By Alan Lee Silva. For Full Score. Carl Fischer First Plus String Orchestra Series. Grade 1.5-2. Full score (large). Published by Carl Fischer

(String Orchestra). By John Tavener (1944-). For Orchestra (Score and Parts). Songbooks and Methods. Music Sales America. Chester Music #CH7115901. Published by Chester Music

(String Orchestra). By Eric Whitacre (1970-). For String Orchestra (Score). Music Sales America. Softcover. 4 pages. Chester Music #CH79409. Published by Chester Music

String Orchestra - Intermediate

SKU: HL.14005636

Composed by Charles Wilfred Orr. Music Sales America. Classical. Sheet Music, Score and Parts. With Text language: English. Chester Music #CH61640. Published by Chester Music (HL.14005636).

UPC: 884088811549. 8.5x11.0x0.09 inches.

Written for string orchestra.

From Shakespeare's England. Composed by Nicholas Hare. Arranged by Nicholas Hare. Playstrings. Classical. Book Only. Composed 2005. 16 pages. Chester Music #MUSCH55340. Published by Chester Music

Composed by Witold Lutoslawski (1913-1994). Music Sales America. Post-1900. Book Only. Composed 1999. 38 pages. Chester Music #MUSCH60924. Published by Chester Music

By John Tavener. For Cello, String Orchestra, Orchestra. 20th Century. Sheet Music, Score. Text language: English. Published by Chester Music.

By Witold Lutoslawski. For String Orchestra. 20th Century. Sheet Music. 48 pages. Published by Chester Music.

By Katy Perry, Mikkel Eriksen, Tor Erik Hermansen, Sandy Wilhelm, and Ester Dean. Arranged by Todd Parrish. Orchestra. Score; String Orchestra. Pop Beginning String Orchestra. Light Concert; Pop/Rock. Grade 2.5. 16 pages. Published by Alfred Music Publishing

By Katy Perry, Mikkel Eriksen, Tor Erik Hermansen, Sandy Wilhelm, and Ester Dean. Arranged by Todd Parrish. Orchestra. Part(s); Score; String Orchestra. Pop Beginning String Orchestra. Light Concert; Pop/Rock. Grade 2.5. 148 pages. Published by Alfred Music Publishing

By Doris Gazda. For string orchestra. Carl Fischer Primer String Orchestra Series. Grade 0.5. Score and parts. Published by Carl Fischer

Orchestra String Orchestra - Grade 3

SKU: CF.CAS7

Composed by Doris Gazda. Edited by Amy Rosen. FS-SWs. Carl Fischer Concert String Orchestra Series. Score and Parts. With Standard notation. 20+24+24+6+15+15+15 pages. Carl Fischer Music #CAS7. Published by Carl Fischer Music (CF.CAS7).

ISBN 9780825847578. UPC: 798408047573. 8.5 X 11 inches. Key: D major.

When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.
When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody.A Red Rock RagA is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.
When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody.A Red Rock RagA is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.
When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.
When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista. The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color. Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.
When you have the good fortune to visit Red Rock country in the southwestern United States, you will all at once feel that majesty and beauty in the towering red landscape. You can trek, bike, paddle, ride horseback or drive through the canyons, past the strangely shaped rocks and over the enormous boulders. Each time you turn a corner you will be dazzled by yet another magnificent vista.The Red Rock areas in Utah, Nevada, Arizona and New Mexico formed millions of years ago when that part of North America was primarily under water. The water left behind the shells and skeletons of sea creatures that gradually turned into limestone and similar rocks. Beginning 225 million years ago, the earth's crust began to move and the seabed slowly rose. Streams entering the shallow water deposited mud and sand that turned into shale and marine sandstone. As the land continued to rise and dry out, some of the rocks oxidized (combined with oxygen) and turned red in color. Subsequently the area was covered with sands that eventually compressed into what is called Aztec sandstone. Sometimes, when iron was concentrated in the rock, the sandstone turned a bright red color.Following the introduction, the music in Red Rock Rag takes on a typical ragtime melody and rhythm. It then transitions by changing key, time signature and the structure into a swing waltz. At m. 60, it moves into a combined time signature of one measure of 3/4 time and two measures of 2/4 time with an occasional lick in the bass line. Finally, it moves back into the swing-waltz style and finishes with the original ragtime melody. Red Rock Rag is challenging stylistically and rhythmically. It would be appropriate to study both the ragtime and swing styles while working on it.

