SKU: CL.011-4376-01

Make no bones about it - this mysterious sounding novelty piece is sure to lift your audience’s spirits! Optional use of whirly tubes will add a haunting effect that your performers and audience will remember long after the concert! Sure to be a performance favorite!

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: HL.44001921

UPC: 073999819113. 6.75x10.5 inches.

Rudolph the Red Nosed Reindeer told the story of Rudolph, a young reindeer who was teased by the other deer because of his large, glowing, red nose. But, when Christmas Eve turned foggy the former outcast saved Christmas by leading the sleigh by the light of his red nose. This version for concert band by Naohiro Iwai is perfect as a cheerful interlude and will soon find a firm place in your Christmas repertoire.

Rudolph the Red Nosed Reindeer told the story of Rudolph, a young reindeer who was teased by the other deer because of his large, glowing, red nose. But, when Christmas Eve turned foggy the former outcast saved Christmas by leading the sleigh by the light of his red nose. This version for concert band by Naohiro Iwai is perfect as a cheerful interlude and will soon find a firm place in your Christmas repertoire.

Rudolph, das rotnasige Rentier aus Nordamerika, das zuerst von seinen Artgenossen nur ausgelacht wird, dann aber als Zugtier fur den Schlitten vom Weihnachtsmann Karriere macht, erfreut sich mittlerweile auch in Europa grosser Beliebtheit. Die gelungene Blasorchesterbearbeitung des lustigen Liedes von Naohiro Iwai sorgt fur frohliche Stimmung und wird sich schnell einen festen Platz in Ihrem Weihnachts-konzertrepertoire erobern.

Parmi les rennes du Pere Noel, il en est un pas comme les autres : il s'appelle Rudolph et a un nez rouge. Il est ne de l'imaginaire du poete Robert L. May, un soir de 1939. Son histoire fera le tour du monde et enchantera des generations d'enfants. La musique est lumineuse et joyeuse. Un standard de Noel !

Tra le renne di Babbo Natale c'e ne e una diversa dalle altre: si chiama Rudolph ed ha il naso rosso. E' nata dall'immaginazione del poeta Robert L. May, una sera del 1939. La sua storia fara il giro del mondo e deliziera intere generazioni di bambini. La musica e luminosa e gioiosa. Un vero piacere per esecutori e pubblico!

SKU: BT.DHP-0920412-140

Rudolph the Red Nosed Reindeer told the story of Rudolph, a young reindeer who was teased by the other deer because of his large, glowing, red nose. But, when Christmas Eve turned foggy the former outcast saved Christmas by leading the sleigh by the light of his red nose. This version for concert band by Naohiro Iwai is perfect as a cheerful interlude and will soon find a firm place in your Christmas repertoire.

Rudolph, das rotnasige Rentier aus Nordamerika, das zuerst von seinen Artgenossen nur ausgelacht wird, dann aber als Zugtier für den Schlitten vom Weihnachtsmann Karriere macht, erfreut sich mittlerweile auch in Europa großer Beliebtheit. Die gelungene Blasorchesterbearbeitung des lustigen Liedes von Naohiro Iwai sorgt für fröhliche Stimmung und wird sich schnell einen festen Platz in Ihrem Weihnachts-konzertrepertoire erobern.

Parmi les rennes du Père Noël, il en est un pas comme les autres : il s’appelle Rudolph et a un nez rouge. Il est né de l’imaginaire du poète Robert L. May, un soir de 1939. Son histoire fera le tour du monde et enchantera des générations d’enfants. La musique est lumineuse et joyeuse. Un standard de Noël !

Tra le renne di Babbo Natale c’e ne è una diversa dalle altre: si chiama Rudolph ed ha il naso rosso. E’ nata dall’immaginazione del poeta Robert L. May, una sera del 1939. La sua storia far il giro del mondo e delizier intere generazioni di bambini. La musica è luminosa e gioiosa. Un vero piacere per esecutori e pubblico!

SKU: BT.PWM4901

Concerto for String Orchestra - the magnum opus of Grayna Bacewicz (1909-1969), the outstanding composer and violinist - was composed in 1948 and at once became one of the most frequently performed works of this Polish artist. This masterpieceof neoclassicism fascinates as much by its invention and virtuosic briliance as its harmonious combination of formal elements of a traditional nature with new tonal ideas. The form of the three-movement Concerto oscillates between that of the baroqueconcerto grosso and the early classical sonata cycle. The neoclassical tendency is evident, above all, in the articulation of the musical structure in keeping with the rigours of periodicity and the manner of developing thematic threads derived fromthem, while the concertato character of particular movements and the generally linear texture indicate baroque connections. The first movement (Allegro) - in the form of an early classical sonata allegro - begins with a subject with energeticfigurations, emblematic for the whole piece and based on a constant, pendulum-like semiquaver movement anchored securely on D. It is precisely because of the nature of this subject that Bacewiczs work has been compared to the Brandenburg Concertosby Jan Sebastian Bach The second movement (Andante), while retaining its concertato charakter, is, at the same time, an example of the composers ability to create emotionally serene lyrical moods, and her sense of cantilena derived from the spiritof romantic song (a motto-subject presented at the beginning by cello solo). In this movement it is both the process of evolution and the instrumental colouring which constitute the constructional agents forming here a self-containedvalue. In thethird movement (Vivo) the composer returns to her favourite type of music, understood as an expression of pure motion in the form of figural motives with infinite transformational possibilities. The spontaneity of the music, the constant mutabilityof the tonal situations, and the sophisticated, acerbic harmonies - as Witold Lutosawski described them - form a colourful mosaic built in the structural skeleton of a sonata rondo. Concerto for String Orchestra is not only proof of thestylizing tendency of the composer but also of an unerring intuition concerning the technical and expressive possibilities inherent in a string instruments ensemble. [Magorzata Gsiorowska, translated by Ewa Cholewka].

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: HL.49045925

ISBN 9783795712662. UPC: 888680826222. 6.0x9.0x0.19 inches.

Re-edited with a detailed preface by Wolfgang Birtel. The famous Symphonic Poem from 1984: Death plays a dance tune, the skeletons rise from their graves and dance an eerie dance to the music until the crowing of the cock puts an end to the macabre.

SKU: FJ.W9459

UPC: 241444395264. English.

A cheerfully macabre solo with a tempo mark that indicates with bones rattling! In A minor, this pedagogical piece with sequential five-finger patterns explores the lower range of the piano with an 8vb. Legato and staccato touches are juxtaposed, and putting hands together is easy. Great teaching material.