SKU: CF.CAS37
ISBN 9780825863660. UPC: 798408063665. 8.5 X 11 inches. Key: C major.
A salute to the famous sailboat race, this rollicking piece in A minor introduces compound time with an opening (and closing) section in 12/8. The fast flowing music of the opening, vividly suggestive of a ship slicing through the waves, returns in a higher key (B minor) after a warmly scored, sweepingly melodic middle section. This is a piece whose sophistication is an excellent showcase for a more advanced performing group.Written in 12/8 in A minor, America’s Cup evokes the intensity and momentum of a wild sea with driving triplets, sweeping melodies, and accented downbeats. The A-material from the opening measure is played aggressively but lightly enough to keep the feeling of forward motion. Strong accents and rhythmically precise playing in the cello and bass provide solid support for the fast moving violin and viola passages. Measure 67 begins the slow, pastoral setting of the B-material. A gentle, lyrical violin motive in A major grows into a high, sweeping melody over sustained harmonies. This provides a brief repose before returning to the fastoriginal tempo and minor key as the recapitulation begins at m. 90. A modulation to B minor (m. 94) lifts the energy of the piece and gives young players the challenge of playing the running lines in another key. Measure 118 builds to the end, keeping the intensity a soft dynamic and growing into the final syncopated tutti unison figure in mm. 122–123.
About Carl Fischer Concert String Orchestra Series
This series of pieces (Grade 3 and higher) is designed for advancing ensembles. The pieces in this series are characterized by:
SKU: CF.CAS36
ISBN 9780825863646. UPC: 798408063641. 8.5 X 11 inches. Key: F major.
A warm and richly scored setting of the popular Christmas carol Bring a Torch Jeanette, Isabella, this full sounding arrangement will greatly enrich seasonal programming. Roy Phillippe has employed a broad palette of harmonic and instrumental colors to craft a memorable holiday selection.Bring a Torch is a lovely Christmas carol. Using techniques such as suspensions, re-harmonization and modulations, my goal is to provide an interesting showcase for this familiar melody. the introduction in F major features sustained violins with a pattern of moving eighth notes in the violas and cellos. This pattern recurs throughout the piece. The first statement of the melody is in the first violins. The second violins supply harmonic support along with the viola/cello pattern. Measures 13-29 feature a section of tutti chordal playing. Measure 30 crescendos into the modulation to D major at m. 32. Here, the dynamic is forte, and the viola/cello pattern returns. At m. 40, the violas and cellos have the melody with violin accompaniment. A crescendo begins at m. 44 and builds to fortissimo at m. 48, featuring a modulation to G major. At this point the melody should soar. A descrescendo at m. 60 is followed by a ritard at m. 64. The final four measures are in the original tempo ending on a tutti chord.Careful attention to dynamics, especially in the accompanying parts, will result in a fine performance.
SKU: CF.CAS36F
ISBN 9780825863653. UPC: 798408063658. 8.5 X 11 inches. Key: F major.
A warm and richly scored setting of the popular Christmas carol Bring a Torch Jeanette, Isabella, this full sounding arrangement will greatly enrich seasonal programming. Roy Phillippe has employed a broad palette of harmonic and instrumental colors to craft a memorable holiday selection.
SKU: FJ.ST6511
UPC: 241444418888. English.
Expand the reach of your holiday program with this wonderful arrangement of the medieval carol Personet Hodie (Let resound today in Latin). Often relegated to choir, this version for strings and percussion showcases bold, powerful lines and a strong rhythmic backdrop. An excellent addition to any winter program.
About FJH Developing Strings
Slightly more advanced than Beginning Strings, this series begins to involve more position work and a slightly more complex rhythmic figures. Rehearsal piano is often provided. Ideal for middle school and smaller high school programs. Grade 2 - 2.5
SKU: HL.4493045
UPC: 196288156482.
Elevate your orchestra's performance to new heights with the â??Flying Theme from E.T.â? by John Williams, brilliantly arranged for string orchestra by Robert Longfield. Let the enchanting melody and soaring strings take your audience through the skies, capturing the magic and wonder of this iconic Spielberg masterpiece. Perfect for young orchestras seeking to create a memorable musical experience. Bring the magic of E.T. to your stage with this exquisite arrangement, where the music truly takes flight!
SKU: FJ.ST6511S
English.
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.SO219C
UPC: 8402701447.
Based on the Civil War song, The Cruel War, this poignant work is about women who disguised themselves as men.
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