The Rock Canyon

SKU: CL.011-3763-01

Here is wonderful program music for young bands suggesting the imagery of wild horses roaming free in the Red Rock canyons of Utah. Interesting parts abound, with unison and independent lines for all players. The short opening fanfare sets the stage for the brisk allegro section. A short interlude leads to a lyrical section for the woodwinds and low brass. A new transitional fanfare leads us back to a recap of the main themes. An inspiring concert or festival selection!

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: 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: KN.19920

UPC: 822795199208.

Inspired by the world-famous canyon in southwestern Utah, where thousands of brightly-colored hoodoos (odd-shaped pillars of rock left standing from the forces of erosion) greet visitors, the dynamics in this bold presentation range from p to fff in the final bar. Snare drum rolls are intentionally limited to 9 and 17 strokes for developing players. Duration 2:16.

SKU: CF.CAS53F

ISBN 9780825869778. UPC: 798408069773. 8.5 X 11 inches.

About Carl Fischer Concert String Orchestra Series

This series of pieces (Grade 3 and higher) is designed for advancing ensembles. The pieces in this series are characterized by:

• Expanded use of rhythms, ranges and keys but technical demands are still carefully considered
• More comprehensive bowing techniques
• Viola T.C. included
• Careful selection of keys and degree of difficulty for advancing musicians

SKU: BT.AMP-011-140

This piece depicts the refined beauty of the Grand Canyon at sunrise and sunset. These are the best times to view the Canyon with the sun low in the sky casting shadows that give depth and form to the vast panorama. Angel’s Gate is one of the many named rock formations in the canyon. The composer has tried to depict the sights and sounds of dawn, birdsong in the early morning sky and the gradual revelation of the Canyon itself as sunlight reaches into its rocky depths.Towards the end of the piece, to the sound of a tolling bell, we are however reminded of the dangers that the beauty of the Grand Canyon so cleverly hides.

SKU: MB.WBM76M

ISBN 9781736363096. 8.75x11.75 inches.

This comprehensive book contains the solos found in five William Bay guitar solo collections.á The solos range from colorful foot tapping reels, breakdowns, hornpipes, jigs, fiddle tunes and sea chanteys to country and Celtic ballads and waltzes.á Also included are numerous original guitar solos.á All 143 solos in this collection are recorded by the author and online access to the recordings is included. All solos are presented in notation and tablature.

SKU: PR.466000470

UPC: 680160099405. 11 x 17 inches.

This is the second incarnation of a work I first composed in 1994 for symphonic wind ensemble. The earlier version was intended to be the summation of three-part suite, each part being named for a different national park in the Western United States. This orchestral version, commissioned in 1999 by the Utah Symphony and dedicated to the memory of Aaron Copland, is more than a re-scoring of the earlier piece; it is a re-thinking of all its elements. Zion is a place with unrivaled natural grandeur, being a sort of huge box canyon in which the traveler is constantly overwhelmed by towering rock walls on every side of him -- but it is also a place with a human history, having been inhabited by several tribes of native Americans before the arrival of the Mormon settlers in the mid-19th century. By the time the Mormons reached Utah, they had been driven all the way from New York State through Ohio and, with tragic losses, through Missouri. They saw Utah in general as a place nobody wanted, but they were nonetheless determined to keep it to themselves. Although Zion Canyon was never a Mormon Stronghold, the people who reached it and claimed it (and gave it its present name) had been through extreme trials. It is the religious fervor of these persecuted people that I was able to draw upon in creating Zion as a piece of music. There are two quoted hymns in the work: Zion's Walls (which Aaron Copland adapted to his own purposes in both his Old American Songs and the opera The Tender Land) and Zion's Security, which I found in the same volume in which Copland found Zion's Walls -- that inexhaustible storehouse of 19th-century hymnody called The Sacred Harp. My work opens with a three-verse setting of Zion's Security, a stern tune in F-sharp minor which is full of resolve. (The words of this hymn are resolute and strong, rallying the faithful to be firm, and describing the city of our God they hope to establish). This melody alternates with a fanfare tune, whose origins will be revealed in later music, until the second half of the piece begins: a driving rhythmic ostinato based on a 3/4-4/4 alternating meter scheme. This pauses at its height to restate Zion's Security one more time, in a rather obscure setting surrounded by freely shifting patterns in the flutes, clarinets, and percussion -- until the sun warms the ground sufficiently for the second hymn to appear. Zion's Walls is set in 7/8, unlike Copland's 9/8-6/8 meters (the original is quite strange, and doesn't really fit any constant meter), and is introduced by a warm horn solo. The two hymns vie for attention from here to the end of the piece, with the glowingly optimistic Zion's Walls finally achieving prominence. The work ends with a sense of triumph.

SKU: AP.49072S

ISBN 9781470647797. UPC: 038081567013. English.

This multi-level piece includes a full set of parts for grade 1 as well as a full set for grade 2 ensembles. Mix and match the parts as you need---perfect for mixed-ability ensembles!

Representing one of Mark Wood's favorite places to visit, Arizona Sun was inspired by the sheer beauty and power of the American southwest, specifically that of the Grand Canyon State. The work is in the key of A major, and based on a traditional blues progression that can be found in early rock and roll. Arizona Sun features two sections that allow the players to improvise. For string orchestra with optional rock rhythm section parts. (3:00)

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