Piano / keyboard - easy to intermediate SKU: M7.MF-2067-01 6 Chart Hit...(+)
Piano / keyboard - easy
to intermediate
SKU:
M7.MF-2067-01
6
Chart Hits: Blurred Lines
- Ho Hey - Bei meiner
Seele - Read All About
It, Pt. III - Give Me A
Reason - Only Teardrops.
Noten + CD für Klavier
und Keyboard/Gitarre. Mit
MIDI-Files, Playalon.
Arranged by Uwe Bye. This
edition: Saddle-wire
stitching. Sheet music
with CD. Music Factory.
CD with MIDI-Files &
Play-Along-Tracks. 56
pages. Music Factory #MF
2067-01. Published by
Music Factory
(M7.MF-2067-01).
Sand Waltz Flûte, Hautbois, Clarinette, Basson Hal Leonard
Flute, Oboe, Clarinet, Bassoon and Horn Woodwind Ensemble (Score and Parts) S...(+)
Flute, Oboe, Clarinet,
Bassoon and Horn Woodwind
Ensemble (Score and
Parts)
SKU:
HL.48022746
Score
and Parts. Composed
by Elena Kats-Chernin.
Boosey and Hawkes Chamber
Music. Classical,
Contemporary. Softcover.
Hal Leonard #M202532959.
Published by Hal Leonard
(HL.48022746).
UPC:
884088925239.
9.25x12.0x0.28
inches.
The title
refers to the writer
Aurore Dupin (1804-1876)
who, under the pseudonym
of George Sand, ranks
among the important
self-confident and
socio-critical women in
19th-century literature.
Musicians have known her
from her relationship of
nine years with
Chopin.
By Bruce Berr. For Piano. Contents include: Wispy Clouds; The Distant Shore; Ska...(+)
By Bruce Berr. For Piano.
Contents include: Wispy
Clouds; The Distant
Shore; Skating on the
Boardwalk; Playful
Dolphins; Medieval Sand
Castle; Playing Tag;
Going Home. Animals and
Nature. Level: Early
Intermediate. Book.
Published by The FJH
Music Company, Inc.
For
Sixteen Instrumentalists,
Two Singers and
Computer-Processed
Sound. Composed by
Roger Reynolds. Orchestra
Score. Classical; Living
Composer. Score. Composed
1989-93 (Parts I and II);
First Performance: 17
June 1993 Georges
Pompidou Center, Paris
Ensemble. 84 pages.
Duration 00:50:00.
Edition Peters
#98-EP67370. Published by
Edition Peters
(PE.EP67370).
ISBN
9790300738994. Language:
French/English.
Between the shingle and
the dune for
Mezzo-Soprano (singing in
French); Bass-Baritone
(singing in English);
Flute (Piccolo), Oboe, Bb
Clarinet, Bassoon, Horn,
Trumpet, Trombone, Bass
Trombone, 3
Percussionists, Piano, 2
Violins, Violoncello,
Contrabass, 8 channels of
computer-processed sound
(vocal and instrumental)
projected over a
6-channel loudspeaker
system
Texts by
Samuel Beckett: I. they
come - II. what would I
do - III. my way is in
the sand - IV. section IX
(from Texts for Nothing;
French and English) //
Commissioned by
IRCAM
Composed by Greg Bartholomew. For "trumpet, timpani & string orches...(+)
Composed by Greg
Bartholomew.
For "trumpet,
timpani & string
orchestra". Pathways
Series.
Level 4. Score and set of
parts. Duration "3
minutes, 40
seconds". Published
by Imagine
Music
By Bruce Berr. For Piano. Composers In Focus. Allows the opportunity to play mus...(+)
By Bruce Berr. For Piano.
Composers In Focus.
Allows the opportunity to
play music that is both
expressive and
imaginative. A variety of
styles is represented,
from the introspective
and dreamy to the quick
and lighthearted.
Contents include: Crystal
Waters; Vacation Sunrise;
The Drifting Ship;
Volleyball Verve;
Climbing the Sand Dunes;
Swimming; Morning Mist;
Sailing; Igor the Crab.
Animals and Nature.
Level: Late
Elementary/Early
Intermediate. Book.
Published by The FJH
Music Company, Inc.
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.
![Odyssey (Entre le galet et la dune) [Full Score]](https://www.sheetmusicplus.com/dw/image/v2/BJFX_PRD/on/demandware.static/-/Sites-smp-main/default/dw87f905f7/images/313/19110313_cover-large_file.png)
