Liv. En.- finish Reproduction packet for homework!
Global: study your notes
Thursday, February 26, 2009
Wednesday, February 25, 2009
Feb. 25, 2009
Global: Study your notes, DBQ tomorrow
Living Environment: homework tonight: first 2 pages of Reproduction packet.
Living Environment: homework tonight: first 2 pages of Reproduction packet.
Tuesday, February 24, 2009
Study for your geography quiz tomorrow
Global: hw: read "the frontier of knowledge" and answer question 1-5 on work sheet. study your map for tomorrow.
Es: signed test corrections due tomorrow.
Es: signed test corrections due tomorrow.
Monday, February 23, 2009
Spread of Islam Map
Thursday, February 12, 2009
Happy Birthday Mr. Ambraham Lincoln - 16th President of the US

Global: HW: create a new file flip:
Vocab cards: 14
Concept cards:5
ES: continue to study for your Energy Test for tomorrow.
Extra credit for ES is due tomorrow; you should try it.
What happens to the temperature of a block of ice when you put a Bunsen burner underneath it?
You might think that the temperature goes up smoothly, but that's not what happens. The graph of temperature against time is called a heating curve. Let's look at the heating curve for water.
A heating curve for water notice that, in general, the temperature goes up the longer the heating continues. However, there are two horizontal flat parts to the graph. These happen when there is a change of state. The first change of state is melting (changing from a solid to a liquid). The temperature stays the same while a substance melts. For water, this temperature is 0°C because the melting point for water is 0°C. The second change of state is boiling (changing from a liquid to a gas). The temperature stays the same while a substance boils. For water, this temperature is 100°C because the boiling point for water is 100°C.
Click the Macbeth image to connect to a site to read and quiz yourself.
Tuesday, February 10, 2009
Friday, February 06, 2009
Have a good weekend -STUDY YOUR NOTES
Global: Study for you Byzantine Empire test, it has been moved to next Thursday; 2/12.
ES: Energy test 2/13 Energy lab is due 2/9
FILL IN THE CORRECT GRAMMAR, PRINT OUT THE "CAMP" STORY AND PRINT OUT FOR EXTRA CREDIT. (APPROPRIATE WORDS ONLY!!)
ES: Energy test 2/13 Energy lab is due 2/9
Byzantine Empire
As the Western Roman empire disintegrated in the fifth century bce, Roman civilization continued to flourish, lasting as the Byzantine Empire in the Eastern Mediterranean for another thousand years. Centered on Constantinople--named for Constantine--aka New Rome, the Eastern Roman Empire existed as a unique mix of Roman law and urban life, Christianity, Greek culture and language, and a cosmopolitan population. As the dominant culture of the Eastern Mediterranean, Byzantine Rome distinctly shaped the politics, economies, religions and cultures of the newly-emerging states and societies in Eastern Europe, Russia and Anatolia. As such, Russia inherited a civilization much more directly linked to the Greek-speaking (and Orthodox Christian) world than to the Latin West. Russia also became the frontier/border between Europe and Asia.
As the Western Roman empire disintegrated in the fifth century bce, Roman civilization continued to flourish, lasting as the Byzantine Empire in the Eastern Mediterranean for another thousand years. Centered on Constantinople--named for Constantine--aka New Rome, the Eastern Roman Empire existed as a unique mix of Roman law and urban life, Christianity, Greek culture and language, and a cosmopolitan population. As the dominant culture of the Eastern Mediterranean, Byzantine Rome distinctly shaped the politics, economies, religions and cultures of the newly-emerging states and societies in Eastern Europe, Russia and Anatolia. As such, Russia inherited a civilization much more directly linked to the Greek-speaking (and Orthodox Christian) world than to the Latin West. Russia also became the frontier/border between Europe and Asia.
