Mount Shasta

Mount Shasta (Karuk: Úytaahkoo or "White Mountain")[5][6] is a potentially active[7] volcano at the southern end of the Cascade Range in Siskiyou County, California. At an elevation of 14,179 feet (4321.8 m), it is the second-highest peak in the Cascades and the fifth-highest in the state. Mount Shasta has an estimated volume of 85 cubic miles (350 km3), which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.[8][9] The mountain and surrounding area are part of the Shasta–Trinity National Forest.

Mount Shasta
MtShasta aerial
Aerial view of Mount Shasta from the southwest, with sun low in the west
Highest point
Elevation14,179 ft (4,322 m) [2] NAVD88
Prominence9,772 ft (2,979 m) [1]
Isolation335 mi (539 km) [1]
Parent peakNorth Palisade[1]
Coordinates41°24′33″N 122°11′42″W / 41.409196033°N 122.194888358°WCoordinates: 41°24′33″N 122°11′42″W / 41.409196033°N 122.194888358°W[2]
Mount Shasta is located in California
Mount Shasta
Mount Shasta
Location in California, U.S.
Mount Shasta is located in the United States
Mount Shasta
Mount Shasta
Mount Shasta (the United States)
LocationShasta–Trinity National Forest, California, U.S.
Parent rangeCascade Range
Topo mapUSGS Mount Shasta
Age of rockAbout 593,000 years
Mountain typeStratovolcano
Volcanic arcCascade Volcanic Arc
Last eruption1786[3]
First ascent1854 by E. D. Pearce and party[4]
Easiest routeAvalanche Gulch ("John Muir") route: talus/snow climb[4]


Mount Shasta is connected to its satellite cone of Shastina, and together they dominate the landscape. Shasta rises abruptly to tower nearly 10,000 feet (3,000 m) above its surroundings.[4] On a clear winter day, the mountain can be seen from the floor of the Central Valley 140 miles (230 km) to the south.[10] The mountain has attracted the attention of poets,[11] authors,[12] and presidents.[13] It is dormant.

The mountain consists of four overlapping volcanic cones that have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft (3,760 m) Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mount Rainier, Rainier's Liberty Cap, and Mount Shasta itself).[4]

Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge[14] runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not now have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft (3,000 m) primarily on the north and east sides.[4] The Whitney Glacier is the longest, and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft (3,400 m) on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek glaciers.


The oldest-known human settlement in the area dates to about 7,000 years ago.

At the time of Euro-American contact in the 1820s, the Native American tribes who lived within view of Mount Shasta included the Shasta, Okwanuchu, Modoc, Achomawi, Atsugewi, Karuk, Klamath, Wintu, and Yana tribes.

The historic eruption of Mount Shasta in 1786 may have been observed by Lapérouse, but this is disputed. Although perhaps first seen by Spanish explorers, the first reliably reported land sighting of Mount Shasta by a European or American was by Peter Skene Ogden (a leader of a Hudson's Bay Company trapping brigade) in 1826. In 1827, the name "Sasty" or "Sastise" was given to nearby Mount McLoughlin by Ogden.[15] An 1839 map by David Burr lists the mountain as Rogers Peak.[16] This name was apparently dropped, and the name Shasta was transferred to present-day Mount Shasta in 1841, partly as a result of work by the United States Exploring Expedition.

Mount Shasta Farm
Mount Shasta seen from south of Weed, California

Beginning in the 1820s, Mount Shasta was a prominent landmark along what became known as the Siskiyou Trail, which runs at Mount Shasta's base. The Siskiyou Trail was on the track of an ancient trade and travel route of Native American footpaths between California's Central Valley and the Pacific Northwest.

