EVERETT LAKE

Species Weather Hydrology


Everett Lake is located in Butte County, California, and is a popular fishing spot for both locals and visitors. The lake is primarily stocked with rainbow trout, and other fish species such as bluegill, bass, and catfish can also be found. Nearby activities include hiking, camping, picnicking, and boating. Fishing tips include using bait such as worms or power bait and targeting areas around the dam or inlet. The best time to visit is from spring to fall, with average temperatures ranging from 60-85°F.

July 26, 2024

°F

°F

mph

Windspeed

%

Humidity

Regional Streamflow

33

Cubic Feet Per Second

248

Cubic Feet Per Second

112

Cubic Feet Per Second

18

Cubic Feet Per Second

Explore the Interactive Map

View recreational hotspots like fishing, camping, and parks, alongside climate-related data such as river levels, snowpack, and weather forecasts. Enjoy 3D mapping for an immersive experience, and switch to satellite view for a detailed look at your favorite spots. Simply click, explore, and discover nature like never before!

5-Day Weather Forecast

16-Day Weather Forecast

Nearby Camping & Amenities

Camping Area Campsites Reservations Toilets Showers Elevation
Milsap Bar 20 1,639 ft
Limesaddle - Lake Oroville State Rec Area Numerous 925 ft
Wyandotte 28 5,060 ft
Black Rock Tent(Family ) 20 5,052 ft
Bidwell - Sacramento River State Park Numerous 137 ft
Tooms RV Numerous 5,049 ft
Little North Fork 6 3,807 ft
Peninsula Tent (Family ) 25 5,033 ft
Little Beaver 120 5,066 ft
Orland Buttes - Black Butte Lake 35 521 ft

Explore Nearby Places

Lava Beds National Monument


Lava Beds National Monument is located in northeastern California, near the border with Oregon. The monument is home to over 700 caves, many of which were formed by volcanic eruptions. Visitors to the area can explore these caves, hike through the surrounding lava fields, and learn about the geological history of the region. One of the main attractions at Lava Beds National Monument is the lava tube caves. These caves were formed when molten lava flowing through the area cooled and hardened on the outside, while the interior lava continued to flow. This created large hollow tubes that visitors can ...