Arranged by Susan H. Day. For string orchestra. Grade 1. Score and set of parts. Duration 3 minutes, 5 seconds. Published by Grand Mesa 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.

Composed by Bob Lipton. Edited by J. Cameron Law. For string orchestra. Grade 2+. Score and set of parts. Duration 2 minutes, 30 seconds. Published by Grand Mesa Music

By Samuel Augustus Ward. Arranged by Carmen Dragon, adapted by Douglas E. Wagner. Orchestra. Part(s); Score; String Orchestra. Pop Beginning String Orchestra. 4th of July; Patriotic; Summer. Grade 2.5. 72 pages. Published by Alfred Music Publishing

By Samuel Augustus Ward. Arranged by Carmen Dragon, adapted by Douglas E. Wagner. Orchestra. Score; String Orchestra. Pop Beginning String Orchestra. 4th of July; Patriotic; Summer. Grade 2.5. 8 pages. Published by Alfred Music Publishing

By David Bobrowitz. Edited by J. Cameron Law. For string orchestra. Grade 2. Score and set of parts. Duration 2 minutes. Published by Grand Mesa Music

Composed by David Bobrowitz. Edited by J. Cameron Law. For string orchestra. Grade 3+. Score and set of parts. Duration 4 minutes, 30 seconds. Published by Grand Mesa Music

By Stan Getz and Beaux Arts String Ensemble. By Eddie Sauter. Edited by Rob Duboff, Jeffrey Sultanof, Alex Chilowicz, and Andrew Homzy. Arranged by Eddie Sauter. For string ensemble (score and parts) (Soloist (parts in concert, B-flat, and E-flat), Violin I (8 parts), Violin II (8 parts), Viola (5 Parts), Cello (5 Parts) , Double Bass (3 Parts), Harp, Piano/Celeste, Percussion (Snare Drum, Marimba, Tambourine)). Advanced. Score and parts. Published by Jazz Lines Publications

Composed by Ted Allen. Edited by J. Cameron Law. For string orchestra. Grade 3 . Score and parts. Duration 2 minutes, 51 seconds. Published by Grand Mesa Music

Composed by David Bobrowitz. Edited by J. Cameron Law. For string orchestra. Grade 3. Score and set of parts. Duration 4 minutes. Published by Grand Mesa Music

Composed by Bob Lipton. Edited by J. Cameron Law. For string orchestra. Grade 3. Score and set of parts. Duration 3 minutes, 45 seconds. Published by Grand Mesa Music

Edited by J. Cameron Law. Arranged by Randall D. Strandridge. For string orchestra. Grade 2+. Score and set of parts. Duration 2 minutes, 30 seconds. Published by Grand Mesa Music

Composed by David Bobrowitz. Edited by J. Cameron Law. For string orchestra. Grade 1+. Score and set of parts. Duration 2 minutes, 20 seconds. Published by Grand Mesa Music

Arranged by J. Cameron Law. For string orchestra. Grade 1. Score and set of parts. Duration 1 minute, 40 seconds. Published by Grand Mesa Music

(Recorded by Meghan Trainor). Composed by Meghan Trainor and Kevin Kadish. Arranged by Victor López. Orchestra. Part(s); Score; String Orchestra. Pop Intermediate String Orchestra. Pop. Grade 2. 78 pages. Published by Alfred Music

(Recorded by Meghan Trainor). Composed by Meghan Trainor and Kevin Kadish. Arranged by Victor López. Orchestra. Score; String Orchestra. Pop Intermediate String Orchestra. Pop. Grade 2. 8 pages. Published by Alfred Music

By Richard Meyer. By Richard Meyer. For String Orchestra. String Orchestra. Highland String Orchestra. Conductor Score & Parts. Published by Alfred Publishing.
Level: 2.5 (grade 2.5).

By Bedrich Smetana (1824-1884). Arranged by Robert Frost. Cadet String Orchestra. Grade 2 -3. Score and Set of Parts

Composed by David Bobrowitz. Edited by J. Cameron Law. For string orchestra. Grade 2. Score and set of parts. Duration 2 minutes, 20 seconds. Published by Grand Mesa Music

Orchestra String Orchestra - Grade 2-2.5

SKU: CF.YAS19

Composed by Alan Lee Silva. Carl Fischer Young String Orchestra Series. Classical. Score and Parts. With Standard notation. 12 pages. Carl Fischer Music #YAS19. Published by Carl Fischer Music (CF.YAS19).

ISBN 9780825854859. UPC: 798408054854. 8.5 X 11 inches. Key: D major.

