SKU: CF.YAS29F
ISBN 9780825858390. UPC: 798408058395. 8.5 X 11 inches. Key: G major.
This fun tune based on the folk song The Little Beggar Man is skillfully arranged by James Uhl and has all the components needed to challenge developing string players. Very playable and with light counterpoint, Mr. Natural encourages rhythmic accuracy wh.
About Carl Fischer Young String Orchestra Series
This 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
SKU: AP.29727S
UPC: 038081320748. English.
Performers and audiences alike will enjoy the varied colors and counterpoint in this energetic work. Interplay, as the name implies, features the interaction of various melodic and rhythmic elements arranged above a cello and bass ostinato. Tonalities shift from major to minor adding to the challenge and excitement! (3:30).
SKU: KN.36380
UPC: 822795363807.
This high energy work for grade 2 groups will excite your audience and give your students a great musical experience. Appropriately challenging for each section of the orchestra, every player gets their chance at melodic content with exciting rhythmic accompaniments. This is a perfect concert closer. Set includes optional 3rd Violin/Viola T.C. and piano parts. Set includes optional 3rd Violin/Viola T.C. and piano parts.
SKU: AP.36-52255570
ISBN 9781581068474. English.
Pay tribute to the Greek muse of dance, Terpsichore, with this lively jig in G minor. Upper strings have the opportunity to shift to third position and stay there to play the main theme. Cellos are the most active shifters, using second, third, and fourth positions, and even the bass section will bounce around! An original work with a distinctly Celtic sound and feel, it's a kid-friendly fiddle tune with a catchy hook - and you can speed it up for a dizzying challenge!
These products are currently being prepared by a new publisher. While many items are ready and will ship on time, some others may see delays of several months.
SKU: 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.
SKU: KJ.SO200C
UPC: 8402701161.
A tribute to the Hubble telescope, this challenging, yet fun composition, includes a special message - but players and listeners must discover what the important message is! Resource material about the Hubble is provided. This is not to be missed.
SKU: AP.36-52255538
ISBN 9781621568636. UPC: 746241260185. English.
A rousing concert ender, this work will challenge all sections with a wide range (every part shifts), running passage work, trills, and syncopated rhythms. The B section, a lyric waltz theme, shows off the principal players with extended solos. The return of the A section superimposes the waltz melody on the original syncopated theme for a wonderful conclusion.
SKU: AP.36-52250538
ISBN 9781621568629. UPC: 679360699294. English.
SKU: FJ.ST6174S
English.
Let your bass section shine and groove in this upbeat medley of funk, swing and good ol' fashioned rock 'n' roll! Opportunities for improvisation are included (with written parts as well) and an optional drum set part really adds to the flair. While the basses show off, the other sections of the orchestra also experience the contagious rhythms and melodies as they get down and rock out. An absolute showstopper!
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
SKU: AP.36-52250490
ISBN 9781628761399. UPC: 746241212191. English.
Mambos just don't get any friendlier than this. Every section in the orchestra is featured, with lots of fun imitation between upper and lower strings. All parts are in first position, with only one low 2 in the violin 1 part. A nice tutti pizzicato section adds additional challenge to a very simple rhythmic theme. Optional percussion parts make this mambo muy bien!
SKU: CF.YAS19
ISBN 9780825854859. UPC: 798408054854. 8.5 X 11 inches. Key: D major.
Summer Dance is a melodic, up-tempo piece with plenty of musical and technical challenges for every player. Musicians should strive to play it with an energetic yet legato feel. A spirited introduction features an opening melody in the violins and active repeated-note pedal patters in the violas and low strings. An AABA form begins at m.5 and the orchestration is immediately pared down to feature violin I and cello. It then builds again in density to the B section, where a quick dynamic drop allows a question-and-answer melody between the two parts to sing out. In m. 29, the melody is harmonized and a countermelody in violin I introduced. The violins take the melody soaring in octaves in m. 33, as the piece again builds to the B section and suddenly quiets. Measure 55 then provides more question-and-answer interplay, this time for viola and cello, while violin continues with its newly harmonized melody. Summer Dance finishes with a soft recurrence of the opening figure and a build toward a powerful divisi voicing on beat 3 of m. 63, right before the final chord.Summer Dance is a melodic, up-tempo piece with plenty of musical and technical challenges for every player. Musicians should strive to play it with an energetic yetA legato feel. A spirited introduction features an opening melody in the violins and active repeated-note pedal patters in the violas and low strings. An AABA form begins at m.5 and the orchestration is immediately pared down to feature violin I and cello. It then builds again in density to the B section, where a quick dynamic drop allows a question-and-answer melody between the two parts to sing out. In m. 29, the melody is harmonized and a countermelody in violin I introduced. The violins take the melody soaring in octaves in m. 33, as the piece again builds to the B section and suddenly quiets. Measure 55 then provides more question-and-answer interplay, this time for viola and cello, while violin continues with its newly harmonized melody. Summer Dance finishes with a soft recurrence of the opening figure and a build toward a powerfulA divisi voicing on beat 3 of m. 63, right before the final chord.Summer Dance is a melodic, up-tempo piece with plenty of musical and technical challenges for every player. Musicians should strive to play it with an energetic yet legato feel. A spirited introduction features an opening melody in the violins and active repeated-note pedal patters in the violas and low strings. An AABA form begins at m.5 and the orchestration is immediately pared down to feature violin I and cello. It then builds again in density to the B section, where a quick dynamic drop allows a question-and-answer melody between the two parts to sing out. In m. 29, the melody is harmonized and a countermelody in violin I introduced. The violins take the melody soaring in octaves in m. 33, as the piece again builds to the B section and suddenly quiets. Measure 55 then provides more question-and-answer interplay, this time for viola and cello, while violin continues with its newly harmonized melody. Summer Dance finishes with a soft recurrence of the opening figure and a build toward a powerful divisi voicing on beat 3 of m. 63, right before the final chord.Summer Dance is a melodic, up-tempo piece with plenty of musical and technical challenges for every player. Musicians should strive to play it with an energetic yet legato feel.A spirited introduction features an opening melody in the violins and active repeated-note pedal patters in the violas and low strings. An AABA form begins at m.5 and the orchestration is immediately pared down to feature violin I and cello. It then builds again in density to the B section, where a quick dynamic drop allows a question-and-answer melody between the two parts to sing out.In m. 29, the melody is harmonized and a countermelody in violin I introduced. The violins take the melody soaring in octaves in m. 33, as the piece again builds to the B section and suddenly quiets. Measure 55 then provides more question-and-answer interplay, this time for viola and cello, while violin continues with its newly harmonized melody. Summer Dance finishes with a soft recurrence of the opening figure and a build toward a powerful divisi voicing on beat 3 of m. 63, right before the final chord.
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