SKU: KN.36315
UPC: 822795363159.
It's winter and the sun has already set, but a bright moon allows the whiteness of the snow covered ground to show a clear path. Everyone is excited in anticipation of a fun evening gliding through the snow on a horse driven sleigh. Then we're off, and a catchy melody follows us as we ride through the winter night. Evening Sleigh Ride is a piece that is a perfect addition to your string orchestras Winter Concert. It will leave both performers and audience with an upbeat feeling to the start of their winter break. Set includes optional 3rd Violin/Viola T.C. and percussion parts.Set includes optional 3rd Violin/Viola T.C. and percussion parts.
SKU: FJ.ST6533
UPC: 241444437384. English.
Journey to the vast countryside of Scotland as you imagine the sound of bagpipes rolling over a heather moor. Memorable melodies abound in every part, portraying the strength and pride of the Scottish Highlanders as well as the beauty of the Highlands. Ideal for expanding range, rhythmic understanding and musical expression.
SKU: FJ.ST6533S
English.
SKU: XC.ISO2105FS
UPC: 812598037296. 9 x 12 inches.
Alan Lee Silva takes us on a journey inspired by the luminous green foliage he experienced hiking with his family on the trails in Oregon. Sparkling greenery is a perfect way to describe the bubbly and iridescent nature of Viridescence. Your audience will be captivated by the sound of this work.
SKU: XC.ISO2105
UPC: 812598037593. 9 x 12 inches.
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: XC.HSO2301FS
9 x 12 inches.
This delightful waltz gives your performers and audience the feeling of a lovely ride on an old-time carousel. As you circle around, the carousel horse gently moves up and down to the soothing music. The piece then moves to a melancholy theme as the ride is coming to an end. A stunning new piece for developing string orchestras.
SKU: XC.HSO2301
SKU: KJ.SO264F
Movement I: Ichabod's Walk Movement II: Hessian's Ride Another exciting work from top-selling composer Kirt Mosier! The two-movement piece is based on The Legend of Sleep Hollow: the first section is an off-beat tango, and the second is a blazing musical chase over a motor rhythm. A thrilling ride!
SKU: CF.CAS44
ISBN 9780825867118. UPC: 798408067113. 8.5 X 11 inches. Key: G minor.
This is a tour-de-force for the advancing string orchestra. Beautiful, dramatic, and flowing, Waterloo Station is very fresh and contemporary. Students will love it for the lush harmonic textures and rhythmic drive that this composer is so noted for.Composed as a characterization of the fast-paced atmosphere of London’s Waterloo Train Station, this fast-slow-fast piece combines technical excitement with heartfelt simplicity.The fast section in G minor consists of two main parts: the intense, emotional A section at m. 21 and the legato, sweeping B section at m. 59. The syncopated tutti figures in the high strings coupled with the fiery cello and bass lines propel the fast sections. The phrase in mm. 1–8 recurs throughout. Making four- to eight-measure exercises of this section below tempo in the violins and viola, focusing on rhythmic clarity, will help to lock in the syncopation. Similarly, the cello and bass should rehearse this slowly as well as mm. 9–16 to gain fluidity and insure a solid foundation.The cellos carry the tune at m. 71, and the ensemble builds from mm. 79–86 to the transition at m. 87. An abrupt change to half tempo here slows the momentum and transitions to a quiet, melancholy tone in m. 91. The middle section (ABA) begins in G minor with a somber quality, highlighted by the Violin I solo. It gradually builds to a beautiful, uplifting setting as it moves to G major in m. 100. Returning back to the hushed G minor tonality, it then speeds up again and transitions back to Tempo I for a brief recapitulation of the fast section. Measure 117 marks the return to vigorous playing, beginning softly and building to a thrilling ride to the end.
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: FJ.ST6334S
Written when the composer was a mere 15 years old, this jaunty scherzo will take your ensemble on a high-speed ride! Sections take turns bouncing around with the work's catchy melodies before moving into a slow detour with lush and yearning harmonies. The work eventually returns to its original tempo before moving into a delightful and unexpected ending. Fabulous!
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
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