SKU: FJ.ST6461S

English.

With compelling melodies and a heroic spirit, Rise of the Majestics is an invigorating piece that features plenty of excitement for the orchestra. The work includes prominent parts for viola and cello, with the option of an advanced cello part to supplement the rich orchestration. Fantastic and engaging music!

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: 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.ISO1904

UPC: 812598030518. 9 x 12 inches.

Escalation is an exciting new work for the developing string orchestra. The title suggests music that lifts and rises throughout. I endeavored to embody this concept but not be limited by it. The music does rise at times, but it also needs to pull back to make a complete musical statement. By its cinematic nature, the piece offers some wonderful teaching opportunities for both rhythmic and lyrical playing.

SKU: FJ.ST6475

UPC: 241444399774. English.

Hear the call of ancient ancestors in this exciting tribute to legend and legacy. Bold, heroic themes of fierce warriors and noble rulers rise through subtle pentatonic harmonies that suggest mighty Chinese dynasties. Adventurous melodies in a driving 6/8 are passed to every section with a few easy accidentals. A great teaching piece to focus on slurred string crossings while staying in first position. (3:15).

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.ST6455

UPC: 241444389010. English.

Follow in the footsteps of Olympians and experience the strength, passion and commitment of these incredible athletes. The soft, yet rich opening foreshadows the powerful music that follows. Aggressive rhythms juxtapose with soaring melodies and harmonic moments filled with tension and release. An exciting work with film score qualities and an optional harp part.

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: BT.EMBZ14451

Hungarian-English-German-French.

The stopping-places in this Musical journey are various countries of Europe, Albania, Bulgaria, Denmark, Poland, Hungary, Germany, Italy, Russia, Spain, Switzerland, Ukraine ? each is represented in this volume by a very easy, short arrangement of a folksong or children?s song. In the string orchestra violas are replaced by 3rd violins, among the parts included with the score there is an ad libitum part for double bass. Every piece is playable in the first position by all sections of the orchestra.

The stopping-places in this Musical Journey are various countries of Europe such as Albania, Bulgaria, Denmark, Poland, Hungary, Germany, Italy, Russia, Spain, Switzerland, and Ukraine. Each is represented in this volume bya very easy, short arrangement of a folksong or children's song. In the string orchestra violas are replaced by 3rd violins, among the parts included with the score there is an ad libitum part for double bass. Every piece is playablein the first position by all sections of the orchestra.Instrumentation: 3 vl1, 3 vl2, 3 vl3, 2 vlc, cbSeries Leggierissmo - growing repertoire for children's and youth string orchestras.

Die Leggerierissmo-Reihe von Editio Musica Budapest umfasst Stücke, mit und an welchen Kinderstreichorchester wachsen können. Jede Ausgabe ist in der ersten Lage spielbar und enthält Partitur und Stimmen (Violine 3 entspricht Viola).Die Stationen dieser Musikalischen Reise sind Albanien, Bulgarien, Dänemark, Polen, Ungarn, Deutschland, Italien, Russland, Spanien, die Schweiz und die Ukraine. Jedes Land wird von einem kurzen leichten Arrangement oder Volkslied repräsentiert. Enthaltene Stimen: 3x Violine 1, 3x Violine 2, 3x Violine 3, Kontrabass.

La collection Leggiero & Leggierissmo proposée par Editio Musica Budapest est une édition enrichie de pièces pour Orchestre Cordes Junior, dans un arrangement de degré de difficulté facile. Elle comprend des œuvres de compositeurs classiques et contemporains ainsi que des transcriptions de pièces faciles. La possibilité de substituer la partie d'alto par un 3e violon facilite l'interprétation des morceaux. Ces arrangements, qui favorisent l'acquisition d'une expérience musicale complète, sont l'œuvre des meilleurs pédagogues et compositeurs. Les annotations figurent en langue française. Voici un impressionnant Voyage Musical en 12 escales : Bulgarie •Albanie • Italie • Suisse • Espagne • Écosse • Danemark • Allemagne • Pologne • Russie • Ukraine • Hongrie.Instrumentation: 3 vl1, 3 vl2, 3 vl3, 2 vlc, cb.