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 Ludwig van Beethoven (1770-1827). Arranged by Bud Caputo. For string orchestra. Concert Work. Grade 3. Conductor score. Duration 4:54. Published by Wingert-Jones Publications

Composed by Brendan Mcbrien. For string orchestra. Christmas/Holiday. Grade 4. Score and set of parts. Duration 3:25. Published by Wingert-Jones Publications

Composed by David Bobrowitz. For string orchestra. Folk. Grade 3. Score and set of parts. Duration 4:18. Published by Wingert-Jones Publications

Composed by David Bobrowitz. For string orchestra. Folk. Grade 3. Conductor score. Duration 4:18. Published by Wingert-Jones Publications

Composed by Jeffrey Bishop. For string orchestra. Original Concert Work. Grade 4. Score and set of parts. Duration 5:18. Published by Wingert- Jones Publications

Composed by Marvin Hamlisch. Arranged by Larry Moore. For String Orchestra, Orchestra (Score and Parts). Pop Specials for Strings. Grade 3-4. Published by Hal Leonard

Arranged by Robert Kerr. Arr. Robert Kerr. For String Orchestra. String Orchestra. String Orchestra. Level: 4 (grade 4). Conductor Score and Parts. 2 pages. Published by Alfred Publishing.

Composed by David Bobrowitz. For string orchestra. Light Concert. Grade 4. Score and set of parts. Duration 4:06. Published by Wingert-Jones Publications

Orchestra String Orchestra - Grade 4

SKU: FJ.ST6364

Composed by Wolfgang Amadeus Mozart. Arranged by John O'Neill. MakeMusic Cloud; String Orchestra. FJH String Orchestra. The Allegro molto from Mozart's Symphony No. 40 is arguably one of the most well-known melodies in all of classical literature. This arrangement goes well beyond the melody to give a broad representation of the entire movement while remaining very accessi. Masterwork Arrangement. Score and Part(s). Duration 3:15. The FJH Music Company Inc #98-ST6364. Published by The FJH Music Company Inc (FJ.ST6364).

UPC: 674398232758. English.

The Allegro molto from Mozart's Symphony No. 40 is arguably one of the most well-known melodies in all of classical literature. This arrangement goes well beyond the melody to give a broad representation of the entire movement while remaining very accessible to students.

About FJH String Orchestra

More emphasis on bow technique and independence of lines. For the accomplished middle, high school, college, or professional group. Grade 3 and up

(Featuring: Magic to Do / Corner of the Sky / With You / Love Song / No Time at All). Composed by Stephen Schwartz. Arranged by Andrew H. Dabczynski. Orchestra. Score; SmartMusic; String Orchestra. Pop Concert String Orchestra. Form: Medley. Broadway. Grade 4. 48 pages. Published by Alfred Music

By Greg Bartholomew. For String Orchestra. Level 3/4. Score and parts. Duration 3 minutes. Published by Imagine Music

By Richard Meyer. Orchestra. For String Orchestra. String Orchestra. Highland String Orchestra. Fall; Halloween. 4 (grade 4). Score. 32 pages

Featuring: The Stars Our Home / The Fall of Shakuras / Honor Guides Me / My Life for Aiur. Composed by Jason Hayes and Michael Patti. Arranged by Michael Story. Part(s); Score; String Orchestra. Pop Intermediate String Orchestra. Video Game. 156 pages. Published by Alfred Music

By Richard Meyer. Orchestra. String Orchestra. Highland String Orchestra. Fall; Halloween. Grade 4. Conductor Score and Parts. 124 pages

By Randy Sabien. Music by Randy Sabien. For String Orchestra. String Orchestra. String Alternatives. Jazz. Level: 4 (grade 4). Conductor Score and Parts. Published by Alfred Publishing.

By Edward Elgar. Arranged by Bender. Concert String Orchestra. Level: Grade 4. Published by Kendor Music Inc.

By Brian Balmages. Beginning String Orchestra. FJH Beginning Strings. This fun-spirited fiddle tune begins with a unison statement of the theme, then gradually expands in harmony until the entire ensemble is into the groove. While the theme develops, the initial pizzicato in the low strings serves as the rhythm section of the group. Other members of the orchestra take over this rhythm section, including violas (and optional violin 3), stomping and clapping as the hoedown begins to roar. As is characteristic of much fiddle music, Hey Fiddle Fiddle! is based mostly on open 4ths and 5ths. These intervals become the focus of the piece at measure 49, where violins and violas trade phrases back and forth with low strings. One final build brings the tune back for a stirring conclusion. Score for this title: ST6120S. Extra part for this title: ST6120P. String Orchestra. Level: 1.5. Score and Set of Parts. Published by The FJH Music Company Inc.

(A Whirlwind Journey). Composed by Harold Arlen, lyrics by E. Y. Harburg, incidental music by Herbert Stothart, George Bassman, and Felix Mendelssohn. Arranged by Steven H. Brook. Orchestra. Score; String Orchestra. Pop Concert String Orchestra. Light Concert; Movie. Grade 4. 44 pages. Published by Alfred Music

(A Whirlwind Journey). Composed by Harold Arlen, lyrics by E. Y. Harburg, incidental music by Herbert Stothart, George Bassman, and Felix Mendelssohn. Arranged by Steven H. Brook. Orchestra. Part(s); Score; String Orchestra. Pop Concert String Orchestra. Light Concert; Movie. Grade 4. 248 pages. Published by Alfred 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