Composed by Wolfgang Amadeus Mozart (1756-1791). Set (Score & Parts). Composed 2009. Editio Musica Budapest #EMBZ14657. Published by Editio Musica Budapest

Composed by Greg Bartholomew. For "trumpet, timpani & string orchestra". Pathways Series. Level 4. Score and set of parts. Duration "3 minutes, 40 seconds". Published by Imagine Music

Composed by Greg Bartholomew. For "trumpet, percussion & string orchestra". Pathways Series. Level 4. Score and set of parts. Duration "3 minutes, 40 seconds". Published by Imagine Music

Composed by Greg Bartholomew. For "trumpet, marimba & string orchestra". Pathways Series. Level 4. Score and set of parts. Published by Imagine Music

By Bob Mathews. (String Orchestra). orchestra. Level: Grade 3. Music book. Published by Neil A. Kjos Music Company.

By Susan H. Day. Orchestra. Part(s); Score; SmartMusic; String Orchestra. Highland String Orchestra. Grade 2.5. 62 pages. Published by Alfred Music

By Richard Meyer. Orchestra. Part(s); Score; SmartMusic; String Orchestra. Highland String Orchestra. Grade 2. 124 pages. Published by Alfred Music

Composed by David Bobrowitz. For string orchestra. Folk. Grade 3. Score and set of parts. Duration 4:18. Published by Wingert-Jones Publications

By Bob Mathews. (String Orchestra). orchestra. Level: Grade 3. Music book. Published by Neil A. Kjos Music Company.

Composed by David Bobrowitz. For string orchestra. Folk. Grade 3. Conductor score. Duration 4:18. Published by Wingert-Jones Publications

Orchestra String Orchestra - Grade 3

SKU: FJ.ST6500S

Score Only. Composed by Neridah Oostenbroek. Series; String Orchestra. FJH String Orchestra. Multicultural. Score. The FJH Music Company Inc #98-ST6500S. Published by The FJH Music Company Inc (FJ.ST6500S).

English.

Get ready to have some fun with this energetic western-style romp! Showcasing a melody that weaves its way through every section, the piece also makes use of open string drones and syncopated rhythms, bringing the country-style flair to life. Outstanding and infectious!

About FJH String Orchestra

More emphasis on bow technique and independence of lines. For the accomplished middle, high school, college, or professional group. Grade 3 and up

By Alan Lee Silva. For String Orchestra. Carl Fischer First Plus String Orchestra Series. Grade 1.5-2. Score and parts

Orchestra string orchestra - Grade 1.5

SKU: KJ.SO119F

Composed by Richard Bell. Score. Neil A. Kjos Music Company #SO119F. Published by Neil A. Kjos Music Company (KJ.SO119F).

Four movements entitled Western Swing, Southern Lullaby, Cowboy Waltz, & Shaker Dances make up this vibrant symphony for string orchestras. Great melodies combined with rhythmic energy will motivate students and will be a favorite at concert time.

By Frueh. For standard string orchestra (88555) with opt. piano accompaniment. Playground String Orchestra Series. Grade 1. Score and set of parts. Duration 2 minutes, 30 seconds. Published by Kendor Music Inc

Orchestra String Orchestra - Grade 3

SKU: FJ.ST6500

Composed by Neridah Oostenbroek. Series; String Orchestra. FJH String Orchestra. Form: Dance. Fiddle; Multicultural. Score and Part(s). The FJH Music Company Inc #98-ST6500. Published by The FJH Music Company Inc (FJ.ST6500).

UPC: 241444414682. English.

Get ready to have some fun with this energetic western-style romp! Showcasing a melody that weaves its way through every section, the piece also makes use of open string drones and syncopated rhythms, bringing the country-style flair to life. Outstanding and infectious!

About FJH String Orchestra

More emphasis on bow technique and independence of lines. For the accomplished middle, high school, college, or professional group. Grade 3 and up