Score and Parts baritone, trumpet, trombone and bass clarinet

SKU: HL.49046406

For Baritone, Trumpet, Trombone, and Bass Clarinet Score and Part. Composed by Lei Liang. Sheet music. Edition Schott. Softcover. Composed 2016. 44 pages. Duration 11'. Schott Music #ED 31309. Published by Schott Music (HL.49046406).

ISBN 9781540086945. UPC: 840126910674. 9.0x12.0x0.26 inches. Chinese - English.

Having been interested in Mahayana Buddhism for a number of years, I went to a Buddhist monastery in upstate New York to study meditation in 1999. One evening, while walking alone by the side of the lake, I caught the sight of a 'V'shape floating and extending on the surface of the water. It was a beaver taking a swim under the moon. This image gave me insight into my relationship with silence: underneath the music is a profoundly deep silence upon which I seekto inscribe my signature through sound. It serves as a point of departure that led to a series of works.In Lakescape V, the tranquility in the original 'lake' series is disturbed by showers of 'phonetic particles' taken from Wai-lim Yip's poetry (in both English and Chinese) as the piece traverses through different states of mind.Lakescape V was written for and dedicated to loadbang who gave its world premiere at the Miller Theatre's Composer Portrait on November 17th, 2016.- Lei Liang.

For piano. Format: piano solo songbook. New age and contemporary instrumental. 88 pages. 9x12 inches. Published by Hal Leonard.

Composed by Various. Piano Solo Songbook. Movies. Softcover. 104 pages. Published by Hal Leonard

Performance Score Flute; Vibraphone - intermediate to advanced

SKU: HL.49046365

For Flute and Vibraphone Performance Score. Composed by Lei Liang. Sheet music. Edition Schott. Classical. Softcover. Composed 2019. Duration 480 seconds. Schott Music #ED 30325. Published by Schott Music (HL.49046365).

ISBN 9781540083852. UPC: 840126906257. 9.0x12.0x0.079 inches.

Having been interested in Mahayana Buddhism for a number of years, I went to a Buddhist monastery in upstate New York to study meditation in 1999. One evening, while walking alone by the side of the lake, I caught the sight of a V shape floating and extending on the surface of the water. It was a beaver taking a swim under the moon. This image gave me insight into my relationshipwith silence: underneath the music is a profoundly deep silence upon which I seek to inscribe my signature through sound. It serves as a point of departure that led to a series of works.

SKU: GI.001116

Sacred. GIA Publications #001116. Published by GIA Publications (GI.001116).

The unique watercolor style of San Antonio artist G. E. Mullan is noted for its lyrical line set against an ordered and complex geometry of interdependent shapes. His technique creates a visual excitement that involves the viewer and invites close study of the excellence of the work. His religious subjects incorporate the historical traditions of the Santos figures of Mexico and the Southwest, the illuminated manuscripts of Western Europe, and the icons and mosaics of the Byzantine style. 4in. x 9in. Notecard.

SKU: GI.001105

Composed by G. E. Mullan. Children. Sacred. GIA Publications #001105. Published by GIA Publications (GI.001105).

English.

The unique watercolor style of San Antonio artist G. E. Mullan is noted for its lyrical line set against an ordered and complex geometry of interdependent shapes. His technique creates a visual excitement that involves the viewer and invites close study of the excellence of the work. His religious subjects incorporate the historical traditions of the Santos figures of Mexico and the Southwest, the illuminated manuscripts of Western Europe, and the icons and mosaics of the Byzantine style. 4in. x 9in. Notecard.

Orchestra String Orchestra - Grade 3

SKU: CF.CAS7

Composed by Doris Gazda. Edited by Amy Rosen. FS-SWs. Carl Fischer Concert String Orchestra Series. Score and Parts. With Standard notation. 20+24+24+6+15+15+15 pages. Carl Fischer Music #CAS7. Published by Carl Fischer Music (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.

By Various. Music Sales America. Softcover. 128 pages. Chester Music #CH72138. Published by Chester Music

Alto Saxophone

SKU: BT.MUSAM1006489

By Jenni Norey. Playalong 50-50. Pop & Rock. Book with Online Audio. Composed 2013. 136 pages. Wise Publications #MUSAM1006489. Published by Wise Publications (BT.MUSAM1006489).

ISBN 9781783050987.

Playalong 50/50: Alto Sax includes 50 pop hits arranged for Alto Saxophone. Step into the spotlight and play these 50 pop hits with specially recorded backing tracks (available online). Includes fullperformanceversions of all the songs - the instrumental part is then omitted so you can play along with the recorded accompaniments.

By Jenni Norey. Playalong 50- 50. Pop & Rock. Book with Online Audio. Composed 2014. 144 pages. Wise Publications #MUSAM1007226. Published by Wise Publications