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: CL.012-4874-01
Composer James Reese Europe, one of the most famous African-American musicians of his day, was called the Martin Luther King of music by pianist Eubie Blake. The first African-American bandmaster in the United States Army, Europe gained great popularity as a dance band leader, a military band leader, recording artist, and a composer of merit. Known in New York music circles, and also for touring Europe with his National Guard band, Europe is remembered today for composing several works, including Castles In Europe with the subtitle The Innovation Trot - Ragtime March. This delightful work is arranged for todayâ??s concert band by Chandler L. Wilson. An enjoyable ragtime work from an American composer to be remembered!
SKU: SU.28120010
Ballet Suite in 5 movements (revised version)3222; 4331; timp, perc, hp, pno; stgs Duration: 24' Composed: 2008 Published by: Alla Pavlova Music Although it maintains the charm of the original Hans Christian Andersen tale, Alla Pavlova's Thumbelina is a considerable musical, visual and narrative expansion of the story to make it suitable as a full-length ballet and family-programming alternative to The Nutcracker. Musically, it is scored for full symphony orchestra ([3,2,2,2]-[4,3,3,1]-[timp.,perc.]-[Hp]-[Strings], Percussion: Bass dr., Snare dr., Wooden Block, Tambourine, Triangle, Glock., Vibraphone, Celesta) and contains not only many beautiful, lyrical and moving waltzes and other classical themes, but also rhythms such as tango, boogie-woogie and ragtime. Narratively, the story has been adapted to include a varied and colorful cast of characters. The Thumbelina Suite (which has been recorded by the Tchaikovsky Symphony Orchestra for Naxos) can be heard at http://www.allapavlova.com/listen.html or by clicking on the image below. She has created a synopsis of the ballet, which is of course based on the Andersen fairy tale. We’ll gladly send this synopsis on request. Recording: 21st Century Classics – Naxos 8.579003 Performance materials available on rental only:.
SKU: AP.45874
UPC: 038081523774. English.
Here's a fun, jazzy, all-pizzicato selection for early beginners to play at one of their first concerts! Built around a strong, steady beat, this original by Doug Spata uses only the D and A strings, and half, quarter, and eighth notes with very limited independence to keep everyone together. Each section gets a melody, making it the perfect way to show off those beginning skills. (1:40).
SKU: AP.45874S
UPC: 038081523781. English.
Here's a fun, jazzy, all-pizzicato selection for early beginners to play at one of their first concerts! Showtime Rag is built around a strong, steady beat. This original by Doug Spata uses only the D and A strings, and half, quarter, and eighth notes with very limited independence to keep everyone together. Each section gets a melody, making it the perfect way to show off those beginning skills. (1:40).
SKU: AP.38488S
UPC: 038081434681. English.
Inspired by ragtime, this arrangement celebrates Claude Debussy's 150th birthday. Lively and fun to play, this piece offers the chance to explore various dynamic changes and accented playing.
SKU: AP.38488
UPC: 038081434674. English.
SKU: AP.31627S
UPC: 038081354026. English.
Join the celebration of the 50th anniversary of the annual string teachers' workshop in Birch Bay, Washington with this two-movement commemoration. The piece develops musical style and provides a great challenge! First presenting a tender and wistful folksong, and then moving to a rousing, virtuosic, fiddle-tune meets ragtime feel, this energetic romp is a non-stop workout that your students will love to play, practice and perform! This title is available in MakeMusic Cloud.
SKU: CL.012-4559-75
Mark Twain's colorful characters come to musical life in A Tom Sawyer Portrait! The journey begins in St. Petersburg, Missouri, with a jaunty musical portrayal of Tom and Huck and a ragtime sequence which depicts the sleepy river town. An Americana-style ballad follows that is tender, lyrical and poignant. This segues into a no holds barred blues section representing the mighty Mississippi. The Portrait concludes with our heroes' return, featuring a recap of the opening theme augmented in the brass and accompanied by woodwind runs and exciting percussion. This is a great selection for the concert band that demands solid musicianship but will reward students for their efforts!