Matériel : Partition
SKU: CL.012-3872-75
Composer Robert W. Smith has enjoyed his sojourns in the great state of Texas each summer since 1985. In a recent visit to the southwest with his family, he was inspired to sketch three impressions of the Lone Star State. Desert Dawn opens the work with Native-American overtones depicting the warmth of the sunrise over a beautiful southwestern vista. Anyone ever visiting San Antonio will delight in the Paseo Del Rio depicting the light and lively Riverwalk of this great city. The energetic and powerful Longhorns concludes the work with a sense of joy while celebrating this uniquely American way of life. Suitable for concert and festival performance, Southwest Summer will be a valued addition to your next program.
SKU: CL.012-3872-01
SKU: AP.49110
ISBN 9781470646301. UPC: 038081564661. English.
Where the Heavens Meet Earth is a beautiful, lyrical work for young band. Featuring flowing melodic lines and a beautiful four-note motive that transfers throughout the ensemble, the piece is a perfect mid-program work to feature the colors of the different instrumental sections, permitting opportunities to teach about blend and balance within the group. This original Jeremy Bell piece was inspired by the picturesque salt flats in Bolivia called Salar de Uyuni. Located in the Southwest near the Andes, the flats were formed by the transformations of several prehistoric lakes. With variations in elevation that average around a meter, the extreme flatness following a rain turns the 80-mile landscape into the world's largest mirror, reflecting the sky above. (3:30).
SKU: CL.012-4523-01
Red River Station is a bright and upbeat work emulating the style popularized by the soundtrack of the great American west. After the Civil War, cattle drives from Texas to Kansas included a stop at Red River Station along the Chisholm Trail, just before leaving Texas. The syncopated rhythms and pentatonic melodies bring to the life the vibrant and beautiful landscape and experience of riding horseback through the southwest. The energetic and inventive orchestration and exciting nature of this work make it an excellent fit for any concert, and a great contest or festival selection.
SKU: CL.012-4523-75
SKU: AP.49110S
ISBN 9781470646318. UPC: 038081564678. English.
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.14030975
ISBN 9788759860199.
Work for Chamber Ensemble dating from 1989. The composer writes: The Title SHADOWLAND refers on the one hand to a blurred 'Landscape' of shadows, where small shadows are formed behind other shadows, and where the outlines are constantly disintegrating. On the other hand, the title refers to the fanciful and unreal landscapes I felt in the music while I was writing it. SHADOWLAND has four movements, with proportions 4-7-4-3. These proportions can be found on various levels, from the smallest cell to the largest form. The first movement is divided into four parts which have exactly the same proportions as the whole pjece, and behind the fastrunning melodies and trills that dominate the whole movement one can hear, in the second, third, and fourth parts, anticipations of the second, third and fourth movements respectively. The second movement begins at the edge of silence with almost unperceptible glissandi and indistinct chorales. Gradually the hushed landscape is drowned out by sudden expressive melodic outbursts and ends with violent dance rhythms. The third movement is built up of clouds of staccato tones and is a further development of the pointillistic ideas from CLAIROBSCUR. In th last movement the horn plays a long soloistic melody line which the other instruments imitate and echo. These echoes swamp the horn line from time to time. SHADOWLAND was commissioned by and dedicated to The London Sinfonietta.
SKU: HL.44005177
UPC: 073999485738. 8.5x11 inches.
The southwestern U.S. state of Arizona has more than its fair share of stunning landscapes, natural phenomena and national monuments. It has, not surprisingly, been featured as the backdrop to many film Westerns. Best known is the Grand Canyon, but there are also numerous deserts, a petrified forest, extinct volcanoes and the huge Sunset Crater.
SKU: AP.49971
ISBN 9781470658441. UPC: 038081576008. English.
Rio Bravo draws on artifacts of iconic western film music to portray the rugged landscape surrounding one of the longest, most fabled rivers in North America. The challenging, arid region along the brave river that divides Mexico from the southwestern United States---depicted in many a song and story---is characterized by mountains, canyons, and desert plains. The river, known north of the border as the Rio Grande, has called to itself settlers, cattle drivers, gunslingers, and outlaws. Rio Bravo transports listeners to a time and place where legends of the Old West were made! (3:00).
SKU: AP.49971S
ISBN 9781470658458. UPC: 038081576015. English.
SKU: CF.CAS149F
ISBN 9781491163153. UPC: 680160921904. Key: G major.
This exciting piece will help orchestra students soar to new heights! The brisk, consistent tempo will keep all players engaged as they alternate playing the two main themes. Light staccato accompaniments offer the opportunity to practice a brushed bow stroke, and Violin I and Bass sections will encounter some easy shifting. Accented syncopation with ties across the bar are performed in all sections, perfect for refining subdividing skills. This piece was inspired by the sight of a majestic falcon flying effortlessly over the scenic landscape of the Blue Ridge Parkway in Virginia.
About Carl Fischer Concert String Orchestra Series
Thi s series of pieces (Grade 3 and higher) is designed for advancing ensembles. The pieces in this series are characterized by:
SKU: CF.CAS149
ISBN 9781491162811. UPC: 680160921560. Key: G major.
SKU: ST.Y224
ISBN 9790220221552.
Scen es from Welsh life and landscape are a frequent source of inspiration for the music of Rhian Samuel, and, in Dovey Junction, the joyful atmosphere of families en route to the Welsh seaside via the little west-coast railway line is the cue for a crackling scherzo for brass quintet. A snappy rondo theme insists on dressing up in a different texture each time it returns. In between, pithy staccato phrases for trumpets are the setting for more cantabile figures from horn and trombone, and a brief and bluesy episode for muted solo trumpet suggests lazy days on the beach, or grown-up nostalgia for holidays long past. But the energy and sense of expectation remain unstoppable from the first bar to the last, and all five instruments sweep the music into a furious coda that ends the work in riotous high spirits. Dovey Junction was written for performance by Borealis Brass (Alaska) at the UNESCO World Forum on Music, Los Angeles, USA in October 20005, at the invitation of the Fondazione Adkins Chiti: Donne in Musica, (Rome).
SKU: HL.4003160
UPC: 884088651367. 10.0x14.0x0.236 inches.
Free Running is an exciting, high velocity tour-de-force that will keep both musicians and the audience on the edge of their seats. Inspiration for the work came from the pointillistic paintings of Seurat (who created images by using tiny spots of primary colors on his canvas) and from Parkour, a form of urban acrobatics in which participants, known as free runners, use the structures of the rural landscape to perform catlike leaps and sprints. The resulting creation is a non-stop piece of music made up of only staccato notes in a constant rhythm moving through different sections of the ensemble. Free Running was commissioned by the Troy University Symphony Band for the 2011 Alabama Music Educators Association Convention. Ideal for concert or festival use, it is guaranteed to leave the audience breathless! Dur: 5:10.