The California Gold Rush brought the first Euro-American settlements into the area in the early 1850s, including at Yreka, California and Upper Soda Springs. The first recorded ascent of Mount Shasta occurred in 1854 (by Elias Pearce), after several earlier failed attempts. In 1856, the first women (Harriette Eddy, Mary Campbell McCloud, and their party) reached the summit.[17][18]

King WhitneyGlacier
Clarence King exploring the Whitney Glacier in 1870

By the 1860s and 1870s, Mount Shasta was the subject of scientific and literary interest. In 1854 John Rollin Ridge titled a poem "Mount Shasta." A book by California pioneer and entrepreneur James Hutchings, titled Scenes of Wonder and Curiosity in California, contained an account of an early summit trip in 1855.[19] The summit was achieved (or nearly so) by John Muir, Josiah Whitney, Clarence King, and John Wesley Powell. In 1877, Muir wrote a dramatic popular article about his surviving an overnight blizzard on Mount Shasta by lying in the hot sulfur springs near the summit.[20] This experience was inspiration to Kim Stanley Robinson's short story "Muir on Shasta".

The 1887 completion of the Central Pacific Railroad, built along the line of the Siskiyou Trail between California and Oregon, brought a substantial increase in tourism, lumbering, and population into the area around Mount Shasta. Early resorts and hotels, such as Shasta Springs and Upper Soda Springs, grew up along the Siskiyou Trail around Mount Shasta, catering to these early adventuresome tourists and mountaineers.

In the early 20th century, the Pacific Highway followed the track of the Siskiyou Trail to the base of Mount Shasta, leading to still more access to the mountain. Today's version of the Siskiyou Trail, Interstate 5, brings thousands of people each year to Mount Shasta.

From February 13–19, 1959, the Mount Shasta Ski Bowl obtained the record for the most snowfall during one storm in the U.S., with a total of 15.75 feet (480 cm).[21]

Mount Shasta was declared a National Natural Landmark in December 1976.[22]


Sunrise on Mount Shasta
Sunrise on Mount Shasta

The lore of some of the Klamath Tribes in the area held that Mount Shasta is inhabited by the Spirit of the Above-World, Skell, who descended from heaven to the mountain's summit at the request of a Klamath chief. Skell fought with Spirit of the Below-World, Llao, who resided at Mount Mazama by throwing hot rocks and lava, probably representing the volcanic eruptions at both mountains.[23]

Italian settlers arrived in the early 1900s to work in the mills as stonemasons and established a strong Catholic presence in the area. Many other faiths have been attracted to Mount Shasta over the years—more than any other Cascade volcano. Mount Shasta City and Dunsmuir, California, small towns near Shasta's western base, are focal points for many of these, which range from a Buddhist monastery (Shasta Abbey, founded by Houn Jiyu-Kennett in 1971) to modern-day Native American rituals. A group of Native Americans from the McCloud River area practice rituals on the mountain.[24]

Mount Shasta has also been a focus for non-Native American legends, centered on a hidden city of advanced beings from the lost continent of Lemuria.[25] The legend grew from an offhand mention of Lemuria in the 1880s, to a description of a hidden Lemurian village in 1925. In 1931, Wisar Spenle Cerve wrote Lemuria: the lost continent of the Pacific, published by the Rosicrucians, about the hidden Lemurians of Mount Shasta that cemented the legend in many readers' minds.[25]

In August 1987, believers in the spiritual significance of the Harmonic Convergence described Mount Shasta as one of a small number of global "power centers".[26] Mount Shasta remains a focus of "New Age" attention.[27]


2016 60cm orthophoto mosaic overlaid on 3m slope map (derived from digital elevation model). Scale 1:50,000.

About 593,000 years ago, andesitic lavas erupted in what is now Mount Shasta's western flank near McBride Spring. Over time, an ancestral Mount Shasta stratovolcano was built to a large but unknown height; sometime between 300,000 and 360,000 years ago the entire north side of the volcano collapsed, creating an enormous landslide or debris avalanche, 6.5 cu mi (27 km3)[28] in volume. The slide flowed northwestward into Shasta Valley, where the Shasta River now cuts through the 28-mile-long (45 km) flow.

What remains of the oldest of Mount Shasta's four cones is exposed at Sargents Ridge on the south side of the mountain. Lavas from the Sargents Ridge vent cover the Everitt Hill shield at Mount Shasta's southern foot. The last lavas to erupt from the vent were hornblende-pyroxene andesites with a hornblende dacite dome at its summit. Glacial erosion has since modified its shape.

