NSS 2021 Convention ~ June 28-July 2* Register

Medicine Lake Highlands

Quick Read:

The most diverse and least visited of the five volcanic centers in California is the Medicine Lake Highlands Volcanic Area, located on the Shasta-Trinity National Forest. The area contains hundreds of unique volcanic features and lava tube caves. If you have the opportunity during your convention visit - don't miss this one!

This area is a bit less developed than Lava Beds National Monument, and offers a more rugged caving experience. You should defiinitely check with the cave trip team at convention headquarters to get directions. As with any cave trip, you should let someone know where you are going and when you plan to return. Mobile phone coverage is unreliable in this area and there are no services once you leave the highway.

Medicine Lake Lava Tube

Welcome to the Medicine Lake Highlands!

Medicine Lake Highlands is the largest identified volcano (in total area) within California, and is one of the most unique geologic features in North America. Because this subrange of the Cascades is somewhat remote, the fascinating nature of this area is largely unappreciated.

Medicine Lake

Medicine Lake

Medicine Lake is in the caldera of the volcano, which measures 4.3 by 7.5 miles. The caldera may have formed by collapse after a large volume of andesite was erupted from vents along the caldera rim. The distribution of late Pleistocene vents, mostly concentrated along the rim, suggests that ring faults already existed when most of the andesite erupted.

Click here to download a USGS geology field-trip guide to the Medicine Lake Highlands.

The great Medicine Lake shield volcano's broad, gently sloping profile (stretching some 15 miles from east to west and nearly 25 miles north and south) belies the fact that it is actually larger in mass than nearby Mt. Shasta. The Medicine Lake Highlands Volcanic Area exceeds 200 square miles and takes in portions of three National Forests; the Modoc, Klamath and Shasta-Trinity in Modoc and Siskiyou Counties. On the Shasta- Trinity the area lies within the boundaries of the McCloud Ranger District. It rises east of Mt. Shasta near the south end of the string of Cascade volcanoes that stretch northward from Mt. Lassen into British Columbia.

Approximately 100,000 years ago, the great volcano underwent a series of eruptions which undermined the center of the mountain and the crest subsided to create a huge crater or caldera. Around the margins of this subsidence, new, smaller volcanoes arose; they are called rampart volcanoes. Medicine Lake now partially fills the crater.

Geologists speculate over what events took place that caused the unusual shapes and features to form and how a series of eruptions changed the face of the countryside in the area. One thing is clear, however; more than a million years of volcanic activity have produced a landscape that is perhaps California's most diverse volcanic field. Furthermore, volcanic eruptions that produced geological features within the Medicine Lake Highlands were no less dramatic than the volcanic eruptions which took place on Mt. St. Helens.

Scenic Attractions

Volcanic formations, such as glass and lava flows, pumice deposits, lava tubes, cinder cones, craters, and faults are found throughout the Medicine Lake Highlands Volcanic Area.

Lava Flows
Lava flows off the flanks of the Medicine Lake shield volcano extend in every direction for over 30 miles. The jumbled, rugged plains of broken rock are interspersed with timbered hills and buttes. The Giant Crater, Tilted Rocks, and Burnt Lava Flows are examples of very recent flows, presenting a vast panorama or stark, unvegetated lava fields.

Obsidian Flow at Medicine Lake

Obsidian Flow at Medicine Lake. Photo: Matt Bowers

Glass mountains (flows) and pumice deposits
The most recent major volcanic activity yet identified in the area occurred about 300 years ago at Little Glass Mountain. These eruptions first spread white pumice for miles around. A nearby cinder cone, Pumice Stone Mountain, was completely covered with pumice and a startling, smooth, white dome remains. These pumice eruptions were followed by flows of black volcanic glass, called obsidian. There are other obsidian flows in the Highlands area, some of which are over 1,000 acres in size. Prehistoric people used this material to make arrowheads and spearpoints. Many archaeological sites have been identified, and some artifacts indicate that the Highlands have been inhabited for at least 4,500 years.

