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Exaggerated altitude image of the San Andreas Fault on the Carrizo Plain in southern California, 35°07'N, 119°39'W. The picture is a composite of radar data and a Landsat photo.

Aerial photo of the San Andreas Fault in the Carrizo Plain

The San Andreas Fault is a continental transform fault that runs a length of roughly 810 miles (1,300 km) through California in the United States. The fault's motion is right-lateral strike-slip (horizontal motion). It forms the tectonic boundary between the Pacific Plate and the North American Plate.

The fault was first identified in Northern California by UC Berkeley geology professor Andrew Lawson in 1895 and named by him after a small lake which lies in a linear valley formed by the fault just south of San Francisco, the Laguna de San Andreas. After the 1906 San Francisco Earthquake, Lawson also discovered that the San Andreas Fault stretched southward into southern California. Large-scale (hundreds of miles) lateral movement along the fault was first proposed in a 1953 paper by geologists Mason Hill and Thomas Dibblee.^[1]

Segments of the Fault[link]

Located at the Highway 138 and Interstate 15 junction, the Mormon Rocks are visual evidence of the San Andreas fault lying beneath the California surface.

Vasquez Rocks in Agua Dulce, California are evidence of the San Andreas Fault line and part of the 2,650 mile Pacific Crest Trail.

Map of the San Andreas Fault, showing relative motion

The San Andreas Fault can be divided into three segments.

Southern segment[link]

The southern segment (known as the Mojave segment) begins near Bombay Beach, California. Box Canyon, near the Salton Sea, contains upturned strata resulting from that section of the fault.^[2] The fault then runs along the southern base of the San Bernardino Mountains, crosses through the Cajon Pass and continues to run northwest along the northern base of the San Gabriel Mountains. These mountains are a result of movement along the San Andreas Fault and are commonly called the Transverse Range. In Palmdale, a portion of the fault is easily examined as a roadcut for the Antelope Valley Freeway runs directly through it.

After crossing through Frazier Park, the fault begins to bend northward. This area is referred to as the "Big Bend" and is thought to be where the fault locks up in Southern California as the plates try to move past each other. This section of the fault has an earthquake-recurrence interval of roughly 140–160 years. Northwest of Frazier Park, the fault runs through the Carrizo Plain, a long, treeless plain within which much of the fault is plainly visible. The Elkhorn Scarp defines the fault trace along much of its length within the plain.

Research has shown that the Southern segment, which stretches from Parkfield in Monterey County, California all the way down to the Salton Sea, is capable of a Richter scale 8.1 earthquake. An earthquake of that size on the Southern segment (which, at its closest, is 40 miles away from Los Angeles) would kill thousands of people in Los Angeles, San Bernandino, Riverside, and other areas, and cause hundreds of billions of dollars in property and economic damage.^[3]

Central segment[link]

The central segment of the San Andreas fault runs in a northwestern direction from Parkfield to Hollister. While the southern section of the fault and the parts through Parkfield experience earthquakes, the rest of the central section of the fault exhibits a phenomenon called aseismic creep, where the fault slips continuously without causing earthquakes.

Map showing the San Andreas (reds and orange) and major "sister" faults in the San Francisco Bay Area

Northern segment[link]

The northern segment of the fault runs from Hollister, through the Santa Cruz Mountains, epicenter of the 1989 Loma Prieta earthquake, then on up the San Francisco Peninsula, where it was first identified by Professor Lawson in 1895, then offshore at Daly City near Mussel Rock. This is the approximate location of the epicenter of the 1906 San Francisco earthquake. The fault returns onshore at Bolinas Lagoon just north of Stinson Beach in Marin County. It returns underwater through the linear trough of Tomales Bay which separates the Point Reyes Peninsula from the mainland, runs just east of the Bodega Heads through Bodega Bay and back underwater, returning onshore at Fort Ross. (In this region around the San Francisco Bay Area several significant "sister faults" run more-or-less parallel, and each of these can create significantly destructive earthquakes.) From Fort Ross the northern segment continues overland, forming in part a linear valley through which the Gualala River flows. It goes back offshore at Point Arena. After that, it runs underwater along the coast until it nears Cape Mendocino, where it begins to bend to the west, terminating at the Mendocino Triple Junction.