JUSTINIAN
The greatest of all the eastern emperors was clearly Justinian (c.482-565), who reigned for thirty-eight years between 527 and 565. Justinian was reformer in the fashion of Augustus Caesar. It was Justinian's desire to restore the Empire -- both East and West -- to all of its former glory. In fact, it has been said that his desire to restore the former Roman Empire was an obsession. His greatest accomplishment toward this end was the revision and codification of Roman law. Justinian understood that a strong government could not exist without good laws. Although the Romans prided themselves on their written laws, several centuries of written laws had brought nothing but confusion. In Justinian's day, a man could have spent a lifetime studying the laws without ever mastering them. The laws had grown too numerous and too confusing. Justinian created a commission of sixteen men to bring order out of all the laws. These men worked for six years and studied more than 2000 texts. In 534, the commission produced the Corpus Juris Civilis – the Body of Civil Law. The Corpus, written in Latin, became the standard legal work until the middle of the 19th century. As such, the Corpus is one of the most sophisticated legal systems ever produced and symbolized Justinian's efforts to create a reunited and well-governed Empire.
Justinian was clearly a man who was driven by his obsession. He was aided by his predecessors, who were able to fend off Germanic invasions, something the western empire could not do until much later. Justinian was also aided by his wife, Theodora (c.500-547), the daughter of a bearkeeper at the Hippodrome, and no less ambitious than her husband. Together, she and Justinian brought new energy to an old, conservative regime.
Justinian was clearly a man who was driven by his obsession. He was aided by his predecessors, who were able to fend off Germanic invasions, something the western empire could not do until much later. Justinian was also aided by his wife, Theodora (c.500-547), the daughter of a bearkeeper at the Hippodrome, and no less ambitious than her husband. Together, she and Justinian brought new energy to an old, conservative regime.
CLICK THE MAD GLIBS PIC TO LINK TO SITE.
FILL IN THE CORRECT GRAMMAR, PRINT OUT THE "CAMP" STORY AND PRINT OUT FOR EXTRA CREDIT. (APPROPRIATE WORDS ONLY!!)
Thursday, February 05, 2009
Grammar
A noun is a naming word.
It names a person, place, thing, idea, living creature, quality, or action. Examples:cowboy, theatre, box, thought, tree, kindness, arrival
Verb A verb is a word which describes an action (doing something) or a state (being something). Examples:walk, talk, think, believe, live, like, want
Adjective
An adjective is a word that describes a noun. It tells you something about the noun. Examples:big, yellow, thin, amazing, beautiful, quick, important
Adverb
An adverb is a word which usually describes a verb. It tells you how something is done. It may also tell you when or where something happened. Examples:slowly, intelligently, well, yesterday, tomorrow, here, everywhere
Pronoun
A pronoun is used instead of a noun, to avoid repeating the noun. Examples:I, you, he, she, it, we, they
It names a person, place, thing, idea, living creature, quality, or action. Examples:cowboy, theatre, box, thought, tree, kindness, arrival
Verb A verb is a word which describes an action (doing something) or a state (being something). Examples:walk, talk, think, believe, live, like, want
Adjective
An adjective is a word that describes a noun. It tells you something about the noun. Examples:big, yellow, thin, amazing, beautiful, quick, important
Adverb
An adverb is a word which usually describes a verb. It tells you how something is done. It may also tell you when or where something happened. Examples:slowly, intelligently, well, yesterday, tomorrow, here, everywhere
Pronoun
A pronoun is used instead of a noun, to avoid repeating the noun. Examples:I, you, he, she, it, we, they
TRY THIS: SUBMIT THIS ANSWER TO ME TOMORROW FOR EXTRA CREDIT.
Wednesday, February 04, 2009
Tuesday, February 03, 2009
Thursday, January 29, 2009
Living environment Mid-Term

Well, we received 5 inches of snow and an inch of ice yesterday causing Mahopac to cancel school yesterday. Hope you enjoyed the day like these two pooches. Now it's time to continue to study for your Living Environment test. It has been rescheduled for Monday 2/2/09 , (9:55am) same room number; Rm. 114 if you have Mrs. C. and Rm. 124 if you have Mrs. G.
Again, I cannot stress how important it is for you to continue your studies for this test.
