Mount Shasta

Mount Shasta is a big volcano in Siskiyou County, California. It is part of the Cascade Range and stands very tall at 14,179 feet (4,322 meters). This makes it the second-highest peak in the Cascades and the fifth-highest in all of California.

People call Mount Shasta a potentially active stratovolcano, meaning it could erupt again someday. It is the most voluminous stratovolcano in the Cascade Volcanic Arc, with an estimated volume of 85 cubic miles (350 cubic kilometers). The area around the mountain is part of the Shasta–Trinity National Forest.

Different cultures have special names for the mountain. In the Shasta language, it is called Waka-nunee-Tuki-wuki, and in the Karuk language, it is known as Úytaahkoo. For information about the nearby town, see Mount Shasta, California. To learn about other peaks named Shasta, see List of peaks named Shasta.

Description

The name "Shasta" has an unclear origin, possibly coming from a local people or changed by early settlers. Mount Shasta is linked to its smaller peak called Shastina, and together they stand out strongly in the area. On clear winter days, the mountain can be seen from California far to the south.

The mountain is made up of four overlapping volcanic cones, creating an interesting shape. Shastina, the most noticeable of these, would be the fourth-highest peak in the Cascade Range if it were a separate mountain. Mount Shasta has several glaciers, with the largest ones flowing down from the main peak. The Whitney Glacier is the longest, and the Hotlum Glacier holds the most ice in California.

History

The first written record of Mount Shasta was made on May 20, 1817, by Spaniard Narciso Durán. He described seeing a very high, snow-covered hill. In 1826, Peter Skene Ogden saw the mountain, and later gave the name “Sasty” or “Sastise” to a nearby peak. The name Shasta was officially used for Mount Shasta in 1841.

Mount Shasta became an important landmark for travelers along the Siskiyou Trail in the 1820s. This trail was an ancient route used by Native Americans between California’s Central Valley and the Pacific Northwest. When the California Gold Rush began in the early 1850s, settlers arrived in the area. The first successful climb of Mount Shasta happened in 1854.

By the late 1800s, Mount Shasta interested scientists, writers, and explorers. Famous climbers like John Muir reached the summit. The completion of the Central Pacific Railroad in 1887 brought more visitors to the area. Resorts and hotels were built to welcome these new tourists.

In the 1950s, Mount Shasta received a record amount of snow during one storm. In 1976, it was declared a National Natural Landmark.

Legends

Main article: Legends of Mount Shasta

The Klamath Tribes have stories about Mount Shasta. They believe the mountain is home to Skell, a spirit who lives above, and Llao, a spirit who lives below. These spirits are said to have fought using hot rocks and lava.

Italian settlers who came to the area in the early 1900s brought strong Catholic traditions. Today, there are many places of worship near Mount Shasta, including a Buddhist monastery and areas for Native American rituals.

Mount Shasta has also inspired many other stories. Some believe a hidden city of advanced people from a lost land called Lemuria is hidden inside the mountain. These stories grew popular in the early 1900s.

In 2024, a large bronze statue of the Virgin Mary was placed in the Ski Park to honor Ray Merlo, who passed away from cancer in 2020.

Climate

Mount Shasta gets a lot of snow each winter, especially near the timberline where it receives around 450 to 500 inches of snow on average. However, it does not get as much snow as some other volcanoes in the Cascade range, like Rainier, Baker, and Lassen. This is because Mount Shasta is located in the rain shadow of the Klamath Mountains, which block many storms from reaching it. The Klamath Mountains are very tall, reaching over 9,000 feet, and they sit directly to the west and southwest of Mount Shasta, right in the path of the main storm track.

Geology

Mount Shasta formed about 593,000 years ago when lava flowed near McBride Spring. Over time, a large volcano grew, but a big part of it fell down between 300,000 and 360,000 years ago, creating a huge landslide that moved into Shasta Valley.

The mountain has four main cones. The oldest one is seen at Sargents Ridge. Another, called Misery Hill, formed between 15,000 and 20,000 years ago. Shastina, another part of the mountain, formed after the last ice age and has a crater at its top. The newest and highest part, Hotlum Cone, formed about 8,000 years ago. It has had several eruptions, with the last big one happening about 200 years ago.

Scientists watch Mount Shasta closely. Though it has been quiet recently, there are signs that it could erupt again. The United States Geological Survey considers it a high-threat volcano because of its history and the ice on its slopes.

Climbing

The best time to climb Mount Shasta is during the summer, from late April to October, but some people also try in the winter. The mountain is also a favorite spot for backcountry skiing. Experienced skiers can go down many of the same paths used for climbing, and there are easier slopes near the bottom of the mountain.

Climbers don’t need to book ahead or get a special permit to try climbing Mount Shasta, but they must get a pass and a permit for the wilderness area.