Orchestra String Orchestra - Grade 3

SKU: CF.CAS7

Composed by Doris Gazda. Edited by Amy Rosen. FS-SWs. Carl Fischer Concert String Orchestra Series. Score and Parts. With Standard notation. 20+24+24+6+15+15+15 pages. Carl Fischer Music #CAS7. Published by Carl Fischer Music (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.

By Samuel Augustus Ward. Arranged by Carmen Dragon, adapted by Douglas E. Wagner. Orchestra. Score; String Orchestra. Pop Beginning String Orchestra. 4th of July; Patriotic; Summer. Grade 2.5. 8 pages. Published by Alfred Music Publishing

String Orchestra - very easy

SKU: BT.DHP-1094713-070

Arranged by Nico Dezaire. De Haske String Orchestra Series. Set (Score & Parts). Composed 2009. 24 pages. De Haske Publications #DHP 1094713-070. Published by De Haske Publications (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 Streich­orchester 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.

Composed by David Bobrowitz. Edited by J. Cameron Law. For string orchestra. Grade 3+. Score and set of parts. Duration 4 minutes, 30 seconds. Published by Grand Mesa Music

By Stan Getz and Beaux Arts String Ensemble. By Eddie Sauter. Edited by Rob Duboff, Jeffrey Sultanof, Alex Chilowicz, and Andrew Homzy. Arranged by Eddie Sauter. For string ensemble (score and parts) (Soloist (parts in concert, B-flat, and E-flat), Violin I (8 parts), Violin II (8 parts), Viola (5 Parts), Cello (5 Parts) , Double Bass (3 Parts), Harp, Piano/Celeste, Percussion (Snare Drum, Marimba, Tambourine)). Advanced. Score and parts. Published by Jazz Lines Publications

By Richard Meyer. By Richard Meyer. For String Orchestra. String Orchestra. Highland String Orchestra. Conductor Score & Parts. Published by Alfred Publishing.
Level: 2.5 (grade 2.5).

(Recorded by Meghan Trainor). Composed by Meghan Trainor and Kevin Kadish. Arranged by Victor López. Orchestra. Score; String Orchestra. Pop Intermediate String Orchestra. Pop. Grade 2. 8 pages. Published by Alfred Music

Composed by David Bobrowitz. Edited by J. Cameron Law. For string orchestra. Grade 1+. Score and set of parts. Duration 2 minutes, 20 seconds. Published by Grand Mesa Music

Edited by J. Cameron Law. Arranged by Randall D. Strandridge. For string orchestra. Grade 2+. Score and set of parts. Duration 2 minutes, 30 seconds. Published by Grand Mesa Music

Composed by David Bobrowitz. Edited by J. Cameron Law. For string orchestra. Grade 2. Score and set of parts. Duration 2 minutes, 20 seconds. Published by Grand Mesa Music

(Featuring: America / America the Beautiful / The Star Spangled Banner). Arranged by Jerry Brubaker. Orchestra. Part(s); Score; String Orchestra. Belwin Intermediate String Orchestra. Form: Medley. 4th of July; Fall; Graduation; Light Concert; Patriotic; Summer; Thanksgiving. Grade 2.5. 104 pages. Published by Belwin Publishing

((Awesome Remixxx!!!)). Composed by Shawn Patterson (1965-). Arranged by Ralph Ford. Orchestra. Score; String Orchestra. Pop Intermediate String Orchestra. Movie. Grade 2.5. 12 pages. Published by Alfred Music

(As performed by Video Games Live� (www.videogameslive.com)). By Tommy Tallarico, Michael Plowman, Emmanuel Fratianni, and Laurie Robinson [Video Games Live]. Arranged by Bob Phillips. Orchestra. String Orchestra. Pop Intermediate String Orchestra. Light Concert; Video Game. Grade 2.5. Conductor Score. 12 pages. Published by Alfred Music Publishing

By Cliff Friend, Dave Franklin, Edward Heyman, Dana Seusse, Eddie Cantor, Charlie Tobias And Murray Mencher. Arranged by Douglas E. Wagner. For String Orchestra. String Orchestra. Pop Beginning String Orchestra. Novelty. Conductor Score. 12 pages. Published by Alfred Publishing.
Level: 1.5 (grade 1.5).