(From The Nutcracker). By Peter Ilyich Tchaikovsky (1840-1893). Arranged by John...(+)
(From The Nutcracker). By
Peter Ilyich Tchaikovsky
(1840-1893). Arranged by
John Caponegro. For
string orchestra (88555)
with optional 3rd
violin/viola TC (1) and
piano. Playground String
Orchestra Series. Grade
1.5. Score and set of
parts. Duration 2
minutes. Published by
Kendor Music Inc
Waltz of the Carols Orchestre à Cordes SATB A Cappella - Débutant Excelcia Music Publishing
String Orchestra Orchestra - Grade 1.5 SKU: XC.HSO2002 Composed by Sean O...(+)
String Orchestra
Orchestra - Grade 1.5
SKU: XC.HSO2002
Composed by Sean
O'Loughlin. Harmony
String Orchestra Series.
Christmas and Holiday.
Set of parts. Excelcia
Music Publishing
#HSO2002. Published by
Excelcia Music Publishing
(XC.HSO2002).
UPC:
812598034233. 9 x 12
inches.
Introduce
your students to 3/4 time
with this clever mash-up
of Christmas Carols in
Waltz style. Each section
has a turn to shine with
the melody, perfect for
parents to get a good
shot of their little ones
at their Christmas
concert.
By Johann Strauss, Jr. Arranged by Mark Williams. Music by Johann Strauss / arr....(+)
By Johann Strauss, Jr.
Arranged by Mark
Williams. Music by Johann
Strauss / arr. Mark
Williams. For String
Orchestra. String
Orchestra. Strictly
Strings Series. Level: 1
(grade 1). Conductor
Score and Parts. 1 pages.
Published by Alfred
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.
By Emile Waldteufel (1837-1915). Arranged by Andrew Balent. String ensemble. For...(+)
By Emile Waldteufel
(1837-1915). Arranged by
Andrew Balent. String
ensemble. For String
Orchestra. Carl Fischer
First Plus String
Orchestra Series.
Classical. Grade 1.5-2.
Score and Parts. Standard
notation. 8 pages.
Published by Carl Fischer
For Full or String Orchestra. Arranged by Larry Clark. For Full Orchestra. Full ...(+)
For Full or String
Orchestra. Arranged by
Larry Clark. For Full
Orchestra. Full
Orchestra. Belwin
Intermediate Full
Orchestra. Level: 2.5
(grade 2.5). Conductor
Score and Parts. 234
pages. Published by
Alfred Publishing.
Composed by Joshua
Reznicow. Performance
Music Ensemble; String
Orchestra. Ludwig
Masters. Score. Latham
Music Enterprises
#36-52255538. Published
by Latham Music
Enterprises
(AP.36-52255538).
ISBN
9781621568636. UPC:
746241260185.
English.
A rousing
concert ender, this work
will challenge all
sections with a wide
range (every part
shifts), running passage
work, trills, and
syncopated rhythms.
The B section, a
lyric waltz theme, shows
off the principal players
with extended solos.
The return of the A
section superimposes the
waltz melody on the
original syncopated theme
for a wonderful
conclusion.
These products
are currently being
prepared by a new
publisher. While many
items are ready and will
ship on time, some others
may see delays of several
months.
Composed by Joshua
Reznicow. Performance
Music Ensemble; String
Orchestra. Ludwig
Masters. Patriotic. Score
and Part(s). Latham Music
Enterprises #36-52250538.
Published by Latham Music
Enterprises
(AP.36-52250538).
ISBN
9781621568629. UPC:
679360699294.
English.
A rousing
concert ender, this work
will challenge all
sections with a wide
range (every part
shifts), running passage
work, trills, and
syncopated rhythms.
The B section, a
lyric waltz theme, shows
off the principal players
with extended solos.
The return of the A
section superimposes the
waltz melody on the
original syncopated theme
for a wonderful
conclusion.
These products
are currently being
prepared by a new
publisher. While many
items are ready and will
ship on time, some others
may see delays of several
months.
For String Orchestra. Composed by Yukiko Nishimura. Southern Music. Concert. ...(+)
For String Orchestra.
Composed by Yukiko
Nishimura.
Southern Music. Concert.
Softcover. Southern Music
Company #SO127C.
Published by
Southern Music Company
Bug's Ballroom Orchestre à Cordes [Conducteur et Parties séparées] - Débutant Kendor Music Inc.
Composed by Frank Halferty. For string orchestra (88555) with optional 3rd violi...(+)
Composed by Frank
Halferty. For string
orchestra (88555) with
optional 3rd violin/viola
TC (3 copies) and piano.
Playground String
Orchestra Series. Grade
1. Score and set of
parts. Duration 3
minutes, 20 seconds.
Published by Kendor Music
Inc
Composed by Almon C. Bock
II. String Orchestra.
Highland/Etling String
Orchestra. Novelty.
Score. 24 pages.
Highland/Etling
#00-31626S. Published by
Highland/Etling
(AP.31626S).
UPC:
038081352893.
English.
This theme
and six variations on the
well-known children's
song incorporate many
string-playing techniques
providing great teaching
opportunities in a
setting sure to be a hit
with young and old alike.
The six variations,
including a waltz and a
cha-cha, are uniquely
woven to maintain the
theme, but impart their
own characters and
flavors featuring each
section of the orchestra
at various times. The
final variation includes
a surprise and will leave
audiences wondering if
they heard correctly. The
piece ends with a rousing
restatement of the
theme.