Three types of craters exist in the Medicine Lake Highlands Volcanic Area. In addition to cinder craters, there are explosion and subsidence craters. Explosion craters are usually recognized by the large fragments or bombs strewn around the crater. Subsidence craters are formed by underground lava flows which deplete a magma chamber causing the cone to fall in upon itself. Consequently, subsidence craters are characterized by steep walled rims, while explosion craters are usually more funnel-like. Giant and Double-Hole Craters, located upon the Giant Crater Lava Flow, are examples of subsidence craters; while Deep Crater, near the Burnt Lava Flow, is an explosion crater.

Jot Dean Ice Cave at Medicine Lake

Jot Dean Ice Cave at Medicine Lake. Photo: Matt Bowers

Lava tubes and ice caves
The lava flows in this area feature literally hundreds of "caves" called lava tubes. Many are seldom visited and probably more are yet undiscovered. These features were formed when molten lava flows cooled and solidified on the surface while the fluid interior continued to flow, forming a cave-like tube. They are often multitiered and may extend for miles. The Giant Crater lava tube, though partially collapsed, extends for almost 18 miles. Many lava tubes and other depressions on the lava flow landscape such as Jot Dean Ice Cave, tend to collect cold air, and large ice formations which form during the winter often persist through the summer.

Natural bridges
Natural bridges, formed when tubes collapsed on either side, can be seen throughout the area.

Spatter cones
These miniature "volcanoes" are formed by hot gasses mixed with molten lava which escaped up through a fissure in the earth's surface. A handful of these chimney-like spatter cones appear in a neat row at one site in the Highlands, probably marking the path of an underground lava tube.

Triple Crater

Double-Hole Crater, located upon the Giant Crater Lava Flow, is a classic example of a subsidence crater. Photo: Matt Bowers

Cinder cones
There are over 100 cinder cones throughout the Medicine Lake Highlands. Oso and Porcupine Buttes, Pumice Stone Mountain, and Paint Pot Crater are examples of this type of volcano which forms when cinders pile up around a central vent. The internal structure of a cone can be examined at Oso Butte near Harris Springs Campground.

Many north-south oriented faults cross the Highland area. These faults are especially apparent along Highway 89, giving it that "rolling" character where the ground has been raised along a fault. A 50 foot high fault headwall (scarp) is strikingly seen near Julia Glover Flat. This north-south fault pattern continues eastward to the Colorado Plateau, forming what geologists call the Basin Range Province.

See it for yourself

Hopefully, we have given you an awareness and perhaps an appreciation of the Medicine Lake Highlands Volcanic Area and what it has to offer a curious sightseer.

Most of these features are easily visited. The Geologic Special Interest Area near Giant Crater is accessible on Forest Road #43N11 just two miles off the Medicine Lake Road (49). This area features spatter cones, lava flows and lava tubes. While the features described here are the most unique, there are countless other points of interest within the Medicine Lake Highlands Volcanic Area. If spectacular scenery is what you want to see, visit the area for yourself. The land ranges from rugged lava flows, barren of most vegetation, to thickly timbered mountain peaks. Small lakes, such as little Medicine Lake, Bullseye, and Blanche, are set among the trees and the view from the higher peaks and cinder cones is breathtaking. One word of caution however... the roads are good, but there are NO services after you leave Highway 89.

Jot Dean Ice Cave

Today's Weather: Lava Beds National Monument, CA

  • Updated: Wednesday, February 24 at 7:38 pm
  • Reporting Station: VAN BREMMER (VABC1)
  • Elevation: 5,303 ft.
  • GPS: 41.642967;-121.794875
  • Data provided by: National Weather Service
30° F
Mostly Clear

Regional Map Forecast Wind: 18 mph (E)
Humidity: 40%
Dewpoint: 9°F
Barometer: N/A
Visibility: N/A

Tonight: Mostly clear. Low around 21, with temperatures rising to around 23 overnight. Southeast wind 2 to 10 mph.
Thursday: Mostly sunny. High near 49, with temperatures falling to around 43 in the afternoon. West wind 2 to 21 mph, with gusts as high as 31 mph.