SKU: FJ.ST6189S
English.
The magical setting of this cherished melody combines exquisite orchestration with dramatic harmonies. At times, the arrangement is quite plaintive sounding, which is balanced with more contemporary harmonies and powerful countermelodies. Endless opportunities for music making abound, and there certainly will not be a dry eye in the house when the group plays the final chord after a haunting violin solo. Inspirational!
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: 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: XC.RSO2006
UPC: 812598034578. 9 x 12 inches.
Strollin’ is a charming new work for String Orchestra, utilizing syncopation in 6/8 time. Written as a contemporary jazz piece, every voice is balanced with the other making this a great piece to reinforce tutti play and blend. We know you and your audiences will love Strollin’.
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: FJ.ST6432S
A rocking celebration of the season! Set in first position with simple rhythms and no slurs, this contemporary arrangement includes the familiar carols Deck the Hall, Hark, the Herald Angels Sing, and Ding, Dong, Merrily On High. Every section of the orchestra is featured and the energetic cello/bass groove is driven by optional drum set and sleigh bells. An exuberant finale for your holiday concert!
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: FJ.ST6350S
Add a unique programming twist with this fantastic piece that blends humor with darkness. The spooky opening uses playable chromatics to set the stage for the thing, which comes across as potentially scary, yet clumsy and whimsical all at the same time. If you are looking for something fun and completely different, you just found it!
SKU: FJ.ST6549
Written to celebrate an amazing orchestra teacher's retirement, this piece strives to capture the joyful things, the emotional, loving, and supportive things - literally All the Things. Opening with a gentle chorale, the music moves from a warm embrace to a rollicking groove based on fiddle music and more. Highly energetic and emotional, this piece will leave you with joyful tears and have a profound impact on your students and audience.
SKU: FJ.ST6549S
SKU: KJ.SO154F
Ms. Atwell has added a unique sparkle to the carol, We Three Kings. Giving all sections of the orchestra a chance to play the melody, this is a true performance piece that offers experienced orchestras a rich ensemble experience.
SKU: XC.ISO2209
12 x 9 inches.
In an attempt to musically capture that creepy feeling of walking in the Dark, Composer Bud Woodruff brings us a spooky new work for String Orchestra. Perfect for that first Fall Concert!
SKU: XC.ISO2209FS
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