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: MH.1-59913-064-5
ISBN 9781599130644.
I wrote Galloping Ghosts (A Ragtime March) to conclude a concert of my chamber music in New York City on October 28, 1986. It is the final part of a work called Rags for Divers Players. This work was written to show the variety possible within the standard rag form. I used all the players available for the finale -- two violins, viola, cello, bass, flute, oboe, clarinet, horn, bassoon, and piano. Since this is a rather unusual instrumental combination and not easy to reassemble, I decided to rescore the work for concert band. Galloping Ghosts is written in a standard march form but incorporates many of the syncopations found in ragtime. The uniquely American music called ragtime traces its history to African rhythms brought over by slaves. Over the years this music became welded to European musical forms such as the quadrille and the march. Drums and banjos and the minstrel tradition lent a special flavor, and from all these elements ragtime slowly evolved within the largely unknown black subculture of the late 19th century. In the late 1890's it emerged as a fully developed form in the classic piano solos of Scott Joplin (1869-1917). Joplin's 1899 hit, Maple Leaf Rag, was an overnight sensation and brought ragtime worldwide fame. Ensemble instrumentation: 1 Piccolo, 8 Flute 1 and 2, 2 Oboe, 1 Eb Clarinet, 4 Bb Clarinet 1, 4 Bb Clarinet 2, 4 Bb Clarinet 3, 2 Eb Alto Clarinet, 3 Bb Bass and Bb Contrabass Clarinet, 2 Bassoon 1 and 2, 2 Eb Alto Saxophone 1, 2 Eb Alto Saxophone 2, 2 Bb Tenor Saxophone, 1 Eb Baritone Saxophone, 3 Bb Cornet 1, 3 Bb Cornet 2, 3 Bb Cornet 3, 2 Horn 1 and 2 in F, 2 Horn 3 and 4 in F, 4 Trombone 1 and 2, 4 Bass Trombone, 2 Baritone (B.C.), 2 Baritone (T.C.), 4 Tuba, 1 String Bass, 1 Timpani, 1 Xylophone, 3 Percussion 1, 3 Percussion 2.
SKU: CL.012-4612-01
During the Jazz age of the 1920's, the cat's pajamas referred to anything special, unique or cool. Musically speaking, the image of a cat in pajamas might suggest combining low clarinets (reminiscent of Prokofiev's use of a clarinet to describe the cat in Peter And The Wolf) with a jaunty little tune in ragtime style, adding a few instrumental meows, and you have (what else?): The Cat’s Pajamas: A Felicitous Feline Ragtime Novelty! Audiences and performers will love it from head to tail!
SKU: CL.012-4612-00
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: MH.1-59913-082-3
ISBN 9781599130828.
Fantasia Nova is a suite comprising two concert marches and a slow, middle movement that derives its themes from both marches. Ragtime (composed in early September, 1978) is a new from old sort of piece. Although its tunefulness and harmonies have an old-fashioned character, its structure, development, and orchestration are unusual for a march. In the chorale section (measures 111 - 148) the band director must be very careful in balancing, for each of the elements must come through. More important is that the audience be brought up by this section -- filled with a joyous exaltation; great attention must be paid to sonority and the band must play earnestly. Ragtime stands on its own and may be performed separately. Dreams (composed in late September, 1978) is the traditional march of the two. It is very closely modeled (in structure only) to Sousa's Stars and Stripes Forever. It even includes a tricky piccolo solo, although the accompaniment has a chorale texture, almost like a school alma mater. This march has a patriotic, inspirational sound, because it was composed for the town of Irondequoit, New York -- for a Town March contest held by the town's community concert band. It did not, so far as I know, become the town's march; one can hear the name, Irondequoit, throughout the Trio, for every turn of the melody (in fact, each group of four notes) fits the accent pattern (Ih-RON-dih-kwoit) of the town's name. Parade stands on its own as a complete work and may be performed separately. Ensemble instrumentation: 1 Piccolo, 6 Flutes, 2 1st & 2nd Oboes, 1 English Horn, 1 Eb Clarinet, 3 1st Bb Clarinet, 3 2nd Bb Clarinet, 3 3rd Bb Clarinet, 1 Eb Alto Clarinet, 2 Bb Bass Clarinet, 1 Eb Contrabass Clarinet (optional), 2 1st & 2nd Bassoons, 1 Contrabassoon (optional), 1 1st Eb Alto Saxophone, 1 2nd Eb Alto Saxophone, 1 Bb Tenor Saxophone, 1 Eb Baritone Saxophone, 3 1st Bb Cornets, 3 2nd Bb Cornets, 3 3rd Bb Cornets, 1 1st Horn in F, 1 2nd Horn in F, 2 3rd and 4th Horns in F, 2 1st Trombones, 2 2nd Trombones, 2 3rd Trombones, 1 Euphonium (Treble Clef), 2 Euphonium (Bass Clef), 4 Tuba, 1 String Bass, 1 Timpani (Triangle), 5 Percussion.
SKU: AP.39609S
UPC: 038081454702. English.
This lively, nostalgic piece will musically transport players and audience alike to the iconic amusement parks of turn-of -the-century Coney Island (near Brooklyn, New York). The sweet, cheerful sounds that flowed from the carousels and bandwagons of a time gone by infuse this characteristic, but level-appropriate work. Ragtime feel is achieved via accessible syncopations, chromatics that lay well on the instruments, and sectional form. Novel percussion, including a slide whistle, adds to the fun! (2:35).
SKU: HL.4005510
UPC: 888680745936. 9.0x12.0x0.07 inches.
This composition reflects a colorful time in American history and is an opportunity for your band to discover ragtime rhythms. Folk hero Billy Miner (the Grey Fox) was the last of the old-time bandits. He was noted for his unusual politeness and is believed to be the originator of the phrase, Hands up! This composition is like a mini movie score and starts with the Billy Miner ragtime theme, followed by a train robbery, his capture, and final release. The artful interplay between sections gives this piece the sophisticated sound and intensity of a much more advanced work. Dur: 3:35.
SKU: CL.011-2555-00
Feature your young F Horn or Alto Saxophone sections with this original ragtime piece by Wisconsin composer, Brian Olson. Skillfully arranged to help your young students attain a genuine ragtime feel.
About C.L. Barnhouse Command Series
The Barnhouse Command Series includes works at grade levels 2, 2.5, and 3. This series is designed for middle school and junior high school bands, as well as high school bands of smaller instrumentation or limited experience. Command Series publications have a slightly larger instrumentation than the Rising Band Series, and are typically of larger scope, duration, and musical content.
SKU: AP.47409
UPC: 038081547084. English.
A 1930s retro-style animation soundtrack that pays homage to ragtime jazz music and the early days of animated cartoons. One of the most popular action-packed video games today, it's fun to play and certainly will excite your students and audience. (3:15).
