So Hallow'd Is the Time

SKU: CL.012-3326-99

For band with optional choir, strings, narrator and audience sing-a-long. This glorious setting of two of America's favorite hymns, Amazing Grace and Battle Hymn of The Republic, is destined to be the work of choice when selecting that special number for your program's grand finale. Playable by band alone, this patriotic arrangement also offers the creative option of adding choir, strings, narrator, bagpiper and even a group sing-a-long. Musically appealing for bands of varied levels, this spectacular production number will offer grateful audiences, young and old alike, a wonderful opportunity to experience the ultimate in listening pleasure. A guaranteed winner!

About Heritage of the March

Full -sized concert band editions of the greatest marches of all time. Each has been faithfully re-scored to accommodate modern instrumentation and incorporate performance practices of classic march style

SKU: CF.SPS71

ISBN 9781491143544. UPC: 680160901043. Key: G minor.

Nordanvind is a tour de force symphonic rhapsody that is built on three Scandinavian folk songs. Composer Carl Strommen has composed these Viking-influenced melodies into a concert setting that brings out all of the history of the Scandinavian people. The piece is at times bold and aggressive, at other times beautiful. Carl employs all of the instrumental colors of the concert band to create a new work for more advanced ensembles.
Modern Scandinavians are descendants of the Vikings, an adventuresome people who were known for their love of the sea, their naval prowess, and as fierce fighters . The Scandinavian Vikings were warriors from Denmark, Norway, and Sweden who traded, raided and settled in various parts of Europe, Russia, the North Atlantic islands, and the northeastern coast of North America .Starting around 1850, over one million Swedes left their homeland for the United States in search of religious freedom and open farm land . Augustana College was founded in 1860 by graduates of Swedish universities and is located on the Mississippi River in Rock Island, Illinois . Home of the “Vikings,” Augustana College is the oldest Swedish- American institution of higher learning in the United States . This powerful and lively piece takes inspiration from Swedish history and from Swedish folk songs and hymns .Havsdrake (Dragon of the Sea)The Nordanvind or “North Wind” blows a cold wind during a journey of a group of courageous Viking rowers . The “Dragon-ship” or long ships designed for raiding and war was a sophisticated, fast ship able to navigate in very shallow water . To musically portray these magnificent seafaring vessels, the director is encouraged to use an Ocean Drum (or a rain stick) during the introduction . Wind players may consider blowing air through their instruments to suggest the North wind . Adding men’s voices to accompany the haunting low brass and percussive “rower” sounds can be helpful in creating the dark and ominous portrayal of Viking adventurers .Slangpolska efter Byss - KalleIn Sweden, a “polska” is a partner dance where the dancers spin each other (släng in Swedish “to sling or toss”) . Slangpolska efter Byss - Kalle is attributed to Byss-Kalle, who was a notable Swedish folk musician, specifically a nyckelharpa player . Slangpolska efter Byss - Kalle is a traditional “polska” dance song most often played on the Nyckelharpa or keyed fiddle and is commonly heard in pubs and at festive events throughout Sweden . Approximately 10,000 nyckelharpa players live in Sweden today, and the Swedish and the American Nyckelharpa Associations are dedicated to this Swedish National instrument . The director is encouraged to share video and audio examples of the nyckelharpa playing the original Slangpolska efter Byss - Kalle .Tryggare Kan Ingen Vara (Children of the Heavenly Father)Tryggare Kan Ingen Vara Is a traditional Swedish melody, possibly of German roots, and was believed to be arranged as a hymn by the Swedish hymn writer, Karolina Wilhelmina Sandell-Berg (1832–1903) . As a daughter of a Swedish Lutheran minister, she began writing poems as a teenager and is said to have written over 1,700 different texts . There are two different accounts as to the inspiration for this hymn . The first story is that Lina (as she was called) wrote the hymn to honor her father and to say thank you to him for raising her and protecting her . A second belief is of her witnessing the tragic death of her father . She and her father were on a boat, when a wave threw her father overboard . It was said that the profound effect of watching her father drown is what caused Lina to write the text to this hymn . Although this is a treasured song to people of Swedish descent everywhere, it speaks to all people about a father tending and nourishing his children, and protecting them from evil .SPS71FThe Augustana College Concert BandFounded in 1874, the Augustana Band program is one of the oldest continuously active collegiate band programs in the country . The Concert Band is one of two bands on campus and was formed more than thirty years ago . The Concert Band attracts students of every skill level and from a wide variety of majors . Students in the ensemble play a large part in choosing their music for performance, which include works from the standard repertoire, orchestral transcriptions, and the latest compositions from leading composers .Rick Jaeschke began his musical career as a clarinet player in the 1st US Army Band . He received a Bachelor of Music degree from Susquehanna University, a Masters of Music from James Madison University, and a doctorate from Columbia University in New York . He was also fortunate to study conducting with Donald Hunsburger and with Frederick Fennell .Dr . Jaeschke taught band and choir at Great Mills High School in Southern Maryland, and for fifteen years, he was the district Music Supervisor in Armonk, New York, where he taught high school concert and jazz bands, beginning band, and music technology . During that time, the music program flourished, and the high school band consistently received Gold Medals in the New York State Festivals, as well as in national, and international festivals . As a clarinet and saxophone player, Dr . Jaeschke performed in the New York metropolitan area with the Rockland Symphony Orchestra, the Putnam Symphony Orchestra, Fine Arts Symphony Orchestra, and served as the concert master for the Hudson Valley Wind Symphony .For several years, Dr . Jaeschke served as the Fine Arts Coordinator for the District 204 schools in Naperville, IL, a district selected as One of the Best 100 Schools in America for Music . Currently, Dr . Jaeschke is an Associate Professor at Augustana College where he teaches music and music education courses, and directs the Concert Band . He has served on various educational boards, is a National edTPA scorer, and has presented at state, national and international music conferences . He lives with his family in Bettendorf Iowa, and enjoys any opportunity to explore the open water in his sea kayak .

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.