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 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.

By Alan Lee Silva. For string orchestra. Carl Fischer Concert String Orchestra Series. Grade 3 and up. Score and parts. Published by Carl Fischer

By Richard Meyer. By Richard Meyer. For String Orchestra. String Orchestra. String Explorer. Level: 1.5 (grade 1.5). Conductor Score and Parts. Published by Alfred Publishing.

Orchestra string orchestra - Grade 2.5

SKU: XC.ISO2204

Composed by Steve Parsons. Contest. Intermezzo. Contest. Score and set of parts. Excelcia Music Publishing #ISO2204. Published by Excelcia Music Publishing (XC.ISO2204).

12 x 9 inches.

A swirling vortex...a spinning clock going backwards and forwards...cities growing or shrinking in size before one's very eyes...these are the images of many a tale of temporal adventure throughout the ages. Take a trip through time with Composer Steve Parsons!

Orchestra string orchestra - Grade 2.5

SKU: XC.ISO2204FS

Composed by Steve Parsons. Contest. Intermezzo. Score. Excelcia Music Publishing #ISO2204FS. Published by Excelcia Music Publishing (XC.ISO2204FS).

12 x 9 inches.

A swirling vortex...a spinning clock going backwards and forwards...cities growing or shrinking in size before one's very eyes...these are the images of many a tale of temporal adventure throughout the ages. Take a trip through time with Composer Steve Parsons!

Orchestra String Orchestra - Grade 2

SKU: FJ.ST6252S

Score Only. Composed by Soon Hee Newbold. Series; String Orchestra. FJH Developing Strings. Multicultural. Score. Duration 1:15. The FJH Music Company Inc #98-ST6252S. Published by The FJH Music Company Inc (FJ.ST6252S).

English.

Experie nce Celtic festivals, maypoles, and country fairs in this spirited and lively piece. Set in an easy 6/8 time, players are transported back to a time of ancient dances and celebrations in Ireland. The lower voices begin with bagpipe drones as violins take on the first theme. Infectious melodies and secondary themes complete this endearing piece. Students have a chance to work on bow distribution, hooked bowing, pizzicato and dynamics.

Orchestra String Orchestra - Grade 3.5

SKU: FJ.ST6145S

Score Only. Composed by Soon Hee Newbold. Series; String Orchestra. FJH String Orchestra. The constellation Equuleus means the Foal or Little Horse and lies between Pegasus and Delphinus. The original name may have been Equus Primus (First Horse) because it rises before Pegasus each evening. The origin of the name and story, however, h. Score. Duration 3:40. The FJH Music Company Inc #98-ST6145S. Published by The FJH Music Company Inc (FJ.ST6145S).

English.

Based on the small constellation Equuleus (The Foal or Little Horse), this rich symphonic work celebrates the life of a student originally from Poland who loved horses and had dreams of joining the air force. From riding horseback through the Polish landscape to flying over the beautiful Tatra Mountains onward to the stars, this moving work will take you on a thrilling and emotional journey.

Orchestra String Orchestra - Grade 2.5

SKU: FJ.ST6515S

Score Only. Composed by Soon Hee Newbold. Series; String Orchestra. FJH Developing Strings. Score. The FJH Music Company Inc #98-ST6515S. Published by The FJH Music Company Inc (FJ.ST6515S).

English.

Take flight through the soaring melodic lines of this bold work that lets your students' imaginations run wild. Whether on the back of a hawk or on a journey to space, this energy-infused piece keeps all sections engaged rhythmically and melodically. A dynamic key change adds to the adrenaline rush. Thrilling!

Study Score. This edition: ETP1331. Eulenburg Taschenpartituren (Pocket Scores). Study Score. 60 pages

By Johann Sebastian Bach. Arranged by Andrew Balent. For String Orchestra. Published by Carl Fischer.