SKU: AP.49967S
ISBN 9781470658496. UPC: 038081576053. English.
Themes are pliable; they can evolve and exist in more than one time signature. Once Upon a Time Signature is the perfect opportunity for your young musicians to improve their craft by adapting to frequent changes in time. 4/4 to 3/4, and back again, they will rise to the challenge. Count on it! (2:30).
SKU: AP.49967
ISBN 9781470658489. UPC: 038081576046. English.
SKU: CL.RWS-2039-01
A thrilling musical adventure for your young band musicians, Race Against Time is a fast and furious journey with an educational focus on the time signature. Driving in 4/4 time, your students will like the intensity and strength of the musical race. However, they will love their journey through the time tunnel with simple yet effective meter changes. Master educator Robert W. Smith has provided a perfect vehicle to teach and reinforce the time signature in a musically relevant setting.
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: AP.1-ADV14279
ISBN 9783954810208. UPC: 805095142792. English.
One of the most popular tunes of all time is Take Five. Musicians know that it's the 5/4 time that makes it swing. Since Dave Brubeck, more and more musicians have devoted themselves to playing in odd meters. This volume by Mike Rossi and Darius Brubeck enables both beginners and professionals to get into the world of 5/4 and 11/8. The reader can learn more about the origin of this fascinating music and is provided with practical tips as well as numerous etudes for all melodic instruments.
SKU: AP.33712S
UPC: 038081394527. English.
As the title suggests, this fun grade 1.5 piece features ever-changing time signatures that will intrigue and challenge the young string orchestra. There are four mood shifts in the piece, suggested by a student narrator who stands up and declares simply Once upon a time, Suddenly, Luckily, and Happily ever after. But what, exactly, is the story? That's up to your students and your audience to decide! This charming piece is simple rhythmically and note-wise, but a great way to get your orchestra counting. Sure to spark everyone's imagination! This title is available in MakeMusic Cloud.
SKU: BT.DHP-1074419-400
ISBN 9789043154185. 9x12 inches. English-German-French-Dutch.
The pieces in Concert Time are fun and varied: they have been written in diverse styles, and different time signatures are featured. The piano accompaniments are included, especially for live performances. The accompaniments are also on the CD - played on a real grand piano. There is a demo version of each piece as well. This book will undoubtedly lead to success on stage! De voordrachtstukken in Concert Time, gecomponeerd door hedendaagse componisten, bieden speelplezier en variatie: ze zijn geschreven in diverse stijlen en er komen verschillende maat- en toonsoorten aan bod. De pianobegeleidingenzijn meegeleverd, speciaal voor liveoptredens. Ze staan ook op de cd, verder is er van elk stuk een voorbeeldversie te beluisteren. Dit boek leidt ongetwijfeld tot succes op het podium! Inhoud: Chameleon Walk Jolly JumperSentimental Tune Baroque Concertino e.a.Die Stücke in Concert Time bieten durch eine Vielfalt an Stilen sowie unterschiedliche Takt- und Tonarten Abwechslung und groÃ?en Lerneffekt. Komponiert wurden die 13 Stücke von zeitgenössischen Komponisten, wie Otto M. Schwarz, André Waignein, Bertrand Moren, Ferrer Ferran u. a. Die Auswahl der Stücke ist sorgfältig auf das Instrument abgestimmt. Die gerade für Live-Auftritte nützlichen Klavierbegleitungen sind im Buch enthalten. Es gibt sie auÃ?erdem auch auf der CD, auf einem echten Flügel aufgenommen. Zusätzlich sind Demoversionen aller Stücke zu hören. Dieses Buch führt auf direktem Wege zum Bühnenerfolg!Concert Time contient des pièces divertissantes et variées écrites par cinq compositeurs européens. Différents chiffrages de mesure, styles et tonalités sont représentés. Cet ouvrage propose un accompagnement de piano (version papier) inclus dans le recueil ainsi quâ??un accompagnement sur compact disc, interprété au piano queue. Les versions intégrales vous serviront de guide. Concert Time en « live », câ??est le succès assuré ! I brani di Concert Time sono variegati e divertenti: sono scritti in diversi stili, e sono proposti in ritmi diversi. Le parti del piano sono incluse per permettervi di suonare in pubblico. Sul CD sono registrati gli accompagnamenti di un vero piano a coda. Troverete una versione demo di ogni brano. Questa pubblicazione è indispensabile per trovare il successo sul palco.
SKU: CF.CPS132F
ISBN 9780825888403. UPC: 798408088408. 9x12 inches.
This piece begins with a long bell striking constant quarter notes, setting up the fast-paced introduction. As the title implies, Time Shift switches rhythmic feels, including a 3 against 2 with changing meters throughout. Its middle section uses segmental chorales, reminiscent of famous band works, before moving back into a quicker time signature. Time Shift is filled with a variety of styles, which create a great amount of interest throughout the work.
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