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: BT.DHP-1094713-070
ISBN 9789043131919. 9x12 inches. English-German-French-Dutch.
The De Haske String Orchestra Series offers attractive pieces especially composed and arranged for string orchestras. Students and teachers are treated to a great variety of musical styles. Each part presents a challenge to the player. The Viola part can be replaced by a 3rd Violin part, and the Double bass part can be replaced by a 2nd Cello part. The Piano part is mainly meant for support, but it occasionally adds new motifs as well.
Classical Highlights is a collection of six arrangements of classical themes dating from 17th to 19th century. The parts have been kept easy and attractive; at the same time they stay close to the original.De De Haske String Orchestra Series biedt u aantrekkelijke, speciaal voor strijkorkest gecomponeerde en gearrangeerde werken. De stukken zijn geschreven in verschillende stijlen: van klassiek en folk tot moderne, populaire muziek. Iedere partij is zo geschreven dat elke speler in het orkest een uitdaging heeft. De partij voor altviool kan door een derde viool worden vervangen. De partij voor contrabas kan ook door een tweede cello worden gespeeld. De pianopartij dient als ondersteuning, maar voegt soms ook nieuwe motieven toe aan de muziek.
Classical Highlights is een verzameling arrangementen van klassieke thema’s die dateren uit de 17e tot en met de 19e eeuw. De partijen zijn eenvoudig en aantrekkelijk geschreven: tegelijkertijd blijven de arrangementen dicht bij het origineel. Die De Haske String Orchestra Series bietet attraktive, speziell fu r StreichÂorchester komponierte und arrangierte Stu cke in einer stilistischen Vielfalt von Klassik u ber Folk bis zu modernen U-Musikstilen. Jede Stimme stellt dabei besondere Herausforderungen an die Spieler. Die Violastimme kann durch eine dritte Violine und der Kontrabass durch ein zweites Cello ersetzt werden. Die Klavierstimme dient zur Unterstu tzung, fu gt aber zuweilen auch neue Motive hinzu.
Classical Highlights enthält Bearbeitungen von sechs klassischen Themen aus der Zeitspanne vom 17. bis zum 19. Jahrhundert. Die Stimmen wurden einfach und ansprechend gestaltet und sinddoch zugleich getreu dem Original. Die Ausgabe enthält ein Rigaudon von Henry Purcell, das berühmte Menuett aus der Feuerwerksmusik von Händel, ein Andante von Haydn (das Thema mit dem berühmten Paukenschlag), das Thema aus Beethovens Violinkonzert, Das große Tor von Kiew aus Bilder einer Ausstellung von Modest Mussorgsky und schließlich noch España von Waldteufel und Chabrier. De Haske String Orchestra Series : Les compositions et les arrangements réunis sous ce label sont en parfait accord avec le niveau ciblé, et proposent des styles très variés. Chaque publication est accompagnée d'un compact disc contenant la version de démonstration des œuvres publiées dans cette collection. L’instrumentation est toujours la même : Violons 1 & 2, Alto (ou Violon 3), Violoncelle, Contrebasse (ou Violoncelle 2) et Piano.
Classical Highlights est un recueil qui réunit six arrangements de grands thèmes classiques du XVIIe au XIXe siècle. Les parties sont motivantes et facilement accessibles, explorant avec justesse l’oeuvreoriginale. De Haske String Orchestra Series è una nuova raccolta pensata per i suonatori di archi principianti. Le composizioni e gli arrangiamenti raccolti sotto questa etichetta sono perfetti per chi inizia a suonare e prongono stili variegati. La strumentazione è sempre la stessa: violino 1 & 2, viola (o violino 3), violoncello, contrabbasso (o violoncello 2) e piano.Classical Highlights è una pubblicazione che raccoglie sei arrangiamenti di grandi temi classici del XVII e XIX secolo. Brani motivanti e facilmente accessibili, che rendono onore all‘originale.Tracce Demo:1. Rigaudon2. Minuet3. Andante4. Allegro5. Great Gate of Kiev6. EspanaPer effettuare il download delle tracce demo, clicca sul titolo selezionato e scegli “Salva come†nel menu.
SKU: CF.YAS19
ISBN 9780825854859. UPC: 798408054854. 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 patters 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 B 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.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 yetA legato feel. A spirited introduction features an opening melody in the violins and active repeated-note pedal patters 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 B 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 powerfulA divisi voicing on beat 3 of m. 63, right before the final chord.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 patters 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 B 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.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 patters 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 B 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
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