Summer Dance is a melodic, up-tempo piece with plenty of musical and technical challenges for every player. Musicians should strive to play it with an energetic yet legato feel. A spirited introduction features an opening melody in the violins and active repeated-note pedal patters in the violas and low strings. An AABA form begins at m.5 and the orchestration is immediately pared down to feature violin I and cello. It then builds again in density to the B section, where a quick dynamic drop allows a question-and-answer melody between the two parts to sing out. In m. 29, the melody is harmonized and a countermelody in violin I introduced. The violins take the melody soaring in octaves in m. 33, as the piece again builds to the B section and suddenly quiets. Measure 55 then provides more question-and-answer interplay, this time for viola and cello, while violin continues with its newly harmonized melody. Summer Dance finishes with a soft recurrence of the opening figure and a build toward a powerful divisi voicing on beat 3 of m. 63, right before the final chord.
Summer Dance is a melodic, up-tempo piece with plenty of musical and technical challenges for every player. Musicians should strive to play it with an energetic yetA legato feel. A spirited introduction features an opening melody in the violins and active repeated-note pedal patters in the violas and low strings. An AABA form begins at m.5 and the orchestration is immediately pared down to feature violin I and cello. It then builds again in density to the B section, where a quick dynamic drop allows a question-and-answer melody between the two parts to sing out. In m. 29, the melody is harmonized and a countermelody in violin I introduced. The violins take the melody soaring in octaves in m. 33, as the piece again builds to the B section and suddenly quiets. Measure 55 then provides more question-and-answer interplay, this time for viola and cello, while violin continues with its newly harmonized melody. Summer Dance finishes with a soft recurrence of the opening figure and a build toward a powerfulA divisi voicing on beat 3 of m. 63, right before the final chord.
Summer Dance is a melodic, up-tempo piece with plenty of musical and technical challenges for every player. Musicians should strive to play it with an energetic yet legato feel. A spirited introduction features an opening melody in the violins and active repeated-note pedal patters in the violas and low strings. An AABA form begins at m.5 and the orchestration is immediately pared down to feature violin I and cello. It then builds again in density to the B section, where a quick dynamic drop allows a question-and-answer melody between the two parts to sing out. In m. 29, the melody is harmonized and a countermelody in violin I introduced. The violins take the melody soaring in octaves in m. 33, as the piece again builds to the B section and suddenly quiets. Measure 55 then provides more question-and-answer interplay, this time for viola and cello, while violin continues with its newly harmonized melody. Summer Dance finishes with a soft recurrence of the opening figure and a build toward a powerful divisi voicing on beat 3 of m. 63, right before the final chord.
Summer Dance is a melodic, up-tempo piece with plenty of musical and technical challenges for every player. Musicians should strive to play it with an energetic yet legato feel.A spirited introduction features an opening melody in the violins and active repeated-note pedal patters in the violas and low strings. An AABA form begins at m.5 and the orchestration is immediately pared down to feature violin I and cello. It then builds again in density to the B section, where a quick dynamic drop allows a question-and-answer melody between the two parts to sing out.In m. 29, the melody is harmonized and a countermelody in violin I introduced. The violins take the melody soaring in octaves in m. 33, as the piece again builds to the B section and suddenly quiets. Measure 55 then provides more question-and-answer interplay, this time for viola and cello, while violin continues with its newly harmonized melody. Summer Dance finishes with a soft recurrence of the opening figure and a build toward a powerful divisi voicing on beat 3 of m. 63, right before the final chord.

About Carl Fischer Young String Orchestra Series

Thi s series of Grade 2/Grade 2.5 pieces is designed for second and third year ensembles. The pieces in this series are characterized by:
--Occasionally extending to third position
--Keys carefully considered for appropriate difficulty
--Addition of separate 2nd violin and viola parts
--Viola T.C. part included
--Increase in independence of parts over beginning levels

Composed by George Frideric Handel (1685-1759). Edited by J. Cameron Law. Arranged by Ronald Wilcott. For string orchestra. Grade 2. Score and set of parts. Duration 2 minutes, 10 seconds. Published by Grand Mesa Music

Arranged by J. Cameron Law. Score and parts. Duration 1 minute, 32 seconds. Published by Grand Mesa Music (GC.GMMOR116).

Composed by Darren Mitchell. Edited by J. Cameron Law. For string orchestra. Grade 4. Score and parts. Duration 3 minutes, 44 seconds. Published by Grand Mesa Music

By Andrew Lloyd Webber. Arranged by Mark Brymer, Calvin Custer. Pop Special String. Size 9x12 inches. Published by Hal Leonard.

(Featuring: America / America the Beautiful / The Star Spangled Banner). Arranged by Jerry Brubaker. Orchestra. Part(s); Score; String Orchestra. Belwin Intermediate String Orchestra. Form: Medley. 4th of July; Fall; Graduation; Light Concert; Patriotic; Summer; Thanksgiving. Grade 2.5. 104 pages. Published by Belwin Publishing

((Awesome Remixxx!!!)). Composed by Shawn Patterson (1965-). Arranged by Ralph Ford. Orchestra. Score; String Orchestra. Pop Intermediate String Orchestra. Movie. Grade 2.5. 12 pages. Published by Alfred Music

(As performed by Video Games Live� (www.videogameslive.com)) . By Tommy Tallarico, Michael Plowman, Emmanuel Fratianni, and Laurie Robinson [Video Games Live]. Arranged by Bob Phillips. Orchestra. String Orchestra. Pop Intermediate String Orchestra. Light Concert; Video Game. Grade 2.5. Conductor Score. 12 pages. Published by Alfred Music Publishing