SOME MOTIVATIONAL QUOTES TO INSPIRE YOU.
In my experience, there is only one motivation, and that is desire. No
reasons or principle contain it or stand against it.
Jane Smiley
reasons or principle contain it or stand against it.
Jane Smiley
Motivation is a fire from within. If someone else tries to light that fire under you, chances are it will burn very briefly.
Stephen R. Covey
Success is getting what you want, and happiness is wanting what you get.
Dave Gardner
The first and most important step toward success is the feeling that we can succeed.
Nelson Boswell
Desire is the starting point of all achievement, not a hope, not a wish, but a keen pulsating desire which transcends everything.
Napoleon Hill
Thursday, January 22, 2009
practice test for global midterm
TRY THIS TEST TO HELP YOU WITH YOUR GLOBAL MIDTERM CONTINUE TO STUDY FOR BOTH LIVING ENVIRONMENT AND GLOBAL.
Click --------->for online Topics tests for Living Environment Midterm
Scientific Method
Measurement
Tools (including Microscope)
Cells
Biochemistry (organic, pH, enzymes)
Cellular Respiration
Fermentation
Photosynthesis
Life Processes (pg. 16 in textbook)

GLOBAL: COMPLETE THE GLOBAL REVIEW PACKET FOR TOMORROW.
Living Environment:
Click --------->for online Topics tests for Living Environment Midterm
Scientific Method
Measurement
Tools (including Microscope)
Cells
Biochemistry (organic, pH, enzymes)
Cellular Respiration
Fermentation
Photosynthesis
Life Processes (pg. 16 in textbook)
Tuesday, January 20, 2009
Welcome President Obama
The mrlambertsupportpage.blogspot.com would like to welcome the United States of America's 44th President; Barack Obama. Good Luck and serve our country well.
Global Studies: Finish the Gladiator essay for tomorrow; also continue to study for your Ancient Rome test which is tomorrow.
HERE IS YOUR SCHEDULE FOR NEXT WEEKS MIDTERMS
IF YOU TAKE A DIFFERENT MATH, GLOBAL OR LIVING ENVIRONMENT CLASS THE ROOM ASSIGNMENTS WILL BE DIFFERENT. ASK YOUR TEACHER FOR THE ROOM NUMBER.
Friday, January 16, 2009
Global Studies
Watch this video on Gladiator combat to help you write your gladiator story. (due 1/21)
Enjoy the long weekend and remember the struggles of the American Hero, Dr. Martin Luther King Jr, who fought to bring justice, equality and civil rights to all mankind.
Thursday, January 15, 2009
Global
HW: Gladiator writing assignment due 1/21
Ancient Rome test 1/21
Schlacter's Global Midterm 1/27 at 9:55 in room 137
Cauthers Living Environment Midterm 1/29 at 7:40, Rm. 114
Gladiators
Only 10% of the gladiators died in the ring (gladiators were expensive to purchase and they were needed for more than one match)
The term ‘Bread and Circuses” is used to describe the free food given out at the gladiator fights and the atmosphere of the arena
Gladiator was derived from the Latin word Gladius which means sword
Ancient Rome test 1/21
Schlacter's Global Midterm 1/27 at 9:55 in room 137
Cauthers Living Environment Midterm 1/29 at 7:40, Rm. 114
Gladiators
Only 10% of the gladiators died in the ring (gladiators were expensive to purchase and they were needed for more than one match)
The term ‘Bread and Circuses” is used to describe the free food given out at the gladiator fights and the atmosphere of the arena
Gladiator was derived from the Latin word Gladius which means sword
Wednesday, January 14, 2009
Ancient Rome
Global: HW: read " the rise and spread of Christianity" answer questions 1-5.
CONTINUE TO STUDY FOR YOUR ANCIENT ROME TEST ON 1/21. STUDY YOUR FILE FLIP CARDS.
ES: ROCK LAB DUE & SIGNED GRADE REPORT DUE 1/16, ES MID-TERM IS 1/21 & 1/22
BEGIN STUDYING.
