Tunnels – If intact, may reduce cost and time to access gravels.
5. Proximity to Proven Producers – Baltimore adjoins historically high-yield mines (New Jersey, Jenny Lind,
Independent).
5. Phase I Objectives

1. Quantify Remaining Gravel – Volume and distribution in target channels.
2. Determine Grade – Representative sampling to establish economic potential.
3. Evaluate Access – Assess condition of existing workings or define drilling approach.

3

Foresthill

History & Facts

Foresthill has a significant gold mining legacy rooted in the California Gold Rush.

Foresthill Today

Local employment by local residents in lieu of commuting off the hill would have a positive effect of reducing the number of commuters during the rush hour. On the flip side, a small portion of residents of the active adult retirement community still would be working. I had read somewhere that the percentage was around 12%, with half working from home. Which means about 6% would have some type of commute. Some obviously would commute locally in Foresthill, some off the hill, some during commute hours and some not. On balance, the number of local jobs created resulting in the reduction of commute hour traffic should outweigh the few retirees who might utilize the road during commute hours. As a result, any increase in the size of a retirement community should not have a negative impact on commute hour traffic. Of course, the specifics of any proposal would have to be analyzed. In addition to the above, the four-fold over-estimation in the FDCP EIR indicates that, at the present time, mitigation measures would not be necessary for a very long time to come. ECONOMIC. As noted in the transportation section, about 500 jobs would be created locally, fulfilling the FDCP’s stated high priority goal of increasing employment on the divide. There are a handful of active adult retirement communities located approximately 20 miles from the nearest urban areas. Economic development in Foresthill would be expected to mirror their experience. For example, in Sequim, Washington, a couple dozen part-time medical specialties opened locally to cater to the senior community. Most, according to the local librarian, operated one to two days a week. Of course, this benefits the non-retiree parts of the community as well. FISCAL. EPS also evaluated the fiscal impacts of Foresthill conceptual plan. Given that seniors commit very few crimes, it is not surprising that the report indicated a net fiscal surplus to the County. SEWAGE. Appendix E of the FDCP requires a wastewater treatment plant with enough capacity to serve both the foresthill project as well as the commercial areas of downtown. The growth of Foresthill commercial area predates many of the current regulations related to sewage disposal. Inclusion of a wastewater treatment plant would rectify potential problems. FIRE. One of the advantages of a master plan community on the Foresthill project site is that dangers from wildfires can be mitigated. Communities built to fire resistance standards and maintained to enforce the standards have been shown to be spared from wildfires. One example is the Crosby subdivision area of Rancho Santa Fe, California. The 2007 WITCH fire burnt everything around this particular subdivision. No homes were lost in the Crosby subdivision. (Source KQED)

What are the “ancient river gravels”?

  • Long before the present American River existed, ancient rivers flowed across the Sierra Nevada millions of years ago (primarily during the Tertiary period, around 50–20 million years ago).
  • These rivers deposited thick beds of gravel, sand, and cobbles, often cemented with clay or silica.
  • Later, volcanic eruptions covered these riverbeds with lava and ash, protecting the gravels from erosion.

Why is this important at Foresthill?

  • The Foresthill Divide, near the Middle Fork of the American River in Placer County, sits on top of one of these buried ancient channels.
  • These gravels are extremely rich in placer gold, which eroded out of quartz veins in nearby bedrock and was concentrated by ancient water flow.
  • During the Gold Rush and after, hydraulic mining (using high-pressure water cannons) was heavily used to wash away entire hillsides to reach these gravels.
  • The Foresthill region—including sites like the Mayflower, Baltimore, and other mines—produced millions of ounces of gold from these ancient channel deposits.

Key geological points about Foresthill gravels

  • Thickness: In some places, over 100 feet of auriferous (gold-bearing) gravel.
  • Gold distribution: Coarse nuggets often found at the base (bedrock contact), with finer gold throughout.
  • Protection by volcanic cap: The gravels are often hidden beneath hard “cap rock” like andesite or rhyolite.
  • Mining history: Operations peaked in the mid-to-late 1800s and early 1900s, though some small-scale mining still occurs.

Modern relevance

  • Historic value: Sites are studied by geologists and mining historians to understand Sierra Nevada river evolution.
  • Exploration potential: Some deposits may still hold untapped gold, especially where hydraulic mining was banned before full extraction.
  • Environmental issues: Old hydraulic mining caused massive siltation of rivers and destruction of downstream farmland, leading to the 1884 Sawyer Decision banning hydraulic mining debris.