Evolution[link]

Tectonic evolution of the San Andreas Fault

The evolution of the San Andreas dates back to the mid Cenozoic, to about 30 Mya (million years ago).^[4] At this time, a spreading center between the Pacific Plate and the Farallon Plate (which is now mostly subducted, with remnants including the Juan de Fuca Plate, Rivera Plate, Cocos Plate, and the Nazca Plate) was beginning to interact with the subduction zone off the western coast of North America. The relative motion between the Pacific and North American Plates was different from the relative motion between the Farallon and North American Plates, so when the spreading ridge was 'subducted', a new relative motion caused a new style of deformation. This style is chiefly the San Andreas Fault, but also includes a possible driver for the deformation of the Basin and Range, separation of Baja California, and rotation of the Transverse Range.

The San Andreas Fault proper, at least the Southern Segment, has only existed for about 5 million years.^[5] The first known incarnation of the southern part of the fault was Clemens Well-Fenner-San Francisquito fault zone around 22–13 Ma. This system added the San Gabriel Fault as a primary focus of movement between 10–5 Ma. Currently, it is believed that the modern San Andreas will eventually transfer its motion toward a fault within the Eastern California Shear Zone. This complicated evolution, especially along the southern segment, is mostly caused by either the "Big Bend" and/or a difference in the motion vector between the plates and the trend of the fault(s).

Plate movement[link]

All land west of the fault on the Pacific Plate is moving slowly to the northwest while all land east of the fault is moving southwest (relatively southeast as measured at the fault) under the influence of plate tectonics. The rate of slippage averages approximately 33 to 37 millimetres (1.3 to 1.5 in) annually across California.^[6]

The westward component of the motion of the North American Plate creates compressional forces which are expressed as uplift in the Coast Ranges. Likewise, the northwest motion of the Pacific Plate creates significant compressional forces where the North American Plate stands in its way, creating the Transverse Ranges in Southern California, and to a lesser, but still significant, extent the Santa Cruz Mountains, site of the Loma Prieta Earthquake of 1989.

Studies of the relative motions of the Pacific and North American plates have shown that only about 75 percent of the motion can be accounted for in the movements of the San Andreas and its various branch faults. The rest of the motion has been found in an area east of the Sierra Nevada mountains called the Walker Lane or Eastern California Shear Zone. The reason for this is not as yet clear, although several hypotheses have been offered and research is ongoing. One hypothesis which gained some currency following the Landers Earthquake in 1992 is that the plate boundary may be shifting eastward, away from the San Andreas to the Walker Lane.

Assuming the plate boundary does not change as hypothesized, projected motion indicates that the landmass west of the San Andreas Fault, including Los Angeles, will eventually slide past San Francisco, then continue northwestward toward the Aleutian Trench, over a period of perhaps twenty million years.

Scientific research[link]

Radar generated 3-D view of the San Andreas Fault, at Crystal Springs Reservoir near San Mateo, California.^[7]

Research at Parkfield[link]

In central California is the small town of Parkfield, California, which lies along the San Andreas Fault. Seismologists discovered that this section of the fault consistently produces magnitude 6.0 earthquakes about every 22 years. Following earthquakes in 1857, 1881, 1901, 1922, 1934, and 1966, scientists predicted an earthquake to hit Parkfield in 1993. This quake eventually struck in 2004 (see Parkfield earthquake). Because of this frequent activity and prediction, Parkfield has become one of the most popular spots in the world to try to capture and record large earthquakes.

In 2004, work began just north of Parkfield on the San Andreas Fault Observatory at Depth (SAFOD). The goal of SAFOD is to drill a hole nearly 2 miles (3.2 km) into the Earth's crust and into the San Andreas Fault. An array of sensors will be installed to capture and record earthquakes that happen near this area.^[8]

The University of California study on "the next big one"[link]

A study^[9] completed by Yuri Fialko in 2006 has demonstrated that the San Andreas fault has been stressed to a level sufficient for the next "big one," as it is commonly called; that is, an earthquake of magnitude 7.0 or greater. The study also concluded that the risk of a large earthquake may be increasing more rapidly than researchers had previously believed. Fialko also emphasized in his study that, while the San Andreas Fault had experienced massive earthquakes in 1857 at its central section and in 1906 at its northern segment (the 1906 San Francisco earthquake), the southern section of the fault has not seen a similar rupture in at least 300 years.

If such an earthquake were to occur, Fialko's study stated, it would result in substantial damage to Palm Springs and a number of other cities in San Bernardino, Riverside and Imperial counties in California, and Mexicali municipality in Baja California. Such an event would be felt throughout much of Southern California, including densely populated areas of metropolitan Los Angeles, Orange County, San Diego, Ensenada and Tijuana, Baja California, San Luis Rio Colorado in Sonora and Yuma, Arizona.