The next cone to form is exposed south of Mount Shasta's current summit and is called Misery Hill. It was formed 15,000 to 20,000 years ago from pyroxene andesite flows and has since been intruded by a hornblende dacite dome.

Black Butte from Weed, California-750px
Nearby Black Butte, seen from Weed, California

There are many buried glacial scars on the mountain which were created in recent glacial periods ("ice ages") of the present Wisconsinian glaciation. Most have since been filled in with andesite lava, pyroclastic flows, and talus from lava domes. Shastina, by comparison, has a fully intact summit crater indicating Shastina developed after the last ice age. Shastina has been built by mostly pyroxene andesite lava flows. Some 9,500 years ago, these flows reached about 6.8 mi (10.9 km) south and 3 mi (4.8 km) north of the area now occupied by nearby Black Butte. The last eruptions formed Shastina's present summit about a hundred years later. But before that, Shastina, along with the then forming Black Butte dacite plug dome complex to the west, created numerous pyroclastic flows that covered 43 sq mi (110 km2), including large parts of what is now Mount Shasta, California and Weed, California. Diller Canyon (400 ft (120 m) deep and 0.25 mi (400 m) wide) is an avalanche chute that was probably carved into Shastina's western face by these flows.

The last to form, and the highest cone, the Hotlum Cone, formed about 8,000 years ago. It is named after the Hotlum glacier on its northern face; its longest lava flow, the 500-foot-thick (150-metre) Military Pass flow, extends 5.5 mi (8.9 km) down its northeast face. Since the creation of the Hotlum Cone, a dacite dome intruded the cone and now forms the summit. The rock at the 600-foot-wide (180-metre) summit crater has been extensively hydrothermally altered by sulfurous hot springs and fumaroles there (only a few examples still remain).

In the last 8,000 years, the Hotlum Cone has erupted at least eight or nine times. About 200 years ago the last significant Mount Shasta eruption came from this cone and created a pyroclastic flow, a hot lahar (mudflow), and three cold lahars, which streamed 7.5 mi (12.1 km) down Mount Shasta's east flank via Ash Creek. A separate hot lahar went 12 mi (19 km) down Mud Creek. This eruption was thought to have been observed by the explorer La Pérouse, from his ship off the California coast, in 1786, but this has been disputed.[29]

Volcanic status

During the last 10,000 years, Mount Shasta has erupted an average of every 800 years, but in the past 4,500 years the volcano has erupted an average of every 600 years. The last significant eruption on Mount Shasta may have occurred about two centuries ago.[3]

Diller Canyon
Diller Canyon on Shastina from Weed

Mount Shasta can release volcanic ash, pyroclastic flows or dacite and andesite lava. Its deposits can be detected under nearby small towns. Mount Shasta has an explosive, eruptive history. There are fumaroles on the mountain, which show Mount Shasta is still alive.

The worst-case scenario for an eruption is a large pyroclastic flow, such as what occurred in the 1980 eruption of Mount St. Helens. Since there is ice, such as Whitney Glacier and Mud Creek Glacier, lahars would also result. Ash would probably blow inland, perhaps as far as eastern Nevada. There is a small chance an eruption could result in a collapse of the mountain, as happened when Mount Mazama in Oregon collapsed to form what is now called Crater Lake, but this is of much lower probability.

The United States Geological Survey monitors Mount Shasta[30] and rates it as a very high-threat volcano.[31]


Shasta boulab
Mount Shasta's west face, June 2009

The summer climbing season runs from late April until October, although many attempts are made in the winter.[4] In winter, Sargents Ridge and Casaval Ridge, to the east and west of Avalanche Gulch,[32] respectively, become the most traveled routes, to avoid avalanche danger. Mount Shasta is also a popular destination for backcountry skiing. Many of the climbing routes can be descended by experienced skiers, and there are numerous lower-angled areas around the base of the mountain.[4]