Tuesday, January 13, 2009
global studies
Global: read " A successful failure" answer questions 1-5. continue to study for ancient rome test 1/21.
ES: we are studying rocks and how they are formed.
1. Sedimentary
2. Igneous
3. Metamorphic
work on your rocks, rocks, and more rocks lab.
I. Igneous Rocks
1. The same geologic processes have always been at work.
2. These processes formed the Earth as it is today over a long
period of time.
B. Rock: - a group of minerals bound together in some way.
C. Igneous rocks form from molten rock.
D. Molten rock is called magma.
E. Rocks that cool underground are called intrusive or plutonic rocks.
1. Distinct mineral crystals are present
F. Rocks that cool quickly are extrusive or volcanic rocks.
1. Cool quickly, so very small mineral crystals are present.
G. Magma comes in different types, ranging from
600 to 1200 degrees C :
1. Felsic magma - High in SiO2 silicates. Light in color.
Typically forms at the top of a magma chamber because of
its lower density.
Examples : Granite, quartz, orthoclase feldspar
2. Mafic magma - Low in silicates. Denser material higher in
magnesium and iron. Dark colored minerals form in this. Typically forms at the bottom of a magma chamber.
Examples : Basalt, hornblende, augite, biotite.
H. Igneous rock textures:
1. Crystal size is dictated by the rate of cooling of the magma
body. A slower cooling rate results in larger mineral
crystals being formed in the rocks as they cool.
2. Porphyritic texture - Large crystals surrounded by fine
grained rock. The rock initially cools slowly to form some large crystals and then cools quickly to form the fine grained rock surrounding them.
I. Common igneous rocks
1. Granite - Felsic. Coarse grained rock high in quartz,
micas, and feldspar
2. Gabbro - Mafic. Large crystals. Dark minerals dominant,
3. Rhyolite - Light colored, fine-grained igneous rock.
4. Obsidian - Cools very quickly. Forms volcanic glass.
Conchoidal fracture.
5. Pumice - Felsic lava that hardened with a lot of gases in it.
Many air bubbles in it make it possible for this
mineral to float on water.
II. Sedimentary Rocks
A. 3 kinds of sediments make up sedimentary rocks:
1. Clastics - fragments of other rocks.
2. Chemical - minerals that precipitate out of a watery
solution
3. Organic - Remains of plants and animals.
B. Clastic Sedimentary Rocks
1. Fragments that make up these rocks come in many sizes
and shapes.
2. Come from the erosion or weathering of pre-existing rocks
on land or underwater.
3. Sediments are cemented together with either silica, calcite,
or iron oxide.
4. Sediments running into a body of water are sorted by size
primarily. Larger particles settle out first because they're
heavier. Lighter silts and clays settle out last because of
their light weight.
5. 3 types of clastic rocks:
a. Conglomerate - Large rounded pebbles and sand
grains cemented together in rough
water.
b. Sandstones - Mostly grains of quartz. Many pores in
it can cause 30% of it to be air! Water
can usually pass through it.
c. Shale - Tiny flakes of the mineral kaolin are cemented
together. Easily broken. Usually form from
muds.
C. Chemically originated sedimentary rocks
1. Usually form when swamps, lakes, ore seas evaporate.
2. Limestone - Tiny grains of calcite cemented together.
3. Rock salt (Halite) - Table salt. Crystals form as seas
evaporate.
4. Gypsum - Form from evaporating seas as well. Main
ingredient of wallboard.
D. Organic Sedimentary Rocks
1. Mostly limestone and coal.
2. Organic limestones form from the shells of dead
microscopic organisms and the shells of ancient marine
mollusks.
E. Stratification is the visible layering of many sedimentary rocks.
Gives geologists clues about how rocks had formed.
III. Metamorphic Rocks
A. Regional Metamorphism, where certain areas of the Earth's crust
undergo extreme heat and pressure form most metamorphic
rocks.
