(Bass). Arranged by Robert Gardner. For Bass. Book; Quartet; String Ensemble - M...(+)
(Bass). Arranged by
Robert Gardner. For Bass.
Book; Quartet; String
Ensemble - Mixed.
Patriotic. Intermediate.
32 pages. Published by
Alfred Music Publishing
(Score). Arranged by Robert Gardner. For Score. Book; Quartet; String Ensemble -...(+)
(Score). Arranged by
Robert Gardner. For
Score. Book; Quartet;
String Ensemble - Mixed.
Patriotic. Intermediate.
80 pages. Published by
Alfred Music Publishing
Orchestra string orchestra - Grade 2.5 SKU: KJ.SO356F Composed by Frank W...(+)
Orchestra string
orchestra - Grade 2.5
SKU: KJ.SO356F
Composed by Frank
Woodruff. Score only.
Neil A. Kjos Music
Company #SO356F.
Published by Neil A. Kjos
Music Company
(KJ.SO356F).
UPC:
084027043981.
A
perfect piece any time of
year to honor the USA and
to recognize audience
members who currently or
have served our nation
through military service.
The piece begins with the
familiar My country 'tis
of thee theme stated in
the 1st violins, then
launches into three
vibrant variations that
allows all sections of
the orchestra to shine. G
Major.
Orchestra string orchestra - Grade 2.5 SKU: KJ.SO356C Composed by Frank W...(+)
Orchestra string
orchestra - Grade 2.5
SKU: KJ.SO356C
Composed by Frank
Woodruff. Score and
parts. Neil A. Kjos Music
Company #SO356C.
Published by Neil A. Kjos
Music Company
(KJ.SO356C).
UPC:
084027043974.
A
perfect piece any time of
year to honor the USA and
to recognize audience
members who currently or
have served our nation
through military service.
The piece begins with the
familiar My country 'tis
of thee theme stated in
the 1st violins, then
launches into three
vibrant variations that
allows all sections of
the orchestra to shine. G
Major.
Orchestra String Orchestra - Grade 1.5-2 SKU: CF.FAS26 Full Score....(+)
Orchestra String
Orchestra - Grade 1.5-2
SKU: CF.FAS26
Full Score.
Composed by Sean
O'Loughlin. Carl Fischer
First Plus String
Orchestra Series. Score
and Parts. With Standard
notation. 12 pages. Carl
Fischer Music #FAS26.
Published by Carl Fischer
Music (CF.FAS26).
ISBN
9780825854811. UPC:
798408054816. 8.5 X 11
inches. Key: D
major.
Arches is a piece for the
developing string
orchestra that derives
its title from the
national park in Utah. I
visited the Arches
National Monument in June
of 2003 during a
cross-country trip. The
Delicate Arch is the
recognizable landmark
from this beautiful
national park. In order
to see this remarkable
natural formation up
close, you have to hike a
trail of over two miles.
The music in this piece
is inspired by my journey
to see the arch. Once
there, you are treated to
a vast panoramic view of
the golden Utah landscape
that leaves one
breathless.
Arches is an
effective piece in
teaching
pizzicato
playing as a melodic
device. Most often,
pizzicato is
used as an effect or
punctuation mark to
larger melodic ideas.
There is a brief arco
section to provide
contrast and build up to
the dramatic return of
the main
pizzicato
melody. Each section in
the ensemble has a
statement of the melody.
It is important to think
linearly in addition to
vertically when playing
these pizzicato
lines. Forward motion is
of up-most importance in
terms of making musical
phrases out of these
pizzicato
lines. Arches
is a piece for the
developing string
orchestra that derives
its title from the
national park in Utah. I
visited the Arches
National Monument in June
of 2003 during a
cross-country trip. The
Delicate Arch is the
recognizable landmark
from this beautiful
national park. In order
to see this remarkable
natural formation up
close, you have to hike a
trail of over two miles.
The music in this piece
is inspired by my journey
to see the arch. Once
there, you are treated to
a vast panoramic view of
the golden Utah landscape
that leaves one
breathless.
Arches is an
effective piece in
teachingA
pizzicato
playing as a melodic
device. Most often,A
pizzicato is
used as an effect or
punctuation mark to
larger melodic ideas.