The most popular route on Mount Shasta is Avalanche Gulch route, which begins at the Bunny Flat Trailhead and gains about 7,300 feet (2,200 m) of elevation in approximately 11.5 miles (18.5 km) round trip. The crux of this route is considered to be to climb from Lake Helen, at approximately 10,443 feet (3,183 m), to the top of Red Banks. The Red Banks are the most technical portion of the climb, as they are usually full of snow/ice, are very steep, and top out at around 13,000 feet (4,000 m) before the route heads to Misery Hill.[33] The Casaval Ridge route is a steeper, more technical route on the mountain's southwest ridge best climbed when there's a lot of snow pack. This route tops out to the left (north) of the Red Banks, directly west of Misery Hill. So the final sections involve a trudge up Misery Hill to the summit plateau, similar to the Avalanche Gulch route.[34]

Mount Shasta west face
Mount Shasta's west face as seen from Hidden Valley high on the mountain. The west face gulley is an alternate climbing route to the summit.

No quota system currently exists for climbing Mount Shasta, and reservations are not required. However, climbers must obtain a summit pass and a wilderness permit to climb the mountain. Permits and passes are available at the ranger station in Mount Shasta and the ranger station in McCloud, or climbers can obtain self-issue permits and passes at any of the trailheads 24 hours a day.[35]

See also

Mount Shasta aerial
Aerial view of Mount Shasta and vicinity from the east, in the spring


  1. ^ a b c "Mount Shasta, California". Retrieved January 6, 2016.
  2. ^ a b "MT SHASTA". NGS data sheet. U.S. National Geodetic Survey. Retrieved January 6, 2016.
  3. ^ a b "Global Volcanism Program - Shasta". Retrieved 23 October 2017.
  4. ^ a b c d e f g Selters, Andy; Michael Zanger (2006). The Mount Shasta Book (3rd ed.). Wilderness Press. ISBN 0-89997-404-X.
  5. ^ Bright, William; Susan Gehr. "Karuk Dictionary and Texts". Retrieved 2012-07-06.
  6. ^ The origin of the name "Shasta" is vague, perhaps from Russian (Чистая, meaning "white, clean, pure" or Счастье, meaning "happiness, luck, fortune, felicity"); the name might have been given to the mountain by the early Russian settlers in California.
  7. ^ Dan Dzurisin; Peter H. Stauffer; James W. Hendley II; Sara Boore; Bobbie Myers; Susan Mayfield (1997). "Living with Volcanic Risk in the Cascades" (PDF). USGS. USGS. p. 2. Retrieved 2017-03-29.
  8. ^ Orr, Elizabeth L.; William N. Orr (1996). Geology of the Pacific Northwest. New York: The McGraw-Hill Companies. p. 115. ISBN 0-07-048018-4.
  9. ^ "Mount Shasta and Vicinity, California". USGS. Retrieved 2009-10-22.
  10. ^ In 1878 the Coast and Geodetic Survey triangulated between heliotropes atop Mount Shasta and Mount St. Helena, 192 miles (309 km) south.
  11. ^ Miller, Joaquin; Malcolm Margolin; Alan Rosenus (January 1996) [1873]. Life amongst the Modocs: unwritten history. Berkeley: Urion Press (distributed by Heyday Books). ISBN 0-930588-79-7.
  12. ^ Muir, John 1838-1914. Letters, 1874-1888, of a personal nature, about Mount Shasta. In: Bade, William Frederic. The Life and Letters of John Muir. New York: Houghton Mifflin Co., 1923. Vol. II, pp. 29-41, 49-50, 82-85, 219. Two Volumes. Cited at Mount Shasta Collection MS176 Archived 2008-05-13 at the Wayback Machine. Retrieved 2008-04-08.
  13. ^ Roosevelt, Theodore 1858-1919. Letter to Harrie Cassie Best, dated Nov. 12, 1908, White House. In: James, George Wharton 1858-1923. Harry Cassie Best: Painter of the Yosemite Valley, California Oaks, and California Mountains. 1930? p. 18. Cited at Mount Shasta Collection MS1032 Archived 2008-05-13 at the Wayback Machine. Retrieved 2008-04-08.
  14. ^ "Sargents Ridge". Geographic Names Information System. United States Geological Survey. Retrieved 2008-04-19.
  15. ^ "History". College of the Siskiyous. 1989. Archived from the original on 2010-03-08. Retrieved 2010-03-31.
  16. ^ "Map of the United States Of North America. - David Rumsey Historical Map Collection".
  17. ^
  18. ^ "Archived copy". Archived from the original on 2014-10-06. Retrieved 2014-10-04.CS1 maint: Archived copy as title (link)
  19. ^ Scenes of Wonder and Curiosity in California, (1862) by James M. Hutchings
  20. ^ "Snow-Storm on Mount Shasta" (PDF). Retrieved 23 October 2017.
  21. ^ "Sierra Snowfall". Welcome to the Storm King. Mic Mac Publishing. 28 January 2011.
  22. ^ "Mount Shasta". NPS: Nature & Science » National Natural Landmarks. National Park Service. Retrieved 2008-04-07.
  23. ^ "History of Crater Lake". Oregon Explorer. Retrieved 2012-04-21.
  24. ^ "In The Light of Reverence". POV. Public Broadcasting Service.
  25. ^ a b "The Origin of the Lemurian Legend". Folklore of Mount Shasta. College of the Siskiyous. Archived from the original on 2012-09-19.
  26. ^ "Harmonic Convergence". College of the Siskiyous. 1989. Archived from the original on 2010-05-27. Retrieved 2010-03-31.
  27. ^ "Legends: Ascended Masters". College of the Siskiyous. 1989. Archived from the original on 2010-03-30. Retrieved 2010-03-31.
  28. ^ Sigurdsson, Haraldur (2001). Encyclopedia of Volcanoes. Academic Press. ISBN 0-12-643140-X.
  29. ^ "Archived copy". Archived from the original on 2010-08-29. Retrieved 2010-03-31.CS1 maint: Archived copy as title (link)
  30. ^ Program, Volcano Hazards. "USGS: Volcano Hazards Program CalVO Mount Shasta". Retrieved 23 October 2017.
  31. ^ "An Assessment of Volcanic Threat and Monitoring Capabilities in the United States: NVEWS Framework for a National Volcano Early Warning System" (PDF). USGS. 2005.
  32. ^ "Avalanche Gulch". Geographic Names Information System. United States Geological Survey. Retrieved 2008-04-19.
  33. ^ "Avalanche Gulch". Mount Shasta Avalanche Center. Retrieved 2016-02-17.
  34. ^ "Casaval Ridge". SummitPost. Retrieved 2014-02-16.
  35. ^ "Mount Shasta Wilderness Permits and Summit Passes". U.S. Forest Service. Retrieved 2014-01-26.


