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: FJ.ST6145S
English.
Based on the small constellation Equuleus (The Foal or Little Horse), this rich symphonic work celebrates the life of a student originally from Poland who loved horses and had dreams of joining the air force. From riding horseback through the Polish landscape to flying over the beautiful Tatra Mountains onward to the stars, this moving work will take you on a thrilling and emotional journey.
SKU: CF.YAS19F
ISBN 9780825854866. UPC: 798408054861. 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 patterns 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 13 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.
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.36-52250531
ISBN 9781628765755. UPC: 746241279828. English.
Take your beginning orchestra on a tour of the old west with this ballad in 3/4 time. A simple D major melody is passed between sections, with nothing more rhythmically complex than quarter notes. The violin 1 part requires a low 2 on the E string.
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: KN.9744
UPC: 822795097443.
This soprano aria from Wolfgang Amadeus Mozart's opera The Marriage Of Figaro in the key of D major, contains some interesting modulations and is playable by grade 2 groups. Much of the charm of this piece results from Mozart's creative and brief exploration of many tonal centers, and is a great example how a composer can take a relatively simple tune and provide a great deal of interest through imaginative harmonies. Each set includes three copies of the 3rd Violin/Viola T.C. part and an optional piano part. Duration 2:40. Available in SmartMusic.
SKU: CF.FAS38
ISBN 9780825861130. UPC: 798408061135. 8.5 X 11 inches. Key: D major.
One of the most beloved of all Christmas carols is presented in an easy, yet beautiful arrangement by Roy Phillippe. Every sections is given a chance to play the melody in the very playable setting. The optional piano part adds interest and colorful lines to this already very special piece.I am of the opinion that a piece of music is not judged by how difficult it is to play, but by how good it sounds. While my arrangement of Silent Night is written for beginning string players, I have tried to keep it interesting for all players. It should be played warmly with expression to create a full sound.The piece begins with an introduction based on the three-note Silent Night motive. The main melody is introduced in m. 5 by the first Violins, and is harmonized by the second Violins and Violas. The Cellos reiterate the motive in mm. 6,8,10 and 11. Beginning at m.12 the motive alternates between the Violin II and the Cellos. The melody is played tutti until the key change at m.29, at which point when the Cellos and Basses take the melody with light accompaniment in the Violins and Violas. The final statement of the melody is played by the first violins beginning in m. 37. The Silent Night motive from the beginning alternates between Violin II and the Cellos to the end.
SKU: FJ.ST6406S
This new setting of Good King Wenceslas will be a welcome addition to any holiday concert. Students get into that action as they march while playing, and all sections take turns playing the melody. Students and teachers will be merrily surprised at how easily this selection comes together. Happy marching!
About FJH Beginning Strings
Appropriate for first year string students. All instruments stay in first position, and optional third violin (viola) parts and piano are included to aid in rehearsal and performance situations. Grade 1 - 1.5
SKU: KN.KES2301
12 x 9 inches.
Take a musical stroll with your young string performers with with this new, very easy piece from David Hinds. An excellent choice for a first concert as well as being a great piece to use for teaching form.
SKU: FJ.ST6252S
Experience Celtic festivals, maypoles, and country fairs in this spirited and lively piece. Set in an easy 6/8 time, players are transported back to a time of ancient dances and celebrations in Ireland. The lower voices begin with bagpipe drones as violins take on the first theme. Infectious melodies and secondary themes complete this endearing piece. Students have a chance to work on bow distribution, hooked bowing, pizzicato and dynamics.
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