By Jeffrey E. Turner. Orchestra. Score; String Orchestra. Belwin Beginning String Orchestra. Light Concert; Pop/Rock; Rock. Grade 2.5. 8 pages. Published by Belwin Publishing

By Jeffrey E. Turner. Orchestra. For string w/ vln 3. Part(s); Score; String Orchestra. Belwin Beginning String Orchestra. Light Concert; Pop/Rock; Rock. Grade 2.5. 144 pages. Published by Belwin Publishing

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

We Will Rock You by Queen. By Brian May. Arranged by Paul Lavender. Score and Parts. Essential Elements String Performer. Grade 1-1.5. Softcover. Published by Hal Leonard

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.

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 featured on Glee (Featuring: Have Yourself a Merry Little Christmas / Jingle Bell Rock)). Arranged by Patrick Roszell. Orchestra. Full Orchestra; Score. Pop Intermediate Full Orchestra. Form: Medley. Christmas; Secular; TV; Winter. Grade 3. 16 pages. Published by Alfred Music

By Andy Firth. Arranged by Bob Phillips. By Andy Firth / arr. Bob Phillips. For String Orchestra. String Orchestra. Belwin Beginning String Orchestra. Level: grade 2 Red. Conductor Score & Parts. 39 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).

Orchestra String Orchestra - Grade 2

SKU: FJ.ST6432S

Score Only. Arranged by Kathryn Griesinger. Series; String Orchestra. FJH Developing Strings. Holiday Pops. Score. Duration 2:00. The FJH Music Company Inc #98-ST6432S. Published by The FJH Music Company Inc (FJ.ST6432S).

English.

A rocking celebration of the season! Set in first position with simple rhythms and no slurs, this contemporary arrangement includes the familiar carols Deck the Hall, Hark, the Herald Angels Sing, and Ding, Dong, Merrily On High. Every section of the orchestra is featured and the energetic cello/bass groove is driven by optional drum set and sleigh bells. An exuberant finale for your holiday concert!

About FJH Developing Strings

Sl ightly more advanced than Beginning Strings, this series begins to involve more position work and a slightly more complex rhythmic figures. Rehearsal piano is often provided. Ideal for middle school and smaller high school programs. Grade 2 - 2.5

(Featuring: Paint It, Black / Ruby Tuesday / (I Can't Get No) Satisfaction). Orchestra. Score; SmartMusic; String Orchestra. Pop Concert String Orchestra. Form: Medley. Rock. Grade 3.5. 20 pages. Published by Alfred Music

(Featuring: Paint It, Black / Ruby Tuesday / (I Can't Get No) Satisfaction). Orchestra. Part(s); Score; String Orchestra. Pop Concert String Orchestra. Form: Medley. Rock. Grade 3.5. 136 pages. Published by Alfred Music Publishing

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 4

SKU: KJ.SO227F

Composed by Shirl Jae Atwell. String Tracks. Score. Neil A. Kjos Music Company #SO227F. Published by Neil A. Kjos Music Company (KJ.SO227F).

Catchy blues with a rock beat that will have feet tapping and fingers snapping!

As Performed by Trans- Siberian Orchestra. Composed by Paul O'Neill [Trans- Siberian Orchestra]. Arranged by Bob Phillips. Part(s); Score; String Orchestra. Pop Concert String Orchestra. Christmas; Pop/Rock; Rock; Secular; Winter. 140 pages. Published by Alfred Music

Arranged by Jack Bullock. Orchestra. String Orchestra. Pop Intermediate String Orchestra. Light Concert. Grade 3. Conductor Score and Parts. 156 pages

(As Performed by Trans-Siberian Orchestra). Composed by Paul O'Neill [Trans-Siberian Orchestra]. Arranged by Bob Phillips. Orchestra. Part(s); Score; String Orchestra. Pop Concert String Orchestra. Christmas; Rock; Secular; Winter. Grade 3. 148 pages. Published by Alfred Music

As Performed by Trans-Siberian Orchestra. Composed by Beethoven/Mozart. Arranged by Paul O'Neill [Trans-Siberian Orchestra]. Part(s); Score; SmartMusic; String Orchestra. Pop Concert String Orchestra. Form: Overture. Pop/Rock; Rock; Secular. 140 pages. Published by Alfred Music (AP.44817).

Composed by Doug Spata. Orchestra. Part(s); Score; String Orchestra. Highland String Orchestra. Rock. Grade 1.5. 128 pages. Published by Highland/Etling

(As Arranged for Vitamin String Quartet). Composed by Glen Hansard and Mark�©ta Irglov�¡. Arranged by Jim McMillen for Vitamin String Quartet. Orchestra. Part(s); Score; String Orchestra. Pop Concert String Orchestra. Form: Ballade. Broadway; Movie; Pop/Rock. Grade 3. 124 pages. Published by Alfred Music

Arranged by Jack Bullock. Orchestra. For String Orchestra. String Orchestra. Pop Intermediate String Orchestra. Light Concert. 3 (grade 3). Score. 20 pages

(Featuring: Communication Breakdown / Immigrant Song / Stairway to Heaven / Dazed and Confused / Rock and Roll). Arranged by Bob Phillips. Orchestra. String Orchestra. Pop Concert String Orchestra. Light Concert; Rock. Grade 3.5. Conductor Score and Parts. 132 pages

(As Performed by Trans-Siberian Orchestra). Composed by Paul O'Neill [Trans-Siberian Orchestra]. Arranged by Bob Phillips. Orchestra. Score; String Orchestra. Pop Concert String Orchestra. Christmas; Rock; Secular; Winter. Grade 3. 44 pages. Published by Alfred Music

(As Arranged for Vitamin String Quartet). Composed by Glen Hansard and Mark�©ta Irglov�¡. Arranged by Jim McMillen for Vitamin String Quartet. Orchestra. Score; String Orchestra. Pop Concert String Orchestra. Form: Ballade. Broadway; Movie; Pop/Rock. Grade 3. 12 pages. Published by Alfred Music