What is Kelseyville known for?

Kelseyville became the first white settlement in Lake County. The first blacksmith shop was opened by a blacksmith named Benham in 1857.

Does Kelseyville have snow?

Kelseyville, California gets 41 inches of rain, on average, per year. The US average is 38 inches of rain per year. Kelseyville averages 2 inches of snow per year. The US average is 28 inches of snow per year.

What is the elevation of Kelseyville?

1,384′
Kelseyville/Elevation

What county is Kelseyville?

Lake County
Kelseyville/Counties

What county is Lower Lake California in?

Lower Lake/Counties

When did Mt Konocti erupt?

11,000 years ago
History. Mount Konocti probably first erupted some 350,000 years ago and last erupted 11,000 years ago.

What is the zip code for Kelseyville California?

95451
Kelseyville/Zip codes

What’s it like living in Kelseyville CA?

Kelseyville is a beautiful place in the center of wine country. It is family friendly and community oriented. The best part about Kelseyville is the community, everyone knows everyone and families have been intermingled for years.

Is Lower Lake California Safe?

Is Lower Lake, CA Safe? The D+ grade means the rate of crime is higher than the average US city. Lower Lake is in the 25th percentile for safety, meaning 75% of cities are safer and 25% of cities are more dangerous.

What is the elevation of Lower Lake CA?

1,371′
Lower Lake/Elevation

Lower Lake is located 4.5 miles (7.2 km) southwest of the City of Clearlake, and 13 miles (21 km) southeast of Kelseyville. It is at an elevation of 1,371 feet (418 m).

Is Mt Konocti an active volcano?

A dormant volcano, Mount Konocti is said by geologists to be a composite cone of lava that was built up over millions of years of gentle eruptions. The volcano became dormant approximately 10,000 years ago, making it the youngest mountain in all of California’s coastal ranges.

Is Cobb mountain a volcano?

2.1. Volcanic rocks in the Geysers – Cobb Mountain area are part of the late-Pliocene-Holocene Clear Lake volcanic field that occurs within the eastern Coast Range of northern California, east of the San Andreas fault and southwest of the active Cascade magmatic arc (Fig. 1; Hearn et al., 1981, 1995).