Arranged by Michael Story and Michael Story. Orchestra. Part(s); Score; String Orchestra. Orchestra Expressions Book 1. Christmas; Novelty; Rock; Secular; Winter. Grade 1. 80 pages. Published by Alfred Music Publishing

Arranged by Bob Phillips. Traditional. For String Orchestra. String Orchestra. String Alternatives. Folk Song. Level: 3 (grade 3). Conductor Score and Parts. 144 pages. Published by Alfred Publishing.

Arranged by Bob Phillips. Traditional. For String Orchestra. String Orchestra. String Alternatives. Folk Song. Level: 3 (grade 3). Conductor Score. 16 pages. Published by Alfred Publishing.

As recorded by DNCE. Composed by Justin Tranter, Robin Fredriksson, Mattias Larsson, and Joe Jonas [DNCE]. Arranged by Victor Lopez. Score; String Orchestra. Pop Intermediate String Orchestra. Pop/Rock. 12 pages. Published by Alfred Music (AP.45833S).

As Recorded by DNCE. Composed by Justin Tranter, Robin Fredriksson, Mattias Larsson, and Joe Jonas [DNCE]. Arranged by Victor Lopez. Part(s); Score; String Orchestra. Pop Intermediate String Orchestra. Pop; Pop/Rock. 152 pages. Published by Alfred Music (AP.45833).

Composed by John O'Neill. For string orchestra. Score and parts. Duration 7 minutes. Published by Imagine Music

By Various. Arranged by Robert Frost. For string orchestra. String Collection. Christmas. Grade 1-2. Full score. Published by Kendor Music Inc

As Performed by Bruno Mars. Composed by Bruno Mars, Jeff Bhasker, Philip Lawrence, Devon Gallaspy, Mark Ronson, Nicholaus Williams, Lonnie Simmons, Ronnie Wilson, Charles Wilson, Rudolph Taylor, and Robert Wilson. Arranged by Michael Story. Part(s); Score; String Orchestra. Pop Intermediate String Orchestra. Funk; Pop/Rock. 78 pages. Published by Alfred Music (AP.44859).

By Matt Turner. Orchestra. Part(s); Score; String Orchestra. Highland String Alternatives. Light Concert; Rock. Grade 2.5. 130 pages. Published by Alfred Music Publishing

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.

Recorded by American Authors. Composed by Zachary Barnett, James Shelley, Matthew Sanchez, David Rublin, Aaron Accetta, Jonnie Davis, and Michael Goodman [American Authors]. Arranged by Victor Lopez. Part(s); Score; String Orchestra. Pop Intermediate String Orchestra. Pop/Rock. 152 pages. Published by Alfred Music

(As performed by Trans-Siberian Orchestra). Composed by Paul O'Neill [Trans-Siberian Orchestra]. Arranged by Bob Phillips. Orchestra. Score; SmartMusic; String Orchestra. Pop Concert String Orchestra. Light Concert; Rock. Grade 3.5. 24 pages. Published by Alfred Music

(As performed by Trans-Siberian Orchestra). Composed by Paul O'Neill [Trans-Siberian Orchestra]. Arranged by Bob Phillips. Orchestra. Part(s); Score; SmartMusic; String Orchestra. Pop Concert String Orchestra. Light Concert; Rock. Grade 3.5. 144 pages. Published by Alfred Music

As Performed by Trans-Siberian Orchestra. By Paul O'Neill [Trans-Siberian Orchestra]. By Paul O'neill. Arranged by Bob Phillips. Full Orchestra; Performance Music Ensemble; Single Titles. Pop Concert Full Orchestra. Christmas; Pop/Rock; Rock; Winter. Part(s); Score. 192 pages. Duration 2:30. Alfred Music #00-44821. Published by Alfred Music (AP.44821).

As recorded by Bruno Mars. Composed by Christopher Brown, Jeremy Reeves, Jonathan Yip, Bruno Mars, Philip Lawrence, James Fauntleroy, Ray Romulus, and Ray McCollough II. Arranged by Michael Story. Full Orchestra; Part(s); Score. Pop Intermediate String/Full Orchestra. Light Concert; Pop; Pop/Rock; Radio; Rock. 142 pages. Published by Alfred Music

(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 Trans-Siberian Orchestra). Arranged by Paul O'Neill [Trans-Siberian Orchestra], setting by Bob Phillips. Orchestra. Part(s); Score; String Orchestra. Pop Concert String Orchestra. Form: March. Christmas; Rock; Sacred; Winter. Grade 3. 148 pages. Published by Alfred Music

By Susan H. Day. Orchestra. String Orchestra. Highland String Orchestra. Grade 2. Conductor Score. 12 pages. Published by Alfred Music Publishing

By Michael Story and Michael Story. Orchestra. String Orchestra. Orchestra Expressions Book 1. Grade 1.5. Conductor Score and Parts. 66 pages. Published by Alfred Music Publishing

By Mykola Leontovich. Arranged by Sandra Dackow. Orchestra. For String Orchestra. String Orchestra. Orchestra Expressions Book 1. Christmas; Winter. 1 (grade 1). Score. 8 pages

As Performed by Bruno Mars. Composed by Bruno Mars, Jeff Bhasker, Philip Lawrence, Devon Gallaspy, Mark Ronson, Nicholaus Williams, Lonnie Simmons, Ronnie Wilson, Charles Wilson, Rudolph Taylor, and Robert Wilson. Arranged by Dean Marshall and Bob Phillips. Part(s); Score; String Orchestra. Pop Concert String Orchestra. Funk; Pop/Rock. 128 pages. Published by Alfred Music (AP.44860).

As Performed by Bruno Mars. Composed by Bruno Mars, Jeff Bhasker, Philip Lawrence, Devon Gallaspy, Mark Ronson, Nicholaus Williams, Lonnie Simmons, Ronnie Wilson, Charles Wilson, Rudolph Taylor, and Robert Wilson. Arranged by Dean Marshall and Bob Phillips. Score; String Orchestra. Pop Concert String Orchestra. Funk; Pop/Rock. 20 pages. Published by Alfred Music (AP.44860S).

By Alan Silvestri, Glen Ballard. Arranged by Bob Cerulli. Words and music by Glen Ballard and Alan Silvestri / arr. Bob Cerulli. For String Orchestra. String Orchestra. Pop Beginning String Orchestra. Movie. Level: 1.5 (grade 1.5). Conductor Score & Parts. 132 pages. Duration 2:04. Published by Alfred Publishing.

By Jason Hayes. Arranged by Victor LÌ_pez. Orchestra. Score; String Orchestra. Pop Beginning String Orchestra. Novelty; Pop; Rock; Video Game. Grade 1.5. 8 pages. Published by Alfred Music Publishing

By Jason Hayes. Arranged by Victor LÌ_pez. Orchestra. For string w/ vln3, pno acc, drumset. Part(s); Score; String Orchestra. Pop Beginning String Orchestra. Novelty; Pop; Rock; Video Game. Grade 1.5. 78 pages. Published by Alfred Music Publishing

By Billy Joe and Green Day. Arranged by Bob Phillips. For String Orchestra. String Orchestra. Pop Intermediate String Orchestra. 0. Rock. Level: grade 2.5. Conductor Score and Parts. 73 pages. Published by Alfred Publishing.