SKU: FJ.ST6432S
English.
A rocking celebration of the season! Set in first position with simple rhythms and no slurs, this contemporary arrangement includes the familiar carols Deck the Hall, Hark, the Herald Angels Sing, and Ding, Dong, Merrily On High. Every section of the orchestra is featured and the energetic cello/bass groove is driven by optional drum set and sleigh bells. An exuberant finale for your holiday concert!
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: CF.YAS59
ISBN 9780825866937. UPC: 798408066932. 8.5 X 11 inches. Key: D major.
Virginia Croft has taken a popular German canon and transformed it into a stunning new piece for young string groups. It begins with the canon as is, and then adds two other composed themes that complement the original tune. With its largely contrapuntal composition, this piece is an excellent opportunity for students to develop their independence.“All things shall perish from under the skyMusic alone shall live, music alone shall live,Music alone shall live, never to die.â€Here is an exciting treatment of a well-known simple canonic melody, first stated in its entirety by the cellos. As it passes through the voices, it should predominate over the accompanying embellishments, resulting in an energetic and exciting presentation of an old tune.What a wonderful way to teach the harmonic aspects of canonic melody while offering a lively and enjoyable experience for both performers and audience.
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: XC.DSO1903
UPC: 812598030426. 9 x 12 inches.
The holiday season is a time of joy, merriment, excitement, and traditions. One such time-honored tradition is the holiday string concert, which is often the debut performance for young musicians. This event is a celebration, not only of the holidays, but also of the growth and dedication of the beginner musicians. Angels in the Halls will enable beginning string students to demonstrate their developing skills while putting the audience in the spirit of the holidays.
SKU: XC.DSO1903FS
UPC: 812598030914. 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: CF.CAS34
ISBN 9780825861055. UPC: 798408061050. 8.5 X 11 inches. Key: E minor.
Cliffhanger is a programmatic work for string orchestra that harkens back to the days of silent film. One of the lasting images of that time period is the Saturday afternoon matinee, where each episode ended on a cliffhanger until it could be continued next week. This piece tells the familiar story of the damsel in distress who is tied up to the train tracks as a train is approaching. Nicely done!.Cliffhanger is a programmatic work for string orchestra that harkens back to the days of silent film. One of the lasting images of that time period is the Saturday-afternoon matinee, where each episode ended on a cliffhanger until it could be continued next week. This piece tells the familiar story of the damsel in distress who is tied up to the train tracks as a train is approaching.The opening of the piece sets the scene with danger and desperation. By m. 6, our hero is making his way on horseback to rescue the fair maiden. This main melody is developed and passed around the ensemble until m. 36, at which point despair sets in. The music is rich with romantic harmonies and inner lines. Be sure to bring out these inner lines to add to the passion and drama of the moment. It continues to build until a thunderous arrival at m. 49. From there we return to our hero, who is now getting close to the train tracks to save the fair maiden. The tension becomes the highest at m. 61, when we are still not sure if our hero will make it in time. But alas, at m. 68 he swoops in to save the day and rescue the fair maiden. Of course, they live happily ever after.My hope is that your ensemble will have some fun with this style of music. It was adapted from an arrangement I wrote for the new pipe organ at the Walk Disney Concert Hall in Los Angeles. They wanted some scary train music to show children how the organ was used back before movies had sound. Strings provide a heightened sense of drama with this genre of music.
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.CAS34F
ISBN 9780825861062. UPC: 798408061067. 8.5 X 11 inches. Key: E minor.
Cliffhanger is a programmatic work for string orchestra that harkens back to the days of silent film. One of the lasting images of that time period is the Saturday afternoon matinee, where each episode ended on a cliffhanger until it could be continued next week. This piece tells the familiar story of the damsel in distress who is tied up to the train tracks as a train is approaching. Nicely done!.Cliffhanger is a programmatic work for string orchestra that harkens back to the days of silent film. One of the lasting images of that time period is the Saturday- afternoon matinee, where each episode ended on a cliffhanger until it could be continued next week. This piece tells the familiar story of the damsel in distress who is tied up to the train tracks as a train is approaching.The opening of the piece sets the scene with danger and desperation. By m. 6, our hero is making his way on horseback to rescue the fair maiden. This main melody is developed and passed around the ensemble until m. 36, at which point despair sets in. The music is rich with romantic harmonies and inner lines. Be sure to bring out these inner lines to add to the passion and drama of the moment. It continues to build until a thunderous arrival at m. 49. From there we return to our hero, who is now getting close to the train tracks to save the fair maiden. The tension becomes the highest at m. 61, when we are still not sure if our hero will make it in time. But alas, at m. 68 he swoops in to save the day and rescue the fair maiden. Of course, they live happily ever after.My hope is that your ensemble will have some fun with this style of music. It was adapted from an arrangement I wrote for the new pipe organ at the Walt Disney Concert Hall in Los Angeles. They wanted some scary train music to show children how the organ was used back before movies had sound. Strings provide a heightened sense of drama with this genre of music.
SKU: FJ.ST6490
UPC: 241444411858. English.
The joy of the Christmas season flows through every measure of this delightful holiday reel that turns your violin section into Celtic fiddlers. Good King Wenceslas and Deck the Hall are intertwined with the classic reel Christmas Eve that will challenge and delight your players. Use optional bodhran (hand drum), guitar and pennywhistle to bring the true spirit of Scotland to your holiday concert.
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: FJ.ST6490S
SKU: FJ.ST6419S
Show your great sense of humor with this novelty piece that winds up creating near chaos in your ensemble! When the first violins join a local branch of the String Players Union, the other musicians and director soon learn that the union members must adhere to some hilarious performance guidelines. Accommodations include playing only some notes, giving the left hand a rest and even left hand free time! Staging possibilities are endless - this piece is easy to put together and is guaranteed to bring a smile to everyone in the hall!
SKU: FJ.ST6419
UPC: 241444375532. English.
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