By Keith Sharp. Arranged by Keith Sharp. Intermediate String Orchestra. FJH Developing Strings. Score for this title: ST6115S. Extra part for this title: ST6115P. String Orchestra. Level: 2.5. Score and Set of Parts. Published by The FJH Music Company Inc.

By Alan Lee Silva. For string orchestra. Carl Fischer Concert String Orchestra Series. Grade 3 and up. Score and parts. Published by Carl Fischer

Composed by Patrick Roszell. Performance Music Ensemble; Single Titles; String Orchestra. Belwin Beginning String Orchestra. Part(s); Score. 112 pages. Duration 1:50. Belwin Music #00-45824. Published by Belwin Music (AP.45824).

(Viola Feature). By Randy Sabien. Orchestra. For string. Part(s); Score; String Orchestra. Highland String Alternatives. Jazz. Grade 3. 124 pages. Published by Alfred Music Publishing

As Performed by Dave Brubeck. Composed by Paul Desmond [Dave Brubeck]. Arranged by Bob Cerulli. Score; String Orchestra. Pop Concert String Orchestra. Jazz. 8 pages. Published by Alfred Music (AP.45852S).

As Performed by Dave Brubeck. Composed by Paul Desmond [Dave Brubeck]. Arranged by Bob Cerulli. Part(s); Score; String Orchestra. Pop Concert String Orchestra. Jazz. 68 pages. Published by Alfred Music

Arranged by Deborah Baker Monday. For string orchestra (88555) with optional 3rd violin/viola TC (3 copies) and piano. Playground String Orchestra Series. Grade 1.5. Score and set of parts. Duration 2 minutes, 45 seconds. Published by Kendor Music Inc (KN

By Sean O'Loughlin. For string orchestra. Carl Fischer First Plus String Orchestra Series. Grade 1.5-2. Score and parts. Published by Carl Fischer

After the Sinfonia concertante K. 364. By Wolfgang Amadeus Mozart. Edited by Hogwood, Christopher. For Violin 1, Violin 2 , Viola 1, Viola 2 , Violoncello 1, Violoncello 2 /Contrabass. Score (paperbound). Published by Baerenreiter-Ausgaben (German import).

By George Frideric Handel (1685-1759). Arranged by Douglas E. Wagner. Orchestra. Masterworks; Part(s); Score; String Orchestra. Belwin Beginning String Orchestra. Form: Transcription. Baroque; Masterwork Arrangement. Grade 1.5. 72 pages. Published by Belwin Publishing

Composed by Chris M. Bernotas. Orchestra. Score; String Orchestra. Sound Innovations for Strings. Grade 2.5. 12 pages. Published by Alfred Music

Orchestra String Orchestra - Grade 1.5-2

SKU: CF.FAS38

Composed by Franz Xaver Gruber. Arranged by Roy Phillippe. Carl Fischer First Plus String Orchestra Series. Sacred, Christmas. Score and Parts. With Standard notation. 8 pages. Carl Fischer Music #FAS38. Published by Carl Fischer Music (CF.FAS38).

ISBN 9780825861130. UPC: 798408061135. 8.5 X 11 inches. Key: D major.

One of the most beloved of all Christmas carols is presented in an easy, yet beautiful arrangement by Roy Phillippe. Every sections is given a chance to play the melody in the very playable setting. The optional piano part adds interest and colorful lines to this already very special piece.
I am of the opinion that a piece of music is not judged by how difficult it is to play, but by how good it sounds. While my arrangement of Silent Night is written for beginning string players, I have tried to keep it interesting for all players. It should be played warmly with expression to create a full sound.The piece begins with an introduction based on the three-note Silent Night motive. The main melody is introduced in m. 5 by the first Violins, and is harmonized by the second Violins and Violas. The Cellos reiterate the motive in mm. 6,8,10 and 11. Beginning at m.12 the motive alternates between the Violin II and the Cellos. The melody is played tutti until the key change at m.29, at which point when the Cellos and Basses take the melody with light accompaniment in the Violins and Violas. The final statement of the melody is played by the first violins beginning in m. 37. The Silent Night motive from the beginning alternates between Violin II and the Cellos to the end.

By Karen Kyriakou. Orchestra. Part(s); Score; String Orchestra. Belwin Concert String Orchestra. Light Concert. Grade 3. 124 pages. Published by Alfred Music Publishing

Composed by Peter Wilhousky. Arranged by Bill Calhoun. For string orchestra. Score and parts. Duration 2 minutes, 4 seconds. Published by Carl Fischer

By Richard Meyer. Orchestra. Score; String Orchestra. Highland String Orchestra. Grade 4. 24 pages. Published by Alfred Music Publishing

By Richard Meyer. Orchestra. For string. Part(s); Score; String Orchestra. Highland String Orchestra. Grade 4. 124 pages. Published by Alfred Music Publishing

By Piotr [Peter] Ilyich Tchaikovsky. Arranged by Steven H. Brook. Orchestra. Part(s); Score; String Orchestra. Belwin Concert String Orchestra. Masterwork Arrangement; Romantic. Grade 4. 124 pages. Published by Belwin Publishing

Arranged by Steven L. Rosenhaus. For string orchestra. Grade 2+. Score and set of parts. Duration 2 minutes, 40 seconds. Published by Grand Mesa Music

By Piotr [Peter] Ilyich Tchaikovsky. Arranged by Steven H. Brook. Orchestra. Score; String Orchestra. Belwin Concert String Orchestra. Masterwork Arrangement; Romantic. Grade 4. 24 pages. Published by Belwin Publishing

By Soon Hee Newbold. For string orchestra. Orchestra. FJH Beginning Strings. Grade 1. Score and parts. Duration 1 minute, 45 seconds. Published by The FJH Music Company Inc

Composed by Brian Balmages. For string orchestra. FJH Beginning Strings. Grade 1.5. Score and parts. Duration 1 minute, 45 seconds. Published by The FJH Music Company Inc

Composed by Soon Hee Newbold. For string orchestra. FJH Developing Strings. Grade 2. Score and parts. Duration 2 minutes, 30 seconds. Published by The FJH Music Company Inc

By Doug Spata. Orchestra. Score; SmartMusic; String Orchestra. Highland String Orchestra. Form: Overture. Grade 2.5. 20 pages. Published by Alfred Music

By Doug Spata. Orchestra. Part(s); Score; SmartMusic; String Orchestra. Highland String Orchestra. Form: Overture. Grade 2.5. 124 pages. Published by Alfred Music

By Pietro Antonio Locatelli (1695-1764). Arranged by Tim McCarrick. Orchestra. For string w/ vln3. Masterworks; Part(s); Score; String Orchestra. Belwin Intermediate String Orchestra. Baroque; Masterwork Arrangement. Grade 3. 144 pages. Published by Alfred Music Publishing

Composed by Gary Edwards. For string orchestra. Pathways Series. Grade 3. Full set. Duration 3 minutes, 45 seconds. Published by Imagine Music

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.

By Michael Hopkins. Orchestra. String Orchestra. Belwin Intermediate String Orchestra. Grade 3. Conductor Score and Parts. 144 pages