External links

Black Butte (Siskiyou County, California)

Black Butte is a cluster of overlapping dacite lava domes in a butte,

a parasitic cone of Mount Shasta. It is located directly adjacent to Interstate 5 at milepost 742 between the city of Mount Shasta and Weed, California. The highway crosses a 3,912 ft (1,192 m) pass, Black Butte Summit, at the western base of the lava domes. The lava domes were extruded at the foot of the cone of Shastina following the period of its major eruptions about 9,000–10,000 years ago.A United States Forest Service fire lookout tower was built on the summit in the early 1930s, but destroyed during the Columbus Day Storm of 1962. A new lookout was built in 1963 and operated until 1973. The building was moved by helicopter to a new location in 1975 and only the concrete foundation remains today. A 2.5-mile-long (4.0 km) trail leads to the summit from a trailhead accessible by gravel roads off the Everitt Memorial Highway.

The summit boasts an outstanding view of the southwest side of Shasta and Shastina, and on clear days Mount McLoughlin is easily visible 70 miles (113 km) to the north in Oregon.

California's 1st State Assembly district

California's 1st State Assembly district is one of 80 California State Assembly districts. It is currently represented by Republican Brian Dahle of Bieber.

California's 1st State Senate district

California's 1st State Senate district is one of 40 California State Senate districts. It is vacant, as Republican Ted Gaines of El Dorado Hills resigned to become a member of the California Board of Equalization in January 2019.

