Left Behind

SKU: FJ.FJH2351

ISBN 9781619283084. UPC: 241444424582. English.

Spice up your holiday recital with these humorous Christmas tunes! Witty and offbeat pieces that allude to traditional carols are sure to entertain both children and adults. Titles include Elves Falling Off Shelves, Santa Got Pulled Over for Speeding, and One Cookie Left Behind, plus nine more. All the giggling will surely put you and your audience into a joyous holiday spirit!

SKU: AP.45817S

UPC: 038081525518. English. Traditional Irish Tune.

All in first position with straightforward rhythms and thematic parts for everyone, this poignant song arranged by Sandra Dackow will be a wonderful addition to any concert. The Girl I Left Behind Me first appears in 18th century Ireland, often known as Brighton Camp. It emigrated to the United States along with many other Anglo/Scots/Irish folk tunes and became a popular marching song for soldiers. During the American Civil War, soldiers in both the Confederate and Union armies sang it. A number of cultures have embraced this song, adding their own local lyrics. (2:15) This title is available in MakeMusic Cloud.

About Orchestra Expressions

Play great songs such as Over the Rainbow, Batman, This Land Is Your Land, and Star Wars (Main Title). Listen to and play a variety of styles of music: popular, traditional, classical, folk and patriotic. Read and write music; compose and improvise. Perform in a concert and play for your family and friends. Be a conductor of the orchestra. Learn about composers, such as Antonin Dvorak, Johann Pachelbel, Jacques Offenbach, Pytor Ilyich Tchaikovsky, Giuseppe Verdi, George M. Cohan, George Frideric Handel, Ludwig van Beethoven, Johann Sebastian Bach, Wolfgang Amadeus Mozart, Giacomo Puccini, Georges Bizet, Neal Hefti, and John Williams. Discover how music and art are related. Learn about a variety of musical ensembles including string orchestra, full orchestra, mariachi band, steel drum band, dixieland jazz band, rock band, and more. Play music from around the world, including North America, Europe, Latin America, Asia, and Africa.

SKU: HL.4005560

UPC: 888680753290. 9.0x12.0x0.044 inches.

This poignant and lyrical work by Richard Saucedo utilizes sections of transparent beauty, with only a few instruments playing, contrasted with sections of dramatic emotional performed by the entire ensemble. Featuring long phrases and sustained intensity, this is a challenging yet rewarding work for mature bands. Dur: 6:00.

SKU: SU.50500020

Mezzo-Soprano, Horn Duration: c. 11' Texts by Edna St. Vincent Millay Composed: 2006 Published by: Seesaw Music Composer's Note: Inspired by the story of a friend who was left behind when her husband went off to Iraq and the personal suffering this caused.

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.YPS239

ISBN 9781491159613. UPC: 680160918201.

This piece is about a journey unlike any other in 2020. We have all been touched by the devastating effects of COVID-19, and we have seen friends, family, and many others succumb to it. For the people who are left behind this piece is dedicated to you, the brave warriors that have survived this pandemic. The piece is set in Eb major with a 4/4 time signature. The beginning starts off robust and full, with the tempo at quarter note= 150. Measure 25 presents many opportunities for shaping to move the melody and counter melody lines around as the ostinato is being played in the percussion and low brass. I wrote mm. 43-51 as a percussion feature. I felt in my eighteen years of experience as an educator that we always have plenty of percussionists! Double students on parts if you have way too many. Overall, this piece has many places for beautiful phrasing and shaping. You will need to assign the students places to breathe in order to achieve maximum effort from the group. I hope you enjoy my new piece The Brave Warrior.
This piece is about a journey unlike any other in 2020. We have all been touched by the devastating effects of COVID-19, and we have seen friends, family, and many others succumb to it. For the people who are left behind this piece is dedicated to you, the brave warriors that have survived this pandemic. The piece is set in Eb major with a 4/4 time signature. The beginning starts off robust and full, with the tempo at quarter note= 150. Measure 25 presents many opportunities for shaping to move the melody and counter melody lines around as the ostinato is being played in the percussion and low brass. I wrote mm. 43–51 as a “percussion” feature.  I felt in my eighteen years of experience as an educator that we always have plenty of percussionists! Double students on parts if you have way too many.  Overall, this piece has many places for beautiful phrasing and shaping. You will need to assign the students places to breathe in order to achieve maximum effort from the group.  I hope you enjoy my new piece The Brave Warrior.

SKU: CF.SPS94F

ISBN 9781491161838. UPC: 680160920518.

On November 5th, 2017, a mass shooting took place at the First Baptist Church in Sutherland Springs, Texas. Twenty-six innocent people lost their lives that day, including an unborn child. Overture to a Small Town is dedicated to these victims and the loved ones they left behind. From the biggest cities to the smallest towns, the senseless bloodshed must end. Despite the darkness of this tragedy, it is my intent through this music to portray a sense of hope, dignity, and innocence deserved by all America's cities and towns. The opening moments of this piece should be treated delicately, ensuring that the brass section moves together in one unified voice, and that the crotales evoke distant flickers of light. Similarly, in mm. 120-127, articulations in the flutes, trumpets and mallets should be strong enough to be heard, but without being aggressive. The textural layering in mm. 48-53 should be executed with machine-like precision of both rhythm and articulation. This passage should evoke the sound of many voices rising together. There should be a great contrast between the opening Piano dynamic and the final Forte dynamic. In mm. 65-69, both mallet percussionists may play the indicated notes in any octave they choose. Both players should move rapidly between notes in any order. This passage should sound fluid and ethereal. In mm. 69-73: If there is no English Horn available to the ensemble, the Trumpet should play this passage solo. If there is an English Horn, both instruments should play the passage together.
On November 5th, 2017, a mass shooting took place at the First Baptist Church in Sutherland Springs, Texas. Twenty-six innocent people lost their lives that day, including an unborn child. Overture to a Small Town is dedicated to these victims and the loved ones they left behind. From the biggest cities to the smallest towns, the  senseless bloodshed must end. Despite the darkness of this tragedy, it is my intent through this music to portray a sense of hope, dignity, and innocence deserved by all America’s cities and towns.  The opening moments of this piece should be treated delicately, ensuring that the brass section moves together in one unified voice, and that the crotales evoke distant flickers of light. Similarly, in mm. 120-127, articulations in the flutes, trumpets and mallets should be strong enough to be heard, but without being aggressive.  The textural layering in mm. 48-53 should be executed with machine-like precision of both rhythm and articulation. This passage should evoke the sound of many voices rising together. There should be a great contrast between the opening Piano dynamic and the final Forte dynamic.  In mm. 65-69, both mallet percussionists may play the indicated notes in any octave they choose. Both players should move rapidly between notes in any order. This passage should sound fluid and ethereal.  In mm. 69-73: If there is no English Horn available to the ensemble, the Trumpet should play this passage solo. If there is an English Horn, both instruments should play the passage together.