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: CF.CAS29
ISBN 9780825860959. UPC: 798408060954. 8.5 X 11 inches. Key: C major.
A programatic work by composer Doris Gazda that sets out to depict the historic moon landing by the Apollo 11 astronauts and the famous first step by Neil Armstrong. A sound portrait of this remarkable event in America history.In July, 1959 the world watched and listened as the astronauts of Apollo 11 traveled from the Earth to the moon. The mission, launched by NASA, successfully carried men to the surface of the moon and returned them safely to earth. The spaceship was made up of a command module, Columbia, and a lunar module, Eagle. Astronauts Neil Armstrong, flight commander, and Buzz Aldrin, pilot of the lunar module, actually walked on the moon. The third astronaut, Michael Collins, piloted Columbia, the command module that orbited the moon while Armstrong and Aldrin were on the lunar surface.The 238,000-mile trip to the moon took four days. Apollo 11 fell into orbit 60 miles above the moon's surface. The Eagle separated from Columbia, orbited the moon nine miles above the surface and then made a powered descent, touching down on the moon in the Seat of Tranquility. Six hours after landing, Armstrong stepped onto the moon's surface uttering these memorable words that brought to reality the possibilities of space travel and exploration, That's one small step for man, one giant leap for mankind.Armstrong and Aldrin spent two hours walking on the lunar surface. They set up some scientific equipment, raised an American flag and left a plaque signed by the Apollo 11 crew and President Richard Nixon, reading:Here men from planet earth first set foot upon the moon. July 1969 A.D. We came in peace for all mankind.Twenty-one hours after landing, the Eagle with Armstrong and Aldrin onboard, left the moon to reunite with Columbia. After docking successfully, all three men got into Columbia. They jettisoned the Eagle and Columbia left lunar orbit to make the return trip. Two days later Columbia re-entered the Earth's atmosphere and splashed down in the Pacific Ocean.
SKU: CF.YAS1
ISBN 9780825840630. UPC: 798408040635. 8.5 X 11 inches. Key: G major.
Moonlight Shadows is a passionate and colorful piece for strings that explores the expressive power of the string orchestra. Sean O'Loughlin uses a lush harmonic palette and variety of texture (including a short pizzicato section), to create an important and soulful addition to the repertoire for younger string ensembles. Duration: 2'30.Moonlight Shadows is a work for string orchestra that reflects my great love for the music of Samuel Barber. His compositions from the 1930s and 1940s were characterized by plush harmonies, flowing melodies and engaging suspensions. These elements are what I focused on in the composition of Moonlight Shadows.The material represents my mood and feelings when I look at a big, bright moon. The shadows it casts create an eerie feeling, while at the same time providing a deep, rich tapestry for the earth at night.The harmony features many major seventh-chords with half-step suspensions. These suspensions function as common tones to the next chord and create the tension of the piece. They also move, in order to provide resolution to the piece which allows the listener to rest. With this in mind, these suspensions should be brought out during performance.Moonlight Shadows is an emotional piece that allows the young musician the opportunity to play with much expression.
About Carl Fischer Young String Orchestra Series
This series of Grade 2/Grade 2.5 pieces is designed for second and third year ensembles. The pieces in this series are characterized by:--Occasionally extending to third position--Keys carefully considered for appropriate difficulty--Addition of separate 2nd violin and viola parts--Viola T.C. part included--Increase in independence of parts over beginning levels
SKU: FJ.ST6543S
English.
Inspired by the composer's frequent visits to Montana, this musical tribute honors the grand landscapes of the state, including stunning mountain views and clear blue skies. Portraying everything from the breathtaking scenery to massive thunderstorms, this piece is an ideal way to explore the beauty and fury of Earth's towering skies. An optional timpani part adds a great deal to the work.
About FJH String Orchestra
More emphasis on bow technique and independence of lines. For the accomplished middle, high school, college, or professional group. Grade 3 and up
SKU: FJ.ST6543
Inspired by the composer's frequent visits to Montana, this musical tribute honors the grand landscapes of the state, including stunning mountain views and clear blue skies. Portraying everything from the breathtaking scenery to massive thunderstorms, this piece is an ideal way to explore the beauty and fury of Earth's towering skies. An optional timpani part adds a great deal to the work. (3:45).
SKU: FJ.ST6553
This stunning 3-movement work has it all! The opening movement, Flights of Fancy, symbolizes the element of air and features soaring phrases. The second movement, Terra, resembles an Appalachian lullaby and represents the element of Earth. The final movement, Fire and Ice, is a tour de force that captures the elements of fire and water meeting to create steam and the resulting kinetic energy. Glorious music!
SKU: FJ.ST6553S
SKU: FJ.ST6386S
Many fictional works portray the moon as a living being, alone in space looking at the Earth. This lullaby honors this living moon, portraying various emotions including the loneliness of seeing us from space. It also includes moments of comfort as the moon proudly watches over us, much as a parent watches over a child. Simply stunning, whether you have a grade 2 or a grade 6 ensemble.
About FJH Developing Strings
Slightly more advanced than Beginning Strings, this series begins to involve more position work and a slightly more complex rhythmic figures. Rehearsal piano is often provided. Ideal for middle school and smaller high school programs. Grade 2 - 2.5
SKU: XC.ISO2008
UPC: 812598034455. 9 x 12 inches.
After traveling out west in America, composer Tyler Arcari was intrigued by the rugged life of the deserts and canyons. When you stand still, the wind across the flat earth sings an eerie tune. This new soundscape is the composer’s attempt to put this idea into sound!
SKU: XC.ISO2008FS
UPC: 812598034462. 9 x 12 inches.
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