"The information available suggests that the fault is ready for the next big earthquake but exactly when the triggering will happen and when the earthquake will occur we cannot tell," Fialko said. "It could be tomorrow or it could be 10 years or more from now," he concluded in September 2005.

Cascadia connection[link]

Recent studies of past earthquake traces on both the northern San Andreas Fault and the southern Cascadia subduction zone indicate a correlation in time which may be evidence that quakes on the Cascadia subduction zone may have triggered most of the major quakes on the northern San Andreas during at least the past 3,000 years or so. The evidence also shows the rupture direction going from north to south in each of these time-correlated events. The 1906 San Francisco earthquake seems to have been a major exception to this correlation, however, as it was not preceded by a major Cascadia quake, and the rupture moved mostly from south to north.^[10]

Notable earthquakes[link]

The San Andreas Fault has had some notable earthquakes in historic times:

• 1857 Fort Tejon earthquake: About 217 miles (349 km) were ruptured in central and southern California. Though it is known as the Fort Tejon earthquake, the epicenter is thought to have been located far to the north, just south of Parkfield. Only two deaths were reported. The magnitude was about 7.9.
• 1906 San Francisco earthquake: About 267 miles (430 km) were ruptured in Northern California. The epicenter was near San Francisco. At least 3000 people died in the earthquake and subsequent fires. This time the magnitude was estimated to be 7.8.
• 1989 Loma Prieta earthquake: About 25 miles (40 km) were ruptured (although the rupture did not reach the surface) near Santa Cruz, California, causing 63 deaths and moderate damage in certain vulnerable locations in the San Francisco Bay Area. Moment magnitude this time was about 6.9. The earthquake also postponed game 3 of the 1989 World Series at Candlestick Park. This quake occurred on October 17, 1989, at approximately 5:04 P.M. PDT.
• 2004 Parkfield earthquake: On September 28, 2004, at 10:15 A.M. PDT, a magnitude 6.0 earthquake struck California on the San Andreas Fault.

See also[link]

San Francisco Bay Area portal

• Calaveras Fault
• Central Valley (California)
• Elsinore Fault Zone
• Garlock Fault
• Geologic timeline of Western North America
• Hayward Fault Zone
• Imperial Fault
• Laguna Salada Fault
• North Anatolian Fault
• San Jacinto Fault

References[link]

Further reading[link]

• Collier, Michael (December 1, 1999). A Land in Motion. UC Press. ISBN 0-520-21897-3. 
• Stoffer, Philip W. (2006). Where's the San Andreas fault? A guidebook to tracing the fault on public lands in the San Francisco Bay region. USGS. General Interest Publication 16. 
• The California Earthquake of April 18, 1906: Report of the State Earthquake Investigation Commission, Andrew C. Lawson, chairman, Carnegie Institution of Washington Publication 87, 2 vols. (1908) - Available online at this USGS webpage.
• Lynch, David K. (2006). Field Guide to the San Andreas Fault: See and Touch the World's Most Famous Fault on any one of Twelve Easy Day Trips. Thule Scientific. ISBN 0-9779935-0-7. Full color, GPS coordinates,. 

External links[link]

Wikimedia Commons has media related to: San Andreas Fault

• The Parkfield, California, Earthquake Experiment at the USGS
• San Andreas Fault Zone Observatory at Depth at the International Continental Scientific Drilling Program
• San Andreas Fault Zone at the Southern California Earthquake Data Center
• The San Andreas Fault by Sandra S. Schulz and Robert E. Wallace
• Complete Report for San Andreas fault zone, Peninsula section (Class A) No. 1c from the USGS
• New Scripps Study Reveals San Andreas Fault Set for the 'Big One' at the Scripps Institution of Oceanography
• San Andreas Fault at Wallace Creek — Kite Aerial Photography from the USGS
• "Scientists Search for a Pulse in Skies Above Earthquake Country" at JPL
• The Day California Cracks at Bloomberg Businessweek
• Google Maps Satellite View on Geology.com

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Coordinates: 35°07′N 119°39′W / 35.117°N 119.65°W / 35.117; -119.65

San Andreas is an archaic variation of the Spanish language San Andrés (Saint Andrew, the apostle). It may refer to:

• San Andreas Fault, a geologic fault that runs through California, USA
• San Andreas Lake, a lake near San Francisco, California for which the fault is named
• San Andreas, California, USA, an unincorporated town
• Grand Theft Auto: San Andreas, a video game by Rockstar North for PlayStation 2, Xbox, Microsoft Windows and Macintosh.
  • San Andreas (state), a fictional state in the Grand Theft Auto video game series
• San Andreas (novel), a 1984 novel by Alistair MacLean

See also[link]

• St Andrews (disambiguation)

This disambiguation page lists articles associated with the same title. If an internal link led you here, you may wish to change the link to point directly to the intended article.

