Antelope: Geode Digging in Wasco County, Oregon
Updated June 2026
Antelope is a mapped rockhounding spot in Wasco County, Oregon. Reported finds include agate, chalcedony, geode, jade, jasper. Below: coordinates, access notes, nearby spots, and trip-planning links.
Map showing Antelope in Wasco County, Oregon
Quick details
- Access
- Permission required
- County
- Wasco County
- State
- Oregon
- Nearest road
- Antelope Highway
- Coordinates
- 44.90805, -120.73853
Geology at Antelope
This spot sits on John Day/Clarno Group; John Day Formation, mapped as tuffaceous sedimentary rocks, buff, red, green; fossils: roots cavities stems leaves locally well preserved and abundant fossils; rhyolitic to dacitic glass shards; alteration: rocks rich in altered glass and bentonite; mineralogy: feldspar pyroxene amphobile; rock fragments, tuff, green, buff; fossils: roots cavities stems leaves locally well preserved and abundant fossils; rhyolitic to dacitic glass shards; alteration: rocks rich in altered glass and bentonite; mineralogy: feldspar pyroxene amphobile; rock fragments, lapilli tuff, buff; rhyolitic to dacitic glass shards; alteration: rocks rich in altered glass and bentonite; mineralogy: feldspar pyroxene amphobile; fossils: roots cavities stems leaves locally well preserved and abundant fossils; rock fragments, tuffaceous claystone, buff; rock fragments; fossils: roots cavities stems leaves locally well preserved and abundant fossils; rhyolitic to dacitic glass shards; alteration: rocks rich in altered glass and bentonite; mineralogy: feldspar pyroxene amphobile, tuffaceous siltstone, and red; fossils: roots cavities stems leaves locally well preserved and abundant fossils; rhyolitic to dacitic glass shards; alteration: rocks rich in altered glass and bentonite; mineralogy: feldspar pyroxene amphobile; rock fragments that formed roughly 56 to 23 million years ago. Volcanic rock like this is classic geode and thunderegg country: gas cavities in the old flows can line themselves with quartz or agate over time.
- Mapped unit
- John Day/Clarno Group; John Day Formation
- Age
- 56–23 Ma (Eocene to Oligocene)
- Rock types
- tuffaceous sedimentary rocks, buff, red, green; fossils: roots cavities stems leaves locally well preserved and abundant fossils; rhyolitic to dacitic glass shards; alteration: rocks rich in altered glass and bentonite; mineralogy: feldspar pyroxene amphobile; rock fragments, tuff, green, buff; fossils: roots cavities stems leaves locally well preserved and abundant fossils; rhyolitic to dacitic glass shards; alteration: rocks rich in altered glass and bentonite; mineralogy: feldspar pyroxene amphobile; rock fragments, lapilli tuff, buff; rhyolitic to dacitic glass shards; alteration: rocks rich in altered glass and bentonite; mineralogy: feldspar pyroxene amphobile; fossils: roots cavities stems leaves locally well preserved and abundant fossils; rock fragments, tuffaceous claystone, buff; rock fragments; fossils: roots cavities stems leaves locally well preserved and abundant fossils; rhyolitic to dacitic glass shards; alteration: rocks rich in altered glass and bentonite; mineralogy: feldspar pyroxene amphobile, tuffaceous siltstone, and red; fossils: roots cavities stems leaves locally well preserved and abundant fossils; rhyolitic to dacitic glass shards; alteration: rocks rich in altered glass and bentonite; mineralogy: feldspar pyroxene amphobile; rock fragments
- Elevation
- 2,660 ft
Geologic mapping via Macrostrat and the underlying state geological survey maps (CC BY 4.0). Bedrock at the surface can vary within a mapped unit.
Best time to visit Antelope
Best months: February to November. Typical highs run 89°F in midsummer and 44°F in midwinter, with winter lows near 27°F.
Climate normals: NOAA 1991-2020 monthlies, ANTELOPE 6 SSW station (6 mi away), adjusted for elevation.
Land & collecting status
Permission required before collecting
Requires landowner or agency permission before any collecting. Do not enter without explicit authorization.
Public-land rules vary by agency, season, and field office. The RockHoundR app pulls live BLM, USFS, NPS, and tribal overlays so you can see exactly which agency manages the ground at this spot.
Sources & verification
Spot details combine the public RockHoundR location dataset, normalized mineral labels, agency land-status checks in the app, and community submissions. Coordinates are approximate until verified in the field.
State guidance last verified:
- BLM Oregon/Washington — Rockhounding & mineral material
- Oregon Department of Geology and Mineral Industries (DOGAMI)
- Oregon Parks and Recreation Department — beach collecting rules
- Community submissions reviewed against published agency rules
Found at Antelope
Each chip opens all spots that produce that material; the encyclopedia link opens the full ID and field guide.
Nearby rockhounding spots
Other rockhounding spots within driving distance of Antelope.
- Polka Dot Agate MineJefferson County, Oregon · 11 mi awayPolka Dot Agate, Thundereggs
- AshwoodJefferson County, Oregon · 12 mi awayAgate, Chalcedony, Geode
- WillowdaleJefferson County, Oregon · 12 mi awayAgate, Chalcedony, Geode
- Priday Agate BedsJefferson County, Oregon · 14 mi awayAgate, Chalcedony, Jasper
- John Day River & StreamsWasco County, Oregon · 15 mi awayFossilized Ferns
- Richardson's Rock RanchJefferson County, Oregon · 17 mi awayThundereggs
- Wheeler High School Fossil BedsWheeler County, Oregon · 26 mi awayFossils
- Lucky Strike MineCrook County, Oregon · 29 mi awayThundereggs
Across the state line from Antelope
Antelope is close enough to the Oregon border that the next-closest rockhounding spots are in a neighboring state. Worth knowing if you are already on the road.