California's 1st congressional district

California's 1st congressional district is a congressional district in the U.S. state of California.

Doug LaMalfa, a Republican, has represented the district since January 2013.

Currently, the 1st district encompasses the northeastern part of the state. It consists of:

Butte County

Lassen County

Modoc County

Plumas County

Shasta County

Sierra County

Siskiyou County

Tehama County

most of Nevada County

part of Glenn County

part of Placer CountyPrior to redistricting by the California Citizens Redistricting Commission of 2011, the 1st district encompassed the northern coast of the state. It consisted of Del Norte, Humboldt, Lake, Mendocino, and Napa counties plus portions of Sonoma and Yolo counties. Much of that area is now the 5th district, while the current 1st district comprises much of the territory that had been the 2nd district.

Horse Camp

Horse Camp is a property on Mount Shasta owned by the nonprofit Sierra Club Foundation. It is a 720-acre (2.9 km2) enclave within the Mount Shasta Wilderness of the Shasta-Trinity National Forest in California, United States. It is located at approximately 7,950 feet (2,420 m) elevation at the lower end of Avalanche Gulch, the most popular climbing route on the mountain.

Horse Camp is accessible from the Bunny Flat trailhead by hiking approximately 2 miles (3.2 km) on a developed trail with an elevation gain of about 950 feet (290 m).

The most notable feature of Horse Camp is the Shasta Alpine Lodge, a climber's hut constructed in 1923. Mostly indigenous materials were used for construction, including volcanic rock and Shasta red fir. The lodge can be used for emergency shelter for climbers. It contains a guest register, a library of mountain books, and displays about Mount Shasta.

Other features of Horse Camp include a freshwater spring, low impact campsites, and a solar-powered composting toilet facility.The lodge measures about 450 square feet (42 m2), and was financed primarily by a donor named Hall McAllister at a cost of $6,725. A caretaker is on duty during the summer months. The first caretaker (1923–1934) was Joseph Macatee "Mac" Olberman (1862–1946). With the help of volunteers, Olberman built a 950 yard long flagstone paved path leading uphill from Horse Camp to facilitate access to the Avalanche Gulch climbing route. This structure still exists and is known as Olberman's Causeway.

The camp and the lodge are open year-round, even when no caretaker is on duty.Horse Camp is utilized as a mountaineering base camp for ascents of Mount Shasta by Avalanche Gulch, Casaval Ridge, the West Face Gully and other routes on the south and west side of the mountain.

Jason Sehorn

Jason Heath Sehorn (born April 15, 1971) is a former American football cornerback who played professionally in the National Football League (NFL) for the New York Giants from 1994 to 2002 and St. Louis Rams in 2003. He played college football at the University of Southern California (USC).


KNSQ (88.1 FM) is a radio station licensed to Mount Shasta, California. The station is owned by Southern Oregon University, and is an affiliate of Jefferson Public Radio, airing JPR's "Rhythm & News" service, consisting of news and adult album alternative music.


KSIZ (102.3 FM) is a radio station based in Mount Shasta, California (city of license is Weed, California), owned by Mark & Cynthia Kay Baird's Buffalo Broadcasting, LLC, which also owns KSYC-FM in Yreka. KSIZ broadcasts to the Siskiyou County and Redding markets, and has one of the largest geographical reaches of any FM station Northern California.

The station hit the air once again under the classic rock format in January 2013 with the slogan "Sizzlin' Classic Rock". Despite the collapse of their broadcast tower in early 2017, the station returned to the air in November 2017.


KZRO (100.1 FM) (also known as Z100fm or The Z-Channel) is an oldies/classic hits/classic rock formatted station based in Mount Shasta, California (city of license is Dunsmuir, California). The owner, general manager, program director and lead on-air talent is Dennis Michaels.

