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 Lorenz Hart, music by Richard Rodgers. Arranged by Jeffrey E. Turner. Orchestra. Part(s); Score; String Orchestra. Pop Concert String Orchestra. Broadway. Grade 3. 64 pages. Published by Alfred Music

Composed by Jeffrey Bishop. String Tracks. Score and parts. Published by Neil A. Kjos Music Company (KJ.SO306C).

Orchestra String Orchestra - Grade 1.5-2

SKU: CF.FAS11

Composed by Larry Clark. FS SWS. Carl Fischer First Plus String Orchestra Series. Classical. Score and Parts. With Standard notation. 8+8+5+5+5+2+8 pages. Carl Fischer Music #FAS11. Published by Carl Fischer Music (CF.FAS11).

ISBN 9780825845048. UPC: 798408045043. 8.5 X 11 inches. Key: G major.

This outstanding original from Larry Clark can be played any time of year! A vigorous theme moves through all the sections and violas combine with second violins for prominent solo passages. A section in minor adds to the drama as strong rhythmic chords give way to a subdued tremolo in the first violins, reminiscent of Vivaldi's Winter This music reaches a level of intensity your players and audience will love.
Out of the Winter is a musical depiction of the many moods of winter from its harsh storms to its simple beauty. The composition is based on a central main theme that is musically developed throughout the composition presented in and out of major and minor keys.The main theme begins right away without introduction and is set to depict the simple delicate beauty of a light falling snow. The theme is then developed in the minor key using simple contrapuntal techniques that give the composition a fresh sound for pieces at this grade level. The aggressive development of the piece is a musical description of a powerful winter storm. The tension of this section is built to a climax using simple divisi in the strongs and some poly-chordal harmonic techniques that give way to a final return of the main theme to complete the piece.Special care should be given to exaggerating the contrast between the two diverse sections of the piece. The main theme should be light and uplifting. The second section with the theme in minor should have an ominous presence, but still be reminiscent of the original light main theme. As with all of my compositions at this grade level, adjust the tempo to fit the ability level of your students. It is hope that this piece helps to reinforce the concepts of good musicianship which you are trying to instill in your students. Bowings should be used as a guide and should be adjusted to your needs.It has been my pleasure to have had the opportunity to write this piece. I hope that you and your students find it useful for your program.

Orchestra String Orchestra - Grade 2-2.5

SKU: CF.YAS33

Composed by Sean O'Loughlin. SWS - FS. Carl Fischer Young String Orchestra Series. Classical. Score and Parts. With Standard notation. 8+16+16+4+10+10+10+3 pages. Carl Fischer Music #YAS33. Published by Carl Fischer Music (CF.YAS33).

ISBN 9780825858468. UPC: 798408058463. 8.5 X 11 inches. Key: G major.

A walk through the park or a morning stroll through the forest is what this piece best calls to mind. With its pastoral setting and lush melodies, Velvet Morning will truly showcase your group's mastery of legato playing.
Velvet Morning is a warm and colorful work for string orchestra. Please play con sordino if available. The music is a reflection of my love for the orchestral music of Barber, Ravel, Debussy and Satie. It should have the same sense of passion and intensity that those masters employ in their music.The opening tempo is marked rubato, and should speed up then slow down based on the phrases. The main melody appears at m. 11 in the first violins and should have a flowing quality. The harmony does utilize some slight dissonances from time to time which should be emphasized. The violas and cellos take over the melody at m.19 with a counter line in the violins. The melody returns to the violin at m. 27 with a pianistic cello line punctuated by pizzicato in the bass. Some transitional material follows that builds up to a full presentation at m. 47. Let the ensemble open up here with an intense, full sound. This winds down to a return of the introduction at m. 60. The ending should be tender and deliberate all the way to the last plush chord.

About Carl Fischer Young String Orchestra Series

Thi s series of Grade 2/Grade 2.5 pieces is designed for second and third year ensembles. The pieces in this series are characterized by:
--Occasionally extending to third position
--Keys carefully considered for appropriate difficulty
--Addition of separate 2nd violin and viola parts
--Viola T.C. part included
--Increase in independence of parts over beginning levels

Orchestra String Orchestra - Grade 2-2.5

SKU: CF.YAS33F

Full Score. Composed by Sean O'Loughlin. Carl Fischer Young String Orchestra Series. Full score. With Standard notation. 8 pages. Carl Fischer Music #YAS33F. Published by Carl Fischer Music (CF.YAS33F).

ISBN 9780825858475. UPC: 798408058470. 8.5 X 11 inches. Key: G major.

A walk through the park or a morning stroll through the forest is what this piece best calls to mind. With its pastoral setting and lush melodies, Velvet Morning will truly showcase your group's mastery of legato playing.
Velvet Morning is a warm and colorful work for string orchestra. Please play con sordino if available. The music is a reflection of my love for the orchestral music of Barber, Ravel, Debussy and Satie. It should have the same sense of passion and intensity that those masters employ in their music.The opening tempo is marked rubato, and should speed up then slow down based on the phrases. The main melody appears at m. 11 in the first violins and should have a flowing quality. The harmony does utilize some slight dissonances from time to time which should be emphasized. The violas and cellos take over the melody at m.19 with a counter line in the violins. The melody returns to the violin at m. 27 with a pianistic cello line punctuated by pizzicato in the bass. Some transitional material follows that builds up to a full presentation at m. 47. Let the ensemble open up here with an intense, full sound. This winds down to a return of the introduction at m. 60. The ending should be tender and deliberate all the way to the last plush chord.

About Carl Fischer Young String Orchestra Series

Thi s series of Grade 2/Grade 2.5 pieces is designed for second and third year ensembles. The pieces in this series are characterized by:
--Occasionally extending to third position
--Keys carefully considered for appropriate difficulty
--Addition of separate 2nd violin and viola parts
--Viola T.C. part included
--Increase in independence of parts over beginning levels