(From The Nutcracker). By Peter Ilyich Tchaikovsky (1840-1893). Arranged by John Caponegro. For string orchestra (88555) with optional 3rd violin/viola TC (1) and piano. Playground String Orchestra Series. Grade 1.5. Score and set of parts. Duration 2 minutes. Published by Kendor Music Inc

By Piotr Ilyich Tchaikovsky [Peter Ilyich Tchaikovsky]. Arranged by Andrew H. Dabczynski. Orchestra. Masterworks; Part(s); Score; String Orchestra. Highland String Explorer. Form: Transcription; Waltz. Masterwork Arrangement; Romantic. Grade 2. 72 pages.

String Orchestra Orchestra - Grade 1.5

SKU: XC.HSO2002

Composed by Sean O'Loughlin. Harmony String Orchestra Series. Christmas and Holiday. Set of parts. Excelcia Music Publishing #HSO2002. Published by Excelcia Music Publishing (XC.HSO2002).

UPC: 812598034233. 9 x 12 inches.

Introduce your students to 3/4 time with this clever mash-up of Christmas Carols in Waltz style. Each section has a turn to shine with the melody, perfect for parents to get a good shot of their little ones at their Christmas concert.

By Johann Strauss, Jr. Arranged by Mark Williams. Music by Johann Strauss / arr. Mark Williams. For String Orchestra. String Orchestra. Strictly Strings Series. Level: 1 (grade 1). Conductor Score and Parts. 1 pages. Published by Alfred 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.

By Emile Waldteufel (1837-1915). Arranged by Andrew Balent. String ensemble. For String Orchestra. Carl Fischer First Plus String Orchestra Series. Classical. Grade 1.5-2. Score and Parts. Standard notation. 8 pages. Published by Carl Fischer

For Full or String Orchestra. Arranged by Larry Clark. For Full Orchestra. Full Orchestra. Belwin Intermediate Full Orchestra. Level: 2.5 (grade 2.5). Conductor Score and Parts. 234 pages. Published by Alfred Publishing.

Orchestra String Orchestra - Grade 4

SKU: AP.36-52255538

Composed by Joshua Reznicow. Performance Music Ensemble; String Orchestra. Ludwig Masters. Score. Latham Music Enterprises #36-52255538. Published by Latham Music Enterprises (AP.36-52255538).

ISBN 9781621568636. UPC: 746241260185. English.

A rousing concert ender, this work will challenge all sections with a wide range (every part shifts), running passage work, trills, and syncopated rhythms.  The B section, a lyric waltz theme, shows off the principal players with extended solos.  The return of the A section superimposes the waltz melody on the original syncopated theme for a wonderful conclusion.

These products are currently being prepared by a new publisher. While many items are ready and will ship on time, some others may see delays of several months.

Orchestra String Orchestra - Grade 4

SKU: AP.36-52250538

Composed by Joshua Reznicow. Performance Music Ensemble; String Orchestra. Ludwig Masters. Patriotic. Score and Part(s). Latham Music Enterprises #36-52250538. Published by Latham Music Enterprises (AP.36-52250538).

ISBN 9781621568629. UPC: 679360699294. English.

A rousing concert ender, this work will challenge all sections with a wide range (every part shifts), running passage work, trills, and syncopated rhythms.  The B section, a lyric waltz theme, shows off the principal players with extended solos.  The return of the A section superimposes the waltz melody on the original syncopated theme for a wonderful conclusion.

These products are currently being prepared by a new publisher. While many items are ready and will ship on time, some others may see delays of several months.

For String Orchestra. Composed by Yukiko Nishimura. Southern Music. Concert. Softcover. Southern Music Company #SO127C. Published by Southern Music Company

Composed by Frank Halferty. For string orchestra (88555) with optional 3rd violin/viola TC (3 copies) and piano. Playground String Orchestra Series. Grade 1. Score and set of parts. Duration 3 minutes, 20 seconds. Published by Kendor Music Inc

By Strauss. Arranged by Deborah Baker Monday. Cadet String Orchestra. Level: Grade 2. Published by Kendor Music Inc.

Orchestra String Orchestra - 3 (grade 3)

SKU: AP.31626S

Composed by Almon C. Bock II. String Orchestra. Highland/Etling String Orchestra. Novelty. Score. 24 pages. Highland/Etling #00-31626S. Published by Highland/Etling (AP.31626S).

UPC: 038081352893. English.

This theme and six variations on the well-known children's song incorporate many string-playing techniques providing great teaching opportunities in a setting sure to be a hit with young and old alike. The six variations, including a waltz and a cha-cha, are uniquely woven to maintain the theme, but impart their own characters and flavors featuring each section of the orchestra at various times. The final variation includes a surprise and will leave audiences wondering if they heard correctly. The piece ends with a rousing restatement of the theme.

By Almon C. Bock II. Orchestra. String Orchestra. Highland String Orchestra. Light Concert; Novelty. Grade 3. Conductor Score and Parts. 124 pages