The Shape of Water

SKU: KJ.SO300F

UPC: 8402702891.

A mix of bowed and pizz. playing creates myriad colors. The deliberate dissonances and intense dynamic shifts offer terrific ensemble work relying on good listening skills and ability to blend and shape the carefully written nuances.

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: PR.11442041L

UPC: 680160687039.

In one of the dedicatory poems to his verse play The Shadowy Waters (1906), William Butler Yeats asks: Is Eden far away...? Do our woods and winds and verponds cover more quiet woods, More shining winds, more star-glimmering ponds? Is Eden out of time and out of space? How do you answer such questions? We have only the vague elusive promptings of our own mysterious, troubled hearts to tell us that the Eden we long for is there, somewhere beyond the physical world which frames our existence, in another realm of different dimensions. And - what is most painful to admit - that it is closed to us in the form in which we live and breathe, even if at times we do have intimations..., Yeats is telling us that this paradise, this Eden we yearn for is here - present even if invisible, palpable even if intangible. In his Second Symphony, Mahler meets an angel who tells him he can't get into heaven, he's locked out. The news is shattering. What follows is an inconsolable sorrowing, the same sorrowing that comes when we wake to the realization that we too are locked out of Eden. Eden is the heaven of our longing and desire for release from pain and suffering. Eden is the image in our restive minds that reflects the reconciled, resolved, quiescent state of soul we hunger for. But Eden eludes -because it is not a place. It is a state of soul which answers none of the illusory, hampering conditions that shape and bind us to the real world of our bodies, our appetites, our passions, and our beliefs. I have turned Yeats' question Is Eden out of time and out of space? into its own answering. However near we may sense its presence at times, Eden remains unreachable, ungraspable, unknowable, unthinkable. It forever eludes us. I wrote this music the way I did to shut out -with quietness and otherworldliness - the clamor and clang of the raucous Garish Day, to turn away its tumult and noise, to negate its stridency and chaos. Perhaps in the cleansing stillness and blessing of this emptied-out state of soul, Eden, through still hidden, may not be so far way; though still unreachable, may be close enough almost to touch.
In one of the dedicatory poems to his verse play “The Shadowy Waters” (1906), William Butler Yeats asks:“Is Eden far away…?Do our woods and windsand verponds cover morequiet woods,More shining winds,more star-glimmeringponds?Is Eden out of timeand out of space?”How do you answer such questions? We have only the vague elusive promptings of our own mysterious, troubled hearts to tell us that the Eden we long for is there, somewhere beyond the physical world which frames our existence, in another realm of different dimensions. And – what is most painful to admit – that it is closed to us in the form in which we live and breathe, even if at times we do have intimations…, Yeats is telling us that this paradise, this Eden we yearn for is here – present even if invisible, palpable even if intangible.In his Second Symphony, Mahler meets an angel who tells him he can’t get into heaven, he’s locked out. The news is shattering. What follows is an inconsolable sorrowing, the same sorrowing that comes when we wake to the realization that we too are locked out of Eden.Eden is the heaven of our longing and desire for release from pain and suffering. Eden is the image in our restive minds that reflects the reconciled, resolved, quiescent state of soul we hunger for. But Eden eludes –because it is not a place. It is a state of soul which answers none of the illusory, hampering conditions that shape and bind us to the real world of our bodies, our appetites, our passions, and our beliefs.I have turned Yeats’ question “Is Eden out of time and out of space?” into its own answering. However near we may sense its presence at times, Eden remains unreachable, ungraspable, unknowable, unthinkable. It forever eludes us.I wrote this music the way I did to shut out –with quietness and otherworldliness – the clamor and clang of the raucous “Garish Day,” to turn away its tumult and noise, to negate its stridency and chaos. Perhaps in the cleansing stillness and blessing of this emptied-out state of soul, Eden, through still hidden, may not be so far way; though still unreachable, may be close enough almost to touch.

SKU: 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.