The station, with the slogan "We're in it for the music, not the money," features only two commercial breaks per hour 24/7 on weekdays plus 26 hours of weekend syndicated programming, including:

[SATURDAY] 6AM-The Car Show, 7AM-Dick Clark's Rock, Roll and Remember, 11AM-Sammy Hagar's Top Rock Countdown, 12PM-The Acoustic Storm with Jeff Parets, 1PM-The Classic Hit List with MG Kelly and 4PM-The Classics with Steve Downes.

[SUNDAY] 6AM-Hot Rod Radio USA with Wings Kalahan, 8AM-Goddard's Gold with Steve Goddard, 11AM-Off the Record with Uncle Joe Benson, 12PM-Get The Led Out with Carol Miller, 1PM-Little Steven's Underground Garage with Little Steven Van Zandt, 3PM-Floydian Slip with Craig Bailey and 4PM-Blues Deluxe with Dave Johnson.

[WEEKDAYS] 6-10AM: The Dennis Michaels Dog And Pony Show includes music features, goofy stories, daily listener emails and requests, The Old Farmer's Almanac, Dick Clark's Music Calendar, The Prime Comedy Cut and Stupid News. Other daily features include Into Tomorrow with Dave Graveline and A Better Life with Sonjay Gupta.

WESTWOOD ONE RADIO NEWS full five minute reports air weekdays at 8AM, 10AM, 12PM, 2PM and 5PM. One minute updates air at the bottom of every hour, 24/7 (weekend times float with programming).

KZRO has been granted a construction permit by the U.S. Federal Communications Commission (FCC) to upgrade to Class C1 at a new transmitter site. The effective radiated power will increase to 13,500 watts and the antenna height above average terrain will increase to 635 meters. This will cover nearly 225,000 persons in the Redding, California Nielson metro radio market. The station currently covers 195,000 persons in five counties throughout its 24,000-square-mile (62,000 km2) coverage area.

Legends of Mount Shasta

California's Mount Shasta has been the subject of an unusually large number of myths and legends. In particular, it is often said to hide a secret city beneath its peaks. In some stories, the city is no longer inhabited, while in others, it is inhabited by a technologically advanced society of human beings or mythical creatures.

McCloud River

The McCloud River is a 77.1-mile (124.1 km) long river that flows east of and parallel to the upper Sacramento River, in Siskiyou County and Shasta County in northern California in the United States. It drains a scenic mountainous area of the Cascade Range, including part of Mount Shasta. It is a tributary of the Pit River, which in turn flows into the Sacramento River. The three rivers join in Shasta Lake, formed by Shasta Dam north of Redding.

Mount Shasta, California

Mount Shasta (also known as Mount Shasta City) is a city in Siskiyou County, California, at about 3,600 feet (1,100 m) above sea level on the flanks of Mount Shasta, a prominent northern California landmark. The city is less than 9 miles (14 km) southwest of the summit of its namesake volcano. As of the 2010 Census the city had a population of 3,394, down from 3,624 at the 2000 census.

Mount Shasta Ski Park

Mount Shasta Ski Park is a ski resort located in northern California which has summer operations including Scenic Chairlift Rides, Mountain Biking, Disc Golf, just east of Interstate 5 along SR 89 between the city of Mount Shasta and the town of McCloud. The ski area lies about 6 mi (9.7 km) south of the summit of 14,179 ft (4,322 m) Mount Shasta, the second highest volcano in the Cascade Range behind Mt. Rainier. It straddles several small volcanic buttes on the lower southern flanks of the massive stratovolcano, with 3 triple chairlifts running to the top of Coyote Butte- 6,880 ft (2,100 m), Douglas Butte- 6,600 ft (2,000 m), and Marmot Ridge- 6,150 ft (1,870 m). Along with 2 magic carpets, one for tubing and one for learning to ski and snowboard. With a total skiable area of 425 acres and 32 conventional trails. The total skiable vertical is 1,435 ft (437 m), with 20% of the terrain rated beginner, 55% intermediate, and 25% advanced.

Mount Shasta Wilderness

The Mount Shasta Wilderness is a 38,200-acre (155 km2) federally designated wilderness area located 5 miles (8.0 km) east of Mount Shasta City in northern California. The US Congress passed the 1984 California Wilderness Act that set aside the Mount Shasta Wilderness. The US Forest Service is the managing agency as the wilderness is within the Shasta-Trinity National Forest. The area is named for and is dominated by the Mount Shasta volcano which reaches a traditionally quoted height of 14,162 feet (4,317 m) above sea level, but official sources give values ranging from 14,104 feet (4,299 m) from one USGS project, to 14,179 feet (4,322 m) via the NOAA. Mount Shasta is one of only two peaks in the state over 14,000 feet (4,300 m) outside the Sierra Nevada Mountain Range. The other summit is White Mountain Peak in the Great Basin of east-central California.The Wintun Glacier is located on Mount Shasta and is the lowest-elevation glacier in the state, lying at 9,100 feet (2,800 m) elevation and extending to the summit.The smaller volcanic cone of Shastina (12,270 ft) lies one mile (1.6 km) west of Mount Shasta and was formed after the ice-age glaciers melted.

The wilderness protects both pristine forests and areas that were intensively logged and roaded

in the past. Although less than half of the mountain remains roadless, Mount Shasta Wilderness is still the premier destination for a variety of activities from mountaineering, day-hiking, and backpacking to cross-country skiing, snowshoeing and ski mountaineering. It is valued for the many scenic, geologic and recreational attributes including glaciers, lava flows, hot springs, waterfalls and forests of Shasta red fir, sugar pine and other conifers.

Mt. Shasta Brewing Company

Mt. Shasta Brewing Company is a brewery in Weed, California. The company markets some brands as Weed Ales & Lagers. Owners Vaune and Barbara Dillmann began commercial production in 2003. Mount Shasta Brewing Company is licensed to distribute its beers in the states of California, Oregon, and Washington. The brewery has won awards for its beers, for local community involvement and for its marketing success with the slogan "Try Legal Weed".

Shasta River

The Shasta River is a tributary of the Klamath River, approximately 58 miles (93 km) long, in northern California in the United States. It drains the Shasta Valley on the west and north sides of Mount Shasta in the Cascade Range.

The river rises in southern Siskiyou County on the edge of the Shasta-Trinity National Forest, approximately 10 miles (16 km) southwest of Weed. It flows generally northwest through the Shasta Valley, past Weed, through Lake Shastina, and past Montague. It joins the Klamath from the south approximately 8 miles (13 km) north-northeast of Yreka.

The Shasta Valley is dominated by nearby Mount Shasta and underlain with volcanic basalt from eruptions of the mountain in recent geologic time. Pluto's Cave is an example of voids remaining after highly fluid lava drained from underground conduits which were fed by volcanic vents to the east. The Shasta Valley is covered with small hillocks extending from the base of Mt. Shasta north to just beyond the city of Montague, that are the debris from the liquefication of the ancestral Mount Shasta sometime within the past 400,000 years.

Siskiyou County, California

Siskiyou County ( SIS-kew) is a county in the northernmost part of the U.S. state of California. As of the 2010 census, the population was 44,900. Its county seat is Yreka and its highest point is Mount Shasta.Siskiyou County is in the Shasta Cascade region along the Oregon border. Because of its outdoor recreation opportunities and Gold Rush era history, it is an important tourist destination within the state.

Terry Huntingdon

Terry Lynn Huntingdon (born May 8, 1940) is an American beauty queen who won Miss USA 1959. She later became a film and TV actress.

Weed, California

Weed is a city in Siskiyou County, California, United States. As of the 2010 Census, the town had a total population of 2,967, down from 2,979 in 2000. There are several unincorporated communities adjacent to, or just outside, Weed proper, including Edgewood, Carrick, and Lake Shastina. These communities generally have mailing addresses that use Weed or its ZIP code. The total population of this area in 2007 was 6,318. Weed is about 10 miles (16 km) west-northwest of Mount Shasta, a prominent northern California landmark, and the second-tallest volcano in the Cascade Range.

Weed's city motto is "Weed like to welcome you". Weed has frequently been noted on lists of unusual place names.

Glaciers of Mount Shasta
British Columbia
Metro regions
Most populous

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