Composed by Greg Bartholomew. For "trumpet, timpani & string orchestra". Pathways Series. Level 4. Score and set of parts. Duration "3 minutes, 40 seconds". Published by Imagine Music

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 Peter Ilyich Tchaikovsky. Arranged by Sandra Dackow. For String Orchestra. Level: Grade 3. Set of parts. Published by Tempo Press.

By Jacques Offenbach. Arranged by Sandra Dackow. For String Orchestra. Level: Grade 1. Score. Published by Tempo Press.

By Peter Ilyich Tchaikovsky. Arranged by Sandra Dackow. For String Orchestra. Level: Grade 3. Score. Published by Tempo Press.

With a Yo Heave Ho. Arranged by Sandra Dackow. Performance Music Ensemble; Single Titles; String Orchestra. Orchestra Expressions. Folk. Score. 12 pages. Duration 2:25. Alfred Music #00-44789S. Published by Alfred Music (AP.44789S).

Arranged by Sandra Dackow. Performance Music Ensemble; Single Titles; String Orchestra. Orchestra Expressions. Folk. Score. 12 pages. Duration 1:30. Alfred Music #00-45825S. Published by Alfred Music (AP.45825S).

Arranged by Sandra Dackow. Part(s); Score; String Orchestra. Orchestra Expressions. Folk. 148 pages. Published by Alfred Music (AP.45825).

With a Yo Heave Ho. Arranged by Sandra Dackow. Part(s); Score; String Orchestra. Orchestra Expressions. Folk. 148 pages. Published by Alfred Music (AP.44789).

4 Tunes from the Scottish Island of Sanday - String Ensemble. By Peter Maxwell Davies. String. 28 pages. Published by Schott.

Composed by Greg Bartholomew. For "trumpet, percussion & string orchestra". Pathways Series. Level 4. Score and set of parts. Duration "3 minutes, 40 seconds". Published by Imagine Music

Composed by Greg Bartholomew. For "trumpet, marimba & string orchestra". Pathways Series. Level 4. Score and set of parts. Published by Imagine Music

By Various. Arranged by Sandy Sandy. For String Orchestra. Carl Fischer First Plus String Orchestra Series. Grade 1.5-2. Full Score. Standard notation. Published by Carl Fischer

(March from Aida, the Anvil Chorus from Il Trovatore, Quando M'en Va from La Boheme, Overture to the Barber of Seville, and Les Toreadors from Carmen - Full Score and Parts). By Sandy Feldstein. Arranged by Sandy Feldstein. String orchestra. For String Orchestra. Carl Fischer First Plus String Orchestra Series. Grade 1.5-2. Score and Parts. Standard notation. 10 pages

By Sandy Feldstein. Arranged by Sandy Feldstein. String orchestra. For String Orchestra. Carl Fischer First Plus String Orchestra Series. Grade 1.5-2. Full Score. Standard notation. 10 pages. Published by Carl Fischer

By The Surfaris. Arranged by Sandra Dackow. By The Surfaris / arr. Sandra Dackow. For String Orchestra. String Orchestra. Orchestra Expressions Book 2. Level: 2 (Red) (grade 2 Red). Conductor Score. Published by Alfred Publishing.

Orchestra string orchestra - Grade 2.5

SKU: XC.ISO2207FS

Composed by Ruth Brittin. Contest. Intermezzo. Score. Excelcia Music Publishing #ISO2207FS. Published by Excelcia Music Publishing (XC.ISO2207FS).

12 x 9 inches.

The butterfly is a powerful metaphor of second chances, rebirth, and metamorphosis. The butterfly, seemingly so delicate and fragile, actually migrates thousands of miles, and is thus a symbol of tenacity and resilience. Composer Ruth Brittin brings us a wonderfully thoughtful and poignant new work for String Orchestra.

By Soon Hee Newbold. FJH String Orchestra. A vast and mighty empire for thousands of years, the ancient Egyptian civilization has intrigued and fascinated the modern world with its art, culture, and amazing architecture. The Great Sphinx, giant pyramids, and statues of pharaohs are the powerful images of Egypt. From King Tut to Cleopatra, ancient Egypt continues to be an influence on societies of today. Level: Grade 4. Published by The FJH Music Company Inc.

Composed by Bud Woodruff. Score and part(s). 12 120 pages. Duration 2 minutes, 31 seconds. Carl Fischer #YAS0157. Published by Carl Fischer (CF.YAS157).

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.

(A Revolutionary Method for Beginning Musicians (Conductor's Score)). By Bob Phillips, Peter Boonshaft, and Robert Sheldon. Orchestra. For Conductor's Score. Method/Instruction; Score; String Orchestra Method/Supplement. Sound Innovations. 200 pages. Published by Alfred Music Publishing

Sound Innovations for String Orchestra, Book 1 (Conductor's Score) (A Revolutionary Method for Beginning Musicians) by Bob Phillips, Peter Boonshaft, and Robert Sheldon. Orchestra. For Conductor's Score. This edition: Conductor's Score. Book; CD; DVD; Method/Instruction; String Orchestra Method/Supplement. 200 pages. Published by Alfred Music Publishing

Orchestra string orchestra - Grade 2.5

SKU: KJ.SO165F

Composed by Doris Gazda. Score. Neil A. Kjos Music Company #SO165F. Published by Neil A. Kjos Music Company (KJ.SO165F).

Composer/Arrang er Doris Gazda discovered a beautiful Mexican song Saludo A Santo San Francisco while visiting the San Xavier Mission located south of Tucson, Arizona. This mission serves as an active church on a reservation, yet is also a museum that attracts thousands of tourists each year. This arrangement is in the key of G minor and is in 6/8 time. A harp part is included.

By Soon Hee Newbold. String Orchestra. FJH String Orchestra. A vast and mighty empire for thousands of years, the ancient Egyptian civilization has intrigued and fascinated the modern world with its art, culture, and amazing architecture. The Great Sphinx, giant pyramids, and statues of pharaohs are the powerful images of Egypt. From King Tut to Cleopatra, ancient Egypt continues to be an influence on societies of today. Score for this title: ST6118S. Extra part for this title: ST6118P. Level: 4. Published by The FJH Music Company Inc.