1) Where the ancient channel runs (Foresthill Divide, Placer County)

  • Provenance & age: These are Tertiary “auriferous gravels” (pre-Quaternary), the remnants of an ancient American River system later capped by volcanics. Darwin OnlineSierra RiversGSA Conference
  • District extent: The Forest Hill (Foresthill) District spans Foresthill town and the classic diggings at BathTodd Valley/Dardanelles, and Yankee JimsWestern Mining History
  • Channel path (simplified): The main early-Tertiary Middle Fork channel enters from Michigan Bluff (E/NE of Foresthill), swings north near Bath, and meanders SW across the Divide—locally called the Forest Hill Channel. Width commonly 300–1,500 ft, up to ~2,500 ft near the Dardanelles Mine; bedrock troughs often >100 ft deepMuseum of CaliforniaMindat

Landmarks you’ll see in historical geology/mining write-ups:

  • Red PointJenny Lind CanyonBaltimore MineDardanelles/Todd ValleyYankee Jims — all along or adjacent to the old channel or its benches. SCVHistoryMindatWestern Mining History

If you’re standing on the Divide today, you’re literally on a broad ridge of ancient river bed between the North and Middle Forks of the American River. Sierra Nevada GeotourismWikipedia

2) Gold endowment & “what’s left”

What’s known (historic extraction):

  • By 1868, mines around Forest Hill had reportedly yielded >$10 million (1860s dollars) and moved into large-scale hydraulicking and later drift mining. Western Mining History
  • Example tally: at several classic Forest Hill exposures, an estimated ~8.63 million cubic yards of gravel were removed for ~$5 million in gold (historic dollars). This illustrates both the scale and the low-to-moderate average grade typical of broad channel gravels. Western Mining History
  • Gravels can be 50–200+ ft thickcoarse “pay” often concentrates on bedrock (basal gravels), with bench/upper gravels variably auriferous. Sierra RiversMindat

What might remain (realistic view):

  • After the 1884 Sawyer Decision curtailed debris hydraulicking statewide, many benches and deeper channel segments became uneconomic to access, leaving pockets behind—especially deep, cap-rock-protected reaches and off-channel benches. (This is a general Sierra gravel pattern reflected in the literature.) Caltrans
  • The Foresthill channel’s width (hundreds to 2,500 ft) and depth (>100 ft) mean not all basal pay was exposed by historic hydraulicking; drift mining targeted some beds, but discontinuous pay and water/ground conditions limited extraction. MindatWestern Mining History

Back-of-envelope framework (how geos estimate “leftover”):

  • Outline the paleochannel footprint (base + benches) from maps/sections (Lindgren plates, Foresthill History Society pamphlets).
  • Subtract areas demonstrably mined (hydraulic pits, drifts) from aerials/LiDAR.
  • Apply conservative thickness for basal gravels (e.g., 5–15 ft) where untouched.
  • Use typical basal grades from nearby documented drifts (historical reports often cite fractions of a gram/ton up to multiple g/t in streaks).
  • Sensitivity-test with pay-streak continuity factors (very discontinuous).

Because pay is highly streaky, any “total remaining ounces” would carry big error bars. Still, the geology and history support the common miner’s adage up there: some gold remains where mining stopped, especially in deep, capped, or awkward segments that weren’t practical with 19th-century methods.

Handy primary references 

  • Classic surveys & maps: Lindgren’s Tertiary Gravels of the Sierra Nevada (USGS Prof. Paper; includes Forest Hill Divide/Mayflower cross-sections). Sierra Rivers
  • Local syntheses: Foresthill Historical Society pamphlets on Ancient River Beds and Gold in Ancient Channels (nice summaries, with period photos and mine notes). foresthillhistory.org+1foresthillhistory.org
  • District overviews: Museum of CA (Gold Districts), Western Mining History, and Mindat entries with locations, production notes, and geology snippetsMuseum of CaliforniaWestern Mining History+1Mindat

Presented By

John Pang

Title

Owner / Operating Principal

Email

info@foresthill.com

Company

Realty One Group Extreme

Web

foresthill.com

Phone

(650) 699-2838

License #

DRE # 02208098 – Office DRE # 02226794