B. When shale undergoes metamorphism, it can form many new
minerals:
1. Slate - 1st rock formed when shale is metamorphosed.
2. Schists - Named for primary mineral in it. Larger crystals present.
3. Gneiss - Coarsest grained metamorphic rock. Minerals form in bands in the rock. Usually light vs. dark colored bands
C. Contact metamorphism occurs when hot magma melts the rocks
in contact with it. Chemicals can react with the rocks along with
the heat and pressure.
ES: we are studying rocks and how they are formed.
1. Sedimentary
2. Igneous
3. Metamorphic
work on your rocks, rocks, and more rocks lab.
MID TERM IS NEXT WEEK DURING CLASS.
I. Igneous Rocks
1. The same geologic processes have always been at work.
2. These processes formed the Earth as it is today over a long
period of time.
B. Rock: - a group of minerals bound together in some way.
C. Igneous rocks form from molten rock.
D. Molten rock is called magma.
E. Rocks that cool underground are called intrusive or plutonic rocks.
1. Distinct mineral crystals are present
F. Rocks that cool quickly are extrusive or volcanic rocks.
1. Cool quickly, so very small mineral crystals are present.
G. Magma comes in different types, ranging from
600 to 1200 degrees C :
1. Felsic magma - High in SiO2 silicates. Light in color.
Typically forms at the top of a magma chamber because of
its lower density.
Examples : Granite, quartz, orthoclase feldspar
2. Mafic magma - Low in silicates. Denser material higher in
magnesium and iron. Dark colored minerals form in this. Typically forms at the bottom of a magma chamber.
Examples : Basalt, hornblende, augite, biotite.
H. Igneous rock textures:
1. Crystal size is dictated by the rate of cooling of the magma
body. A slower cooling rate results in larger mineral
crystals being formed in the rocks as they cool.
2. Porphyritic texture - Large crystals surrounded by fine
grained rock. The rock initially cools slowly to form some large crystals and then cools quickly to form the fine grained rock surrounding them.
I. Common igneous rocks
1. Granite - Felsic. Coarse grained rock high in quartz,
micas, and feldspar
2. Gabbro - Mafic. Large crystals. Dark minerals dominant,
3. Rhyolite - Light colored, fine-grained igneous rock.
4. Obsidian - Cools very quickly. Forms volcanic glass.
Conchoidal fracture.
5. Pumice - Felsic lava that hardened with a lot of gases in it.
Many air bubbles in it make it possible for this
mineral to float on water.
II. Sedimentary Rocks
A. 3 kinds of sediments make up sedimentary rocks:
1. Clastics - fragments of other rocks.
2. Chemical - minerals that precipitate out of a watery
solution
3. Organic - Remains of plants and animals.
B. Clastic Sedimentary Rocks
1. Fragments that make up these rocks come in many sizes
and shapes.
2. Come from the erosion or weathering of pre-existing rocks
on land or underwater.
3. Sediments are cemented together with either silica, calcite,
or iron oxide.
4. Sediments running into a body of water are sorted by size
primarily. Larger particles settle out first because they're
heavier. Lighter silts and clays settle out last because of
their light weight.
5. 3 types of clastic rocks:
a. Conglomerate - Large rounded pebbles and sand
grains cemented together in rough
water.
b. Sandstones - Mostly grains of quartz. Many pores in
it can cause 30% of it to be air! Water
can usually pass through it.
c. Shale - Tiny flakes of the mineral kaolin are cemented
together. Easily broken. Usually form from
muds.
C. Chemically originated sedimentary rocks
1. Usually form when swamps, lakes, ore seas evaporate.
2. Limestone - Tiny grains of calcite cemented together.
3. Rock salt (Halite) - Table salt. Crystals form as seas
evaporate.
4. Gypsum - Form from evaporating seas as well. Main
ingredient of wallboard.
D. Organic Sedimentary Rocks
1. Mostly limestone and coal.
2. Organic limestones form from the shells of dead
microscopic organisms and the shells of ancient marine
mollusks.
E. Stratification is the visible layering of many sedimentary rocks.
Gives geologists clