The Lamb Orchestre à Cordes [Conducteur et Parties séparées] Chester
(String Orchestra). By John Tavener (1944-). For Orchestra (Score and Parts). So...(+)
(String Orchestra). By
John Tavener (1944-). For
Orchestra (Score and
Parts). Songbooks and
Methods. Music Sales
America. Chester Music
#CH7115901. Published by
Chester Music
(String Orchestra). By Eric Whitacre (1970-). For String Orchestra (Score). Musi...(+)
(String Orchestra). By
Eric Whitacre (1970-).
For String Orchestra
(Score). Music Sales
America. Softcover. 4
pages. Chester Music
#CH79409. Published by
Chester Music
SKU: HL.50606986 For String Orchestra. Composed by Esa-Pekka Salon...(+)
SKU: HL.50606986
For String
Orchestra. Composed
by Esa-Pekka Salonen.
Score. Softcover. 56
pages. Duration 720
seconds. Chester Music
#CH88224. Published by
Chester Music
(HL.50606986).
ISBN
9798350128697. UPC:
196288215332.
9.0x12.0x0.138
inches.
Commissione
d by the Stockholm
Concert Hall Foundation,
Stockholm Diary is a
powerful and virtuosic 13
minute piece for string
orchestra. Written in
2004 for Esa-Pekka
Salonen's Composer
Portrait, October 2004,
the work is a prime
example of the composer's
use of harmonies and
rich, creamy
textures.
String Orchestra - Intermediate SKU: HL.14005636 Composed by Charles Wilf...(+)
String Orchestra -
Intermediate
SKU:
HL.14005636
Composed
by Charles Wilfred Orr.
Music Sales America.
Classical. Sheet Music,
Score and Parts. With
Text language: English.
Chester Music #CH61640.
Published by Chester
Music (HL.14005636).
From Shakespeare's England. Composed by Nicholas Hare. Arranged by Nicholas Hare...(+)
From Shakespeare's
England. Composed by
Nicholas Hare. Arranged
by Nicholas Hare.
Playstrings. Classical.
Book Only. Composed 2005.
16 pages. Chester Music
#MUSCH55340. Published by
Chester Music
Composed by Witold Lutoslawski (1913-1994). Music Sales America. Post-1900. Book...(+)
Composed by Witold
Lutoslawski (1913-1994).
Music Sales America.
Post-1900. Book Only.
Composed 1999. 38 pages.
Chester Music
#MUSCH60924. Published by
Chester Music
By Katy Perry, Mikkel Eriksen, Tor Erik Hermansen, Sandy Wilhelm, and Ester De...(+)
By Katy Perry, Mikkel
Eriksen,
Tor Erik Hermansen, Sandy
Wilhelm, and Ester Dean.
Arranged by Todd Parrish.
Orchestra. Score; String
Orchestra. Pop Beginning
String Orchestra. Light
Concert; Pop/Rock. Grade
2.5.
16 pages. Published by
Alfred
Music Publishing
Katy Perry: Firework Orchestre à Cordes [Conducteur et Parties séparées] - Facile Belwin
By Katy Perry, Mikkel Eriksen, Tor Erik Hermansen, Sandy Wilhelm, and Ester ...(+)
By Katy Perry, Mikkel
Eriksen,
Tor Erik Hermansen, Sandy
Wilhelm, and Ester Dean.
Arranged by Todd Parrish.
Orchestra. Part(s);
Score;
String Orchestra. Pop
Beginning String
Orchestra.
Light Concert; Pop/Rock.
Grade
2.5. 148 pages. Published
by
Alfred Music Publishing
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.
Die Zauberflote Orchestre à Cordes EMB (Editio Musica Budapest)
Composed by Wolfgang Amadeus Mozart (1756-1791). Set (Score & Parts). Co...(+)
Composed by Wolfgang
Amadeus
Mozart (1756-1791). Set
(Score & Parts).
Composed
2009. Editio Musica
Budapest
#EMBZ14657. Published by
Editio Musica Budapest
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
Composed by Greg Bartholomew. For "trumpet, percussion & string orc...(+)
Composed by Greg
Bartholomew.
For "trumpet,
percussion &
string orchestra".
Pathways
Series. Level 4. Score
and set
of parts. Duration
"3 minutes,
40 seconds".
Published by
Imagine Music
Score Only.
Composed by Neridah
Oostenbroek. Series;
String Orchestra. FJH
String Orchestra.
Multicultural. Score. The
FJH Music Company Inc
#98-ST6500S. Published by
The FJH Music Company Inc
(FJ.ST6500S).
English.
Get
ready to have some fun
with this energetic
western-style romp!
Showcasing a melody that
weaves its way through
every section, the piece
also makes use of open
string drones and
syncopated rhythms,
bringing the
country-style flair to
life. Outstanding and
infectious!
About FJH
String
Orchestra
More emphasis on bow
technique and
independence of lines.
For the accomplished
middle, high school,
college, or professional
group. Grade 3 and up
Orchestra String Orchestra - Grade 2 SKU: FJ.ST6159S Life of a Cowboy<...(+)
Orchestra String
Orchestra - Grade 2
SKU: FJ.ST6159S
Life of a Cowboy.
Composed by Soon Hee
Newbold. Series; String
Orchestra. FJH Developing
Strings. Score. Duration
2:15. The FJH Music
Company Inc #98-ST6159S.
Published by The FJH
Music Company Inc
(FJ.ST6159S).
English.
In the
spirit of classic western
songs, this haunting work
depicts lonely cowboys on
their long journeys
across dangerous terrain
while facing freezing
temperatures, scorching
heat, blizzards, rain,
and late nights. With
traditional rhythms in
the lower strings and a
fun groove in the violas
(cued in other
instruments), your
students and audience
will be sure to enjoy
this cowboy saga!
Composed by Richard Bell.
Score. Neil A. Kjos Music
Company #SO119F.
Published by Neil A. Kjos
Music Company
(KJ.SO119F).
Four movements
entitled Western Swing,
Southern Lullaby, Cowboy
Waltz, & Shaker Dances
make up this vibrant
symphony for string
orchestras. Great
melodies combined with
rhythmic energy will
motivate students and
will be a favorite at
concert time.
Tumbleweed Blues Orchestre à Cordes [Conducteur et Parties séparées] - Débutant Kendor Music Inc.
By Frueh. For standard string orchestra (88555) with opt. piano accompaniment. P...(+)
By Frueh. For standard
string orchestra (88555)
with opt. piano
accompaniment. Playground
String Orchestra Series.
Grade 1. Score and set of
parts. Duration 2
minutes, 30 seconds.
Published by Kendor Music
Inc