There is a brief arco
section to provide
contrast and build up to
the dramatic return of
the mainA
pizzicato
melody. Each section in
the ensemble has a
statement of the melody.
It is important to think
linearly in addition to
vertically when playing
theseA pizzicato
lines. Forward motion is
of up-most importance in
terms of making musical
phrases out of theseA
pizzicatoA
lines. Arches
is a piece for the
developing string
orchestra that derives
its title from the
national park in Utah. I
visited the Arches
National Monument in June
of 2003 during a
cross-country trip. The
Delicate Arch is the
recognizable landmark
from this beautiful
national park. In order
to see this remarkable
natural formation up
close, you have to hike a
trail of over two miles.
The music in this piece
is inspired by my journey
to see the arch. Once
there, you are treated to
a vast panoramic view of
the golden Utah landscape
that leaves one
breathless.
Arches is an
effective piece in
teachingA
pizzicato
playing as a melodic
device. Most often,A
pizzicato is
used as an effect or
punctuation mark to
larger melodic ideas.
There is a brief arco
section to provide
contrast and build up to
the dramatic return of
the mainA
pizzicato
melody. Each section in
the ensemble has a
statement of the melody.
It is important to think
linearly in addition to
vertically when playing
theseA pizzicato
lines. Forward motion is
of up-most importance in
terms of making musical
phrases out of theseA
pizzicatoA
lines. Arches
is a piece for the
developing string
orchestra that derives
its title from the
national park in Utah. I
visited the Arches
National Monument in June
of 2003 during a
cross-country trip. The
Delicate Arch is the
recognizable landmark
from this beautiful
national park. In order
to see this remarkable
natural formation up
close, you have to hike a
trail of over two miles.
The music in this piece
is inspired by my journey
to see the arch. Once
there, you are treated to
a vast panoramic view of
the golden Utah landscape
that leaves one
breathless.
Arches is an
effective piece in
teaching
pizzicato
playing as a melodic
device. Most often,
pizzicato is
used as an effect or
punctuation mark to
larger melodic ideas.
There is a brief arco
section to provide
contrast and build up to
the dramatic return of
the main
pizzicato
melody. Each section in
the ensemble has a
statement of the melody.
It is important to think
linearly in addition to
vertically when playing
these pizzicato
lines. Forward motion is
of up-most importance in
terms of making musical
phrases out of these
pizzicato
lines. Arches is
a piece for the
developing string
orchestra that derives
its title from the
national park in Utah. I
visited the Arches
National Monument in June
of 2003 during a
cross-country trip. The
Delicate Arch is the
recognizable landmark
from this beautiful
national park. In order
to see this remarkable
natural formation up
close, you have to hike a
trail of over two miles.
The music in this piece
is inspired by my journey
to see the arch. Once
there, you are treated to
a vast panoramic view of
the golden Utah landscape
that leaves one
breathless. Arches is an
effective piece in
teaching pizzicato
playing as a melodic
device. Most often,
pizzicato is used as an
effect or punctuation
mark to larger melodic
ideas. There is a brief
arco section to provide
contrast and build up to
the dramatic return of
the main pizzicato
melody. Each section in
the ensemble has a
statement of the melody.
It is important to think
linearly in addition to
vertically when playing
these pizzicato lines.
Forward motion is of
up-most importance in
terms of making musical
phrases out of these
pizzicato
lines. Arches is a
piece for the developing
string orchestra that
derives its title from
the national park in
Utah. I visited the
Arches National Monument
in June of 2003 during a
cross-country trip. The
Delicate Arch is the
recognizable landmark
from this beautiful
national park. In order
to see this remarkable
natural formation up
close, you have to hike a
trail of over two miles.
The music in this piece
is inspired by my journey
to see the arch. Once
there, you are treated to
a vast panoramic view of
the golden Utah landscape
that leaves one
breathless.Arches is an
effective piece in
teaching pizzicato
playing as a melodic
device. Most
often, pizzicato is
used as an effect or
punctuation mark to
larger melodic ideas.
There is a brief arco
section to provide
contrast and build up to
the dramatic return of
the main pizzicato
melody. Each section in
the ensemble has a
statement of the melody.
It is important to think
linearly in addition to
vertically when playing
these pizzicato lines.
Forward motion is of
up-most importance in
terms of making musical
phrases out of
these pizzicato lin
es.
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.