This biographical article needs additional citations for verification. Please help by adding reliable sources. Contentious material about living persons that is unsourced or poorly sourced must be removed immediately, especially if potentially libelous or harmful. (July 2009)

Natalie Merchant
In concert in Maryhill, Washington in 2010
Background information
Birth name	Natalie Anne Merchant
Born	(1963-10-26) October 26, 1963 (age 48) Jamestown, New York, USA
Occupations	Musician, Songwriter
Instruments	Vocals, keyboard, piano
Years active	1981–present
Labels	Elektra Records Myth America Records Nonesuch/Elektra Records
Associated acts	10,000 Maniacs Michael Stipe
Website	NatalieMerchant.com

Natalie Anne Merchant (born October 26, 1963) is an American singer-songwriter and musician. She joined the alternative rock band 10,000 Maniacs in 1981 and left it to begin her solo career in 1993.

Early life[link]

Natalie Merchant was born October 26, 1963, in Jamestown, New York, the third of four children of Anthony and Ann Merchant. Her paternal grandfather, who played the accordion, mandolin and guitar, emigrated to the United States from Sicily; his surname was "Mercante" before it was Anglicized.^[1] Her maternal grandfather, a cartoonist, piano tuner and member of a barbershop quartet, was Irish.^[1] Her parents divorced when she was eight years old, and her mother later remarried.^[2]

When Merchant was a child, her mother listened to music (The Beatles, Al Green, Aretha Franklin)^[3] and encouraged her children to study music, but she wouldn't allow TV after Natalie was 12. "I was taken to the symphony a lot because my mother loved classical music. But I was dragged to see Styx when I was 12. We had to drive 100 miles to Buffalo, New York. Someone threw up next to me and people were smoking pot. It was terrifying. I remember Styx had a white piano which rose out of the stage. It was awe-inspiring and inspirational."^[4] "She [her mother] had show tunes, she had the soundtrack from West Side Story and South Pacific. And then eventually... she'd always liked classical music and then she married a jazz musician, so that's the kind of music I was into. I never really had friends who sat around and listened to the stereo and said 'hey, listen to this one', so I'd never even heard of who Bob Dylan was until I was 18."^[5] During 1988–1989, Natalie claimed she still didn't have a TV: "I grew up in a house where no one watched the news on television and no one read the paper. I've been discovering these things as I get older, and the news has affected me more than it ever has before."^[6]

"A suicidal high school dropout", Merchant started working in a health food store at 16.^[2] She considered a career in special education following her taking part in a handicapped children's summer program. But eventually in 1981 she started singing for a band called Still Life, which was to become 10,000 Maniacs.^[2]

Career[link]

10,000 Maniacs[link]

The period featuring Merchant was the most critically and commercially successful for 10,000 Maniacs. She is seen here with Rob Buck and the band during that time.

Merchant was lead singer and primary lyricist for 10,000 Maniacs, joining in its infancy in 1981 while she was a student at Jamestown Community College. The group recorded their album Human Conflict Number Five and performed a corresponding Music video at The Hotel Franklin and at Group W Westinghouse studios (Jamestown, New York) in 1982. Merchant sang lead vocals, and later played the piano as well, for 10,000 Maniacs for seven studio albums. In 1993 she announced that she was leaving the group.^[7]

[edit] Tigerlily (1995)

Merchant has said in interviews that after her split with 10,000 Maniacs she was so eager to begin writing her own material that she went home that very day and composed the song "I May Know the Word", which was originally meant to appear on the soundtrack to the Tom Hanks movie Philadelphia. The song was eventually cut from the soundtrack, but it would go on to appear on Merchant's debut solo album, Tigerlily, which was released on the Elektra label in 1995. Merchant chose to name the album Tigerlily as she felt it captured the feel of the album, which she described as both "fierce" and "delicate".

