SKU: HL.50606986
ISBN 9798350128697. UPC: 196288215332. 9.0x12.0x0.138 inches.
Commissioned by the Stockholm Concert Hall Foundation, Stockholm Diary is a powerful and virtuosic 13 minute piece for string orchestra. Written in 2004 for Esa-Pekka Salonen's Composer Portrait, October 2004, the work is a prime example of the composer's use of harmonies and rich, creamy textures.
SKU: HL.14019637
ISBN 9780711950115. 9.0x12.0x0.1 inches.
Study Score. Duration c.9 mins.
SKU: KN.08143S
UPC: 822795081435.
William Billings' illustrious hymn Chester is scored here in a very playable concert setting that allows for a full sound and interesting lines in all parts. The simple nobility of the melodic line and its strong, solid harmonies are major factors in the enduring popularity of this song. Duration 2:55. Available in SmartMusic.
SKU: HL.14021618
SKU: HL.14005636
UPC: 884088811549. 8.5x11.0x0.09 inches.
Written for string orchestra.
SKU: HL.14043724
UPC: 196288024569. 11.75x16.5x0.478 inches.
Nymphea Reflection is a work by renowned composer Kaija Saariaho, arranged for String Orchestra. Commissioned by the Schleswig Holstein Festival, it was first performed on the 16th of August 2001 inElmshorn, Germany by Sinfonietta Cracovia, conducted by John Axelrod.
SKU: BT.EMBZ14570
Hungarian-English-German-French.
Following the Renaissance volume, this time it is Baroque works (more precisely, transcriptions of Baroque vocal and instrumental works) that are presented in the Leggierissimo series, extending the repertoire of junior string orchestras. Roughly half of the selection consists of well-known pieces by the greatest composers of the period (Purcell: Dido and Aeneas, Rameau: Pi ces de clavecin, Händel: Water Music, Music for the Royal Fireworks, J.S. Bach: B major partita, C major orchestral suite), but works by composers less well known nowadays (for example, G. Böhm and J. C. F. Fischer) are also included, together with such unusual items as Polish, German and Hungarian dancesfrom 17th- and 18th-century Hungarian manuscripts: the Kájoni and Vietórisz codexes, and Eleonóra Lányi s music book. Nach dem Renaissance-Band erscheint die Leggierissimo-Serie nunmehr mit Barockwerken (genauer: mit Transkriptionen nach vokalen und instrumentalen Barockwerken), die das Repertoire der Kinderstreichorchestern erweitert. Etwa die Hälfte der Sammlung machen die Stücke der allgemein bekannten Werke der größten Komponisten der Epoche (H. Purcell: Dido und Aeneas, J. Ph. Rameau: Pi ces de clavecin, G. F. Händel: Wassermusik, Feuerwerksmusik, J. S. Bach: Partita B-Dur, Ouverture C-Dur) aus. Es kommen in ihr aber auch Stücke von heute weniger bekannten Komponisten (G. Böhm, J. C. F. Fischer u.a.), daneben als Besonderheit polnische, deutsche und ungarische Tänze aus dem 17. und 18.Jahrhundert aus dem Kájoni- und Vietórisz-Kodizes und aus dem Notenbuch der Eleonora Lányi vor.
SKU: HL.14004140
ISBN 9780711998322. UPC: 502067952679. 7.0x10.0x0.156 inches.
A new edition of one of Berkeley's most frequently performed works, in this the composer's centenary year. This work is a classic in the repertoire of British Music for this medium. The first movement has the sparkling elegance of Mozart whom Berkeley idolised, but also the driving rhythm of a Bach Brandenburg Concerto; the second is a serenade; the third a kind of scherzo; but the final movement seems to reflect the tragic war years with a slow reminiscence of the opening theme at the very end. A critical commentary by Berkeley expert, Peter Dickinson, is provided.
SKU: BT.EMBZ14407
This volume in Leggierissimo series contains character pieces and dances, most of them transcriptions of piano pieces, though they also include excerpts from the ballets Swan Lake, The Nutcracker and The Sleeping Beauty. This volume in the Leggierissimo series contains character pieces and dances, most of them transcriptions of piano pieces, though they also include excerpts from the ballets Swan Lake, The Nutcracker and The SleepingBeauty.Instrumentation: 3 vl1, 3 vl2, 3 vl3, 2 vlcThe Leggierissmo series - growing repertoire for children's and youth string orchestras (position 1)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 Ausgabe Tchaikovsky: Dreizehn leichte Stücke enthält Charakterstücke und Tänze, die meisten davon ursprünglich für Klavier geschreiben, aber auch Auszüge aus Schwanensee, dem Nussknacker und Dornröschen. Enthaltene Stimmen: 3x Violine 1, 3x Violine 2, 3x Violine 3, 2x Cello.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. Le recueil Tchaikovsky: Treize Etudes Légères contient des piècesde caractère et des danses, transcrites pour orchestre cordes junior, mais également des extraits du Lac des Cygnes, Casse-Noisette, et La Belle au Bois Dormant.Instrumentation: 3 vl1, 3 vl2, 3 vl3, 2 vlc.
SKU: BT.EMBZ14335
The material of this volume consists of the dances most popular in Vienna at he beginning of the 19th century: ländler, écossaises and German dances. They were originally piano pieces, but were certainly performed on all sorts of instruments at social gatherings and in public places of entertainment. This transcription for children's orchestra of these miniature compositions is a modern continuation of the old tradition of their 'transcription'. 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 Ausgabe Schubert: Tänze enthält Tänze, die im Wien des beginnenden 19. Jahhunderts sehr beliebt waren: Ländler, Écossaises und Deutsche Tänze. Enthaltene Stimmen: 3x Violine 1, 3x Violine 2, 3x Violine 3, 2x Cello.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. Le recueil Schubert: Danses rassemble des danses les pluspopulaires Vienne au début il du 19ème siècle. Pièces de musique festive écrites l'origine pour piano, elles ont été interprétées par de nombreux instruments. Transcrites présent pour orchestre cordes junior, ces miniatures raviront musiciens et auditoire.Instrumentation: 3 vl1, 3 vl2, 3 vl3, 2 vlc.
SKU: BT.EMBZ14411
The latest volume in this popular series contains little character pieces and dances (Heroic ballad, Lullaby, Peasant song, Religious song, The Suitor's song, Solveig's song, Peasant dance, etc.), most of which are transcriptions of piano pieces. As in the case of the other volumes in the Leggierissimo series, these works scored for a junior orchestra consisting of 1st, 2nd and 3rd violin and cello can be played in the first position. Der neueste Band der beliebten Serie beinhaltet kleine Charakterstücke und Tänze (Heroischer Gesang, Wiegenlied, Bauernlied, Religiöser Gesang, Lied des Freiers, Solveigs Lied, Dorftanz usw.), die in ihrer Mehrheit Übertragungen von Klavierstücken darstellen. Wie bei anderen Stücken der Leggierissimo-Serie lassen sich die Werke für ein mit 1., 2., 3. Violine und Cello besetztes Kinderorchester in der ersten Lage spielen.
SKU: BT.EMBZ14159
English-German-Hungarian.
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.ST6500S
English.
Get ready to have some fun with this energetic western-style romp! Showcasing a melody that weaves its way through every section, the piece also makes use of open string drones and syncopated rhythms, bringing the country-style flair to life. Outstanding and infectious!
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.ST6500
UPC: 241444414682. English.
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