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.

For String Orchestra. Composed by Ulysses Kay. Score. 16 pages. Carl Fischer Music #BE26. Published by Carl Fischer Music

By Johann Sebastian Bach (1685-1750). Arranged by Elizabeth Start. Orchestra. Part(s); Score; String Orchestra. Belwin Concert String Orchestra. Form: Fugue; Prelude. Baroque; Masterwork Arrangement. Grade 3.5. 124 pages. Published by Belwin Publishing

Composed by Soon Hee Newbold. For string orchestra. FJH Developing Strings. Grade 2. Score and parts. Duration 2 minutes, 30 seconds. Published by The FJH Music Company Inc

By Mark Williams. For String Orchestra. String Orchestra. Strictly Strings Series. Novelty. Level: 1.5 (grade 1.5). Conductor Score & Parts. 36 pages. Published by Alfred Publishing.

By Alan Menken, Stephen Schwartz. Arranged by Jim Kazik. (Score and Parts). Pop Specials for Strings. Published by Hal Leonard.

By Michael Hopkins. Orchestra. Score; String Orchestra. Belwin Beginning String Orchestra. Light Concert. Grade 2.5. 12 pages

Arranged by Virginia Croft. Score and part(s). 8 70 pages. Duration 1 minute, 52 seconds. Carl Fischer #FAS0095. Published by Carl Fischer (CF.FAS95).

Composed by Girolamo Frescobaldi (1583-1643). Edited by J. Cameron Law. Arranged by John Beeman. For string orchestra. Grade 2. Score and set of parts. Duration 2 minutes. Published by Grand Mesa Music

By Peter Ilyich Tchaikovsky (1840-1893). Arranged by Mark Weston, scored by Douglas E. Wagner. Orchestra. For strings w/ vln 3. Masterworks; Part(s); Score; String Orchestra. Belwin Beginning String Orchestra. Christmas; Light Concert; Masterwork Arrangement; Novelty; Romantic; Winter. Grade 2.5. 144 pages. Published by Belwin Publishing

Composed by Richard Meyer. Orchestra. Part(s); Score; String Orchestra. Highland� String Explorer. Grade 1.5. 144 pages. Published by Highland/Etling

Composed by Nikolay Andreyevich Rimsky-Korsakov (1844-1908). Arranged by Bob Lipton. For string orchestra. FJH Developing Strings. Level 2.5. Score only. Duration 2:30. Published by The FJH Music Company Inc

By Wolfgang Amadeus Mozart (1756-1791). Arranged by Sandra Dackow. For String Orchestra. Grade 3. Set of parts

(Bass Section Feature). By Jacques Offenbach (1819-1880). Arranged by Richard Meyer. Orchestra. Masterworks; Part(s); Score; String Orchestra. Highland String Explorer. Form: Dance. Light Concert; Masterwork Arrangement; Romantic. Grade 1.5. 72 pages. Published by Alfred Music Publishing

Composed by Bill Calhoun. For string orchestra (violin I, violin II, violin III (viola T.C.), viola, cello, bass, piano). Score and parts. Duration 2 minutes, 11 seconds. Published by Carl Fischer

By Victor López. Orchestra. Part(s); Score; SmartMusic; String Orchestra. Belwin Beginning String Orchestra. Light Concert. Grade 1. 78 pages. Published by Belwin Music

By Antonin Dvorák. Arranged by Jeffrey E. Turner. Orchestra. String Orchestra. Belwin Concert String Orchestra. Romantic. Grade 3.5. Conductor Score and Parts. 62 pages

Composed by Todd Parrish. Orchestra. Part(s); Score; String Orchestra. Highland String Orchestra. Grade 1. 62 pages. Published by Highland/Etling

2nd Movement. Composed by Ludwig van Beethoven (1770-1827). Arranged by Bud Caputo. Masterworks; Part(s); Score; String Orchestra. Highland/Etling String Orchestra. Form: Sonata; Transcription. Classical; Masterwork Arrangement; Romantic. 124 pages. Published by Highland/Etling (AP.40471).

By Wolfgang Amadeus Mozart (1756-1791). Arranged by Sandra Dackow. For String Orchestra. Grade 3. Score

Composed by Michael Hopkins. Score; SmartMusic; String Orchestra. Belwin Intermediate String Orchestra. 16 pages. Published by Belwin Music (AP.41202S).

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

By De Boismortier. Arranged by Robert D. Mccashin. String Orchestra. FJH String Orchestra. The opening Adagio is excellent for working on a full-bodied sound while developing a moderate to weighty bow arm. The Allegro section can be performed either as a full tutti work or in a concerto grosso fashion, giving you the flexibility of featuring your outstanding individual players while still programming the work with a younger ensemble. Outstanding! Score for this title: S. Extra part for this title: P. Level: 4. Published by The FJH Music Company Inc.