The third song on the album, "Beloved Wife", was featured as the first song in the trailer for the movie Message in a Bottle.

Seeking creative control, Merchant chose to fund Tigerlily herself, refusing the advance from the record company. She also wanted to work with a core-group of young musicians who she felt would be enthusiastic about the music. The group would consist of guitarist Jennifer Turner, bassist Barrie Maguire, and former-Wallflower and eventual boyfriend to Merchant, Peter Yanowitz, who played drums on the album and who continued to do so with Merchant until their abrupt split in 2000.

Tigerlily was a critical and commercial success, spawning her first top-ten hit in the single "Carnival", and achieving top-40 success with subsequent singles "Wonder" and "Jealousy". The album would go on to sell over 5 million copies, and continues to be Merchant’s most successful album to date. Merchant did extensive touring for the album and made numerous television appearances, including performances on SNL, The Rock and Roll Hall of Fame, and all late-night talk shows. The media's immediate and critical impact on culture and cultural icons was of particular interest to Merchant. In "River", a song from Tigerlily, Merchant defends River Phoenix as she castigates the media for systematically dissecting the child actor after his death. Much of their emphasis was on Phoenix' suspected drug-using lifestyle. In "River," Merchant asks, "Why don't you let him be / Give his mother and father peace." Merchant's anger is later replaced with quiet reflection, asking, "It was such a nightmare raving, 'How could we save him from himself?'"^[8]

[edit] Ophelia (1998–1999)

Three years passed before Merchant would release her second solo effort, Ophelia. While Tigerlily contained a lot of sparse instrumentation, the music on Ophelia featured plenty of lush symphonic arrangements composed and conducted by British composer Gavin Bryars. Merchant treated the recording of Ophelia as a series of workshops, where she would invite various musicians she had met over the years into her home studio to collaborate and record. In the end, 30 different musicians featured on the album, among them Brand New Heavies frontwoman N'Dea Davenport (with whom she duets on the song Break Your Heart), famed trumpet player Chris Botti, and the husband and wife duo, Don and Karen Peris, from the band The Innocence Mission.

While Ophelia is not a concept record in the traditional sense, the album-cycle saw Merchant flexing her creative muscles in surprising ways. The name of the album and the title track are a literary reference to Shakespeare's Ophelia, who in the play Hamlet becomes mad and eventually commits suicide when Hamlet remains non-committal and lost in himself. Merchant's Ophelia describes a series of women throughout time—women who dared question the patriarchal status quo and who were often castigated for doing so—and is a cry for women's rights and for more understanding of female archetypes beyond the scope of the "mother" and the "whore", both of which severely limit women and attempt to turn them into little more than chattel. The portrayal of the women in the song is a tribute to the non-traditional, the "too smart for her own good" type of woman who is often misunderstood by society. As a lyric to the title song cries: "Your common sense, your best defense, was wasted and in vain!" A reflection of women driven mad by social limitations, Natalie's tribute described Ophelia as being at once a "novice carmelite," a "suffragette," a "circus queen," a "demigoddess" and a "mafia courtesan." The album sleeve saw Merchant pictured in colorful and ornate costumes as each of these different characters. As a companion to the album, she also released a film where she portrays each of these different characters, with voice-overs used for the "novice carmelite," the "sweetheart" and the "courtesan" as they are Spanish, German and Italian, respectively.

The first single off the album was a happy and uncharacteristically simple song called "Kind and Generous", which received massive airplay on VH1 and which solidified Merchant's role as a bona fide solo artist. That summer, Sarah McLachlan invited Merchant to co-headline the year's biggest music festival with her, Lilith Fair. The exposure from the tour helped the album reach Platinum status in just under a year, with subsequent singles "Break Your Heart" and "Life Is Sweet" receiving moderate airplay on adult contemporary stations. No video was filmed for the latter, however, with a clip from Merchant's appearance on VH1's Storytellers being used instead. She would also go on to appear on PBS' Sessions at West 54th and VH1's Hard Rock Live before the year's end. In 1998, Merchant also recorded George Gershwin's "But Not for Me" for the Red Hot Organization's compilation album Red Hot + Rhapsody, a tribute to George Gershwin, which raised money for various charities devoted to increasing AIDS awareness and fighting the disease.

The Ophelia tour ended in 1999 with the final few shows being performed and recorded on Broadway. The performance would be released as the album Natalie Merchant: Live in Concert with a companion video of the same name. The performance was notable in that it featured numerous covers including songs by David Bowie, Neil Young, and the Breton-Welsh singer-songwriter Katell Keineg.

