By Soon Hee Newbold. For orchestra. FJH Developing Strings. Full set (score and parts). Score only also available: ST6199S. Halloween. Grade 2.5. Score and set of parts. Composed 2009. Published by The FJH Music Company Inc

By Soon Hee Newbold. For orchestra. FJH Developing Strings. Score only. Full set (score and parts) also available: ST6199. Halloween. Grade 2.5. Score. Composed 2009. Published by The FJH Music Company Inc

Composed by Leopold Mozart (1719-1787). Arranged by Jan Farrar-Royce. Masterworks; Performance Music Ensemble; Single Titles; String Orchestra. Belwin Intermediate String Orchestra. Baroque; Christmas; Classical; Masterwork Arrangement; Winter. Part(s); Score. 144 pages. Duration 2:35. Belwin Music #00-45829. Published by Belwin Music (AP.45829).

By The Beatles. Arranged by Larry Moore. Pop Specials for Strings. Softcover. Published by Hal Leonard (HL.4626437).

String Orchestra string orchestra (88555) with optional 3rd violin/viola TC (3) and percussion - Grade 2.5

SKU: KN.36315

Composed by David Bobrowitz. Solo or Ensemble. Voyager String Orchestra. Score and parts. Kendor Music Inc #36315. Published by Kendor Music Inc (KN.36315).

UPC: 822795363159.

It's winter and the sun has already set, but a bright moon allows the whiteness of the snow covered ground to show a clear path. Everyone is excited in anticipation of a fun evening gliding through the snow on a horse driven sleigh. Then we're off, and a catchy melody follows us as we ride through the winter night. Evening Sleigh Ride is a piece that is a perfect addition to your string orchestras Winter Concert. It will leave both performers and audience with an upbeat feeling to the start of their winter break. Set includes optional 3rd Violin/Viola T.C. and percussion parts.

Set includes optional 3rd Violin/Viola T.C. and percussion parts.

String Orchestra String Orchestra - Grade 1.5

SKU: XC.HSO2301FS

Composed by Erica Donahoe. Harmony. Score. Excelcia Music Publishing #HSO2301FS. Published by Excelcia Music Publishing (XC.HSO2301FS).

9 x 12 inches.

This delightful waltz gives your performers and audience the feeling of a lovely ride on an old-time carousel. As you circle around, the carousel horse gently moves up and down to the soothing music. The piece then moves to a melancholy theme as the ride is coming to an end. A stunning new piece for developing string orchestras.

String Orchestra String Orchestra - Grade 1.5

SKU: XC.HSO2301

Composed by Erica Donahoe. Harmony. Set of parts. Excelcia Music Publishing #HSO2301. Published by Excelcia Music Publishing (XC.HSO2301).

9 x 12 inches.

This delightful waltz gives your performers and audience the feeling of a lovely ride on an old-time carousel. As you circle around, the carousel horse gently moves up and down to the soothing music. The piece then moves to a melancholy theme as the ride is coming to an end. A stunning new piece for developing string orchestras.

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

Arranged by Michael Story. Performance Music Ensemble; Single Titles; String Orchestra. Belwin Intermediate String Orchestra. Folk. Part(s); Score. 80 pages. Duration 1:50. Belwin Music #00-45828. Published by Belwin Music (AP.45828).

Orchestra string orchestra - Grade 3

SKU: KJ.SO264F

Composed by Kirt Mosier. String Tracks. Score. Neil A. Kjos Music Company #SO264F. Published by Neil A. Kjos Music Company (KJ.SO264F).

Movement I: Ichabod's Walk Movement II: Hessian's Ride Another exciting work from top-selling composer Kirt Mosier! The two-movement piece is based on The Legend of Sleep Hollow: the first section is an off-beat tango, and the second is a blazing musical chase over a motor rhythm. A thrilling ride!

(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 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

Composed by Wolfgang Amadeus Mozart (1756-1791). Arranged by Richard Meyer. Part(s); Score; String Orchestra. Highland/Etling String Orchestra. Classical; Light Concert; Masterwork Arrangement; Novelty. 128 pages. Published by Highland/Etling

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.

Orchestra String Orchestra - Grade 3.5

SKU: FJ.ST6533

Composed by Katie O'Hara LaBrie. Series; String Orchestra. FJH String Orchestra. Multicultural. Score and Part(s). The FJH Music Company Inc #98-ST6533. Published by The FJH Music Company Inc (FJ.ST6533).

UPC: 241444437384. English.

Journey to the vast countryside of Scotland as you imagine the sound of bagpipes rolling over a heather moor. Memorable melodies abound in every part, portraying the strength and pride of the Scottish Highlanders as well as the beauty of the Highlands. Ideal for expanding range, rhythmic understanding and musical expression.

Orchestra String Orchestra - Grade 3.5

SKU: FJ.ST6533S

Score Only. Composed by Katie O'Hara LaBrie. Series; String Orchestra. FJH String Orchestra. Multicultural. Score. The FJH Music Company Inc #98-ST6533S. Published by The FJH Music Company Inc (FJ.ST6533S).

English.

Journey to the vast countryside of Scotland as you imagine the sound of bagpipes rolling over a heather moor. Memorable melodies abound in every part, portraying the strength and pride of the Scottish Highlanders as well as the beauty of the Highlands. Ideal for expanding range, rhythmic understanding and musical expression.

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

By Rudolf Stephan. For String Orchestra. Orchestra. Level: Grade 2. Music Book. Published by Neil A. Kjos Music Company.

Score and Parts. Composed by Yukiko Nishimura. Southern Music. Classical. Softcover. Southern Music Company #SO121C. Published by Southern Music Company

Composed by Ron DeGrandis. For String Orchestra (Score and Parts). Easy Music For Strings. Grade 1. Published by Hal Leonard

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

Orchestra String Orchestra - Grade 1

SKU: FJ.ST6450

Composed by Chris Thomas. MakeMusic Cloud; String Orchestra. FJH Beginning Strings. Christmas; Holiday Pops. Score and Part(s). Duration 2:00. The FJH Music Company Inc #98-ST6450. Published by The FJH Music Company Inc (FJ.ST6450).

UPC: 241444387894. English.

Imagine a horse-drawn sleigh coasting leisurely through the park with blanket-coated passengers in tow. This music features a bright melody, a sparkly glockenspiel part, and jingle bells to mimic the sound of the sleigh. The melody is passed around to multiple sections in this light-hearted, and very playable addition to any holiday program.

About FJH Beginning Strings

Ap propriate for first year string students. All instruments stay in first position, and optional third violin (viola) parts and piano are included to aid in rehearsal and performance situations. Grade 1 - 1.5

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