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 Johann Sebastian Bach (1685-1750). Arranged by Elizabeth Start. Orchestra. Pa...(+)
By Johann Sebastian Bach
(1685-1750). Arranged by
Elizabeth Start.
Orchestra. Part(s);
Score; String Orchestra.
Belwin Concert String
Orchestra. Form: Fugue;
Prelude. Baroque;
Masterwork Arrangement.
Grade 3.5. 124 pages.
Published by Belwin
Publishing
Newbold : Viking Orchestre à Cordes [Conducteur et Parties séparées] - Facile FJH
Composed by Soon Hee Newbold. For string orchestra. FJH Developing Strings. Grad...(+)
Composed by Soon Hee
Newbold. For string
orchestra. FJH Developing
Strings. Grade 2. Score
and parts. Duration 2
minutes, 30 seconds.
Published by The FJH
Music Company Inc
Fiddles at Shady Gulch Orchestre à Cordes [Conducteur et Parties séparées] - Débutant Alfred Publishing
By Mark Williams. For String Orchestra. String Orchestra. Strictly Strings Serie...(+)
By Mark Williams. For
String Orchestra. String
Orchestra. Strictly
Strings Series. Novelty.
Level: 1.5 (grade 1.5).
Conductor Score & Parts.
36 pages. Published by
Alfred Publishing.
Orchestra String Orchestra - Grade 1 SKU: CF.BAS31 Full Score and Part...(+)
Orchestra String
Orchestra - Grade 1
SKU: CF.BAS31
Full Score and
Parts. Composed by
Russian Folk Song.
Arranged by Doris Gazda.
Carl Fischer Beginning
String Orchestra Series.
Score and Parts. With
Standard notation. 8
pages. Carl Fischer Music
#BAS31. Published by Carl
Fischer Music (CF.BAS31).
ISBN 9780825860874.
UPC: 798408060879. 8.5 X
11 inches. Key: C
major.
One of the
most recognizable folk
songs of all-time is
presented in a fine new
Doris Gazda arrangment
for beginning strings.
Optional part for bells,
tone blocks or chimes
will give you the
opportunity to involve
other students in
performing with the
string orchestra. The
Volga River is the
longest river in Europe
(about 2,300 miles long)
and the principal
waterway of Russia. The
Volga has played an
important part in the
life of the Russian
people, and in Russian
folklore is called Mother
Volga. For centuries it
has served as the chief
thoroughfare of Russia
and as the lifeline of
Russian colonization to
the east. It carries
one-half of the total
river freight of Russia
and irrigates the vast
steppes of the lower
Volga region. Grain,
building materials, salt,
fish and caviar (from the
Volga delta and the
Caspian Sea) are shipped
upstream; lumber is the
main commodity shipped
downstream.The folk
song The Volga Boatman
is supposed to represent
the rhythmic rowing of
the hard-working oarsmen
who took their boats and
rafts up and down this
long waterway. The boats
carried goods for trade,
travelers and the armies
and invaders who fought
throughout the Russian
lands.Close your eyes
while you listen to the
song. Imagine that you
have a boat carrying
grain and fish for a long
distance. Then pretend
you are rowing your boat
in rhythm to the
melody.
Composed by Girolamo Frescobaldi (1583-1643). Edited by J. Cameron Law. Ar...(+)
Composed by Girolamo
Frescobaldi (1583-1643).
Edited by J. Cameron Law.
Arranged by John Beeman.
For
string orchestra. Grade
2.
Score and set of parts.
Duration 2 minutes.
Published
by Grand Mesa Music
By Peter Ilyich Tchaikovsky (1840-1893). Arranged by Mark Weston, scored by Doug...(+)
By Peter Ilyich
Tchaikovsky (1840-1893).
Arranged by Mark Weston,
scored by Douglas E.
Wagner. Orchestra. For
strings w/ vln 3.
Masterworks; Part(s);
Score; String Orchestra.
Belwin Beginning String
Orchestra. Christmas;
Light Concert; Masterwork
Arrangement; Novelty;
Romantic; Winter. Grade
2.5. 144 pages. Published
by Belwin Publishing
Time Machine Orchestre à Cordes [Conducteur et Parties séparées] - Débutant Highland/Etling
Composed by Richard Meyer. Orchestra. Part(s); Score; String Orchestra. Highland...(+)
Composed by Richard
Meyer. Orchestra.
Part(s); Score; String
Orchestra.
Highland� String
Explorer. Grade 1.5. 144
pages. Published by
Highland/Etling
Composed by Nikolay Andreyevich Rimsky-Korsakov (1844-1908). Arranged by Bob Lip...(+)
Composed by Nikolay
Andreyevich
Rimsky-Korsakov
(1844-1908). Arranged by
Bob Lipton. For string
orchestra. FJH Developing
Strings. Level 2.5. Score
only. Duration 2:30.
Published by The FJH
Music Company Inc
Can Can Basses Orchestre à Cordes [Conducteur et Parties séparées] - Facile Alfred Publishing
(Bass Section Feature). By Jacques Offenbach (1819-1880). Arranged by Richar...(+)
(Bass Section Feature).
By
Jacques Offenbach
(1819-1880).
Arranged by Richard
Meyer.
Orchestra. Masterworks;
Part(s); Score; String
Orchestra. Highland
String
Explorer. Form: Dance.
Light
Concert; Masterwork
Arrangement; Romantic.
Grade
1.5. 72 pages. Published
by
Alfred Music Publishing
Composed by Bill Calhoun. For string orchestra (violin I, violin II, violin ...(+)
Composed by Bill Calhoun.
For
string orchestra (violin
I,
violin II, violin III
(viola
T.C.), viola, cello,
bass,
piano). Score and parts.
Duration 2 minutes, 11
seconds. Published by
Carl
Fischer
Armada Orchestre à Cordes [Conducteur et Parties séparées] - Débutant Belwin
By Victor López. Orchestra. Part(s); Score; SmartMusic; String Orchestra. Bel...(+)
By Victor López.
Orchestra. Part(s);
Score; SmartMusic; String
Orchestra. Belwin
Beginning String
Orchestra. Light Concert.
Grade 1. 78 pages.
Published by Belwin Music
2nd Movement. Composed by Ludwig van Beethoven (1770-1827). Arranged by B...(+)
2nd Movement.
Composed by Ludwig van
Beethoven (1770-1827).
Arranged by Bud Caputo.
Masterworks; Part(s);
Score; String Orchestra.
Highland/Etling String
Orchestra. Form: Sonata;
Transcription. Classical;
Masterwork Arrangement;
Romantic. 124 pages.
Published by
Highland/Etling
(AP.40471).
Composed by Michael Hopkins. Score; SmartMusic; String Orchestra. Belwin Interme...(+)
Composed by Michael
Hopkins. Score;
SmartMusic; String
Orchestra. Belwin
Intermediate String
Orchestra. 16 pages.
Published by Belwin Music
(AP.41202S).
By De Boismortier. Arranged by Robert D. Mccashin. String Orchestra. FJH String ...(+)
By De Boismortier.
Arranged by Robert D.
Mccashin. String
Orchestra. FJH String
Orchestra. The opening
Adagio is excellent for
working on a full-bodied
sound while developing a
moderate to weighty bow
arm. The Allegro section
can be performed either
as a full tutti work or
in a concerto grosso
fashion, giving you the
flexibility of featuring
your outstanding
individual players while
still programming the
work with a younger
ensemble. Outstanding!
Score for this title: S.
Extra part for this
title: P. Level: 4.
Published by The FJH
Music Company Inc.