[edit] American Folk Music Tour (2000) and Motherland (2001)

In 2000, Merchant embarked on a folk tour in the United States with many shows being supported by alt-country band Wilco.

Merchant's next studio album on the Elektra label was Motherland, released in 2001. Motherland saw Merchant at her most experimental musically. Motherland achieved Gold on the Billboard charts after debuting at No. 30 on the Billboard 200 and No. 13 on the Top Internet Albums of 2001, respectively. Rolling Stone favored this album with 3½ stars, and also noticed a difference in Merchant's voice, which was more deep and gritty than her previous albums. Singles that were released from Motherland were "Just Can't Last", "Build a Levee" and "Tell Yourself".

Merchant embarked on a year and a half world tour to promote Motherland. The first leg of the tour started in Minneapolis, Minnesota on October 17, 2001, trekking all over the United States, and then heading to Europe with some special acoustic shows in Europe. Merchant also participated in the Rock am Ring Festival and Rock im Park in 2002. In the summer of 2002, she was paired with Chris Isaak and both played at stadiums and arenas.

[edit] The House Carpenter's Daughter (2003)

Merchant at the piano in 2005

After her contract with Elektra expired in August 2002, Merchant decided not to sign with them again, or any other major label.^[9] Her next studio album, The House Carpenter's Daughter, was released in September 2003 on her own label, Myth America Records. To date this has been the only release on Myth America.

[edit] Leave Your Sleep (2010)

In October 2009, the official websites of Nonesuch Records and Natalie Merchant announced that she had signed with the label. Leave Your Sleep was released on April 13, 2010 ^[10] and is a compilation of five years of inspiration from a "conversation" with her daughter over the "first 6 years of her life." The album debuted on the Billboard Top 200 at No. 17, Billboard Folk Albums at No. 1, Amazon.com at No.1, and ITunes, No. 3. The album was co-produced by Grammy winning Andres Levin.

Merchant contributed a cover of Buddy Holly's "Learning the Game" to the tribute album Listen to Me: Buddy Holly, released September 6, 2011.

Personal life[link]

Merchant became known for her swirling style of dancing and her simple dress while performing with 10,000 Maniacs

In 2003, Merchant married Daniel de la Calle and had a daughter with him named Lucia. However, in an interview in 2012, she indicated that she is now divorced.^{[11] [12]} She likes gardening and painting.^[13] Some paintings can be seen at her official website.

She has been a vegetarian since 1980,^[14] save for the duration of her pregnancy when she temporarily resumed eating meat.^[11] In 1997, she said:

"The '60s aesthetic has never really appealed to me, the tie-dyed Deadhead running barefoot through the forest on LSD. I don't think that's really me. But I've been a vegetarian for 17 years and I consider myself an environmentalist in as much as I can be, considering the job that I have. I prefer living in the countryside rather than the city; I find it more sane and sustaining for myself..."^[15]

Discography[link]

With 10,000 Maniacs[link]

• Human Conflict Number Five (EP) (1982)
• Secrets of the I Ching (1983)
• The Wishing Chair (1985)
• In My Tribe (1987)
• Blind Man's Zoo (1989)
• Hope Chest: The Fredonia Recordings 1982-1983 (1990)
• Our Time in Eden (1992)
• MTV Unplugged (1993)
• Campfire Songs: The Popular, Obscure and Unknown Recordings (2004)

Solo[link]

• 1995: Tigerlily
• 1998: Ophelia
• 2001: Motherland
• 2003: The House Carpenter's Daughter
• 2005: Retrospective (1990 - 2005)
• 2010: Leave Your Sleep

Filmography[link]

Films[link]

Television[link]

References[link]

External links[link]

Wikimedia Commons has media related to: Natalie Merchant

Wikiquote has a collection of quotations related to: Natalie Merchant

This article's use of external links may not follow Wikipedia's policies or guidelines. Please improve this article by removing excessive or inappropriate external links, and converting useful links where appropriate into footnote references. (May 2012)

• Official website
• Natalie Merchant at the Open Directory Project
• Natalie Merchant at the Ectophile's Guide to Good Music
• Natalie Merchant at the Internet Movie Database
• Natalie Merchant discography at MusicBrainz
• Launch's page on Merchant
• Natalie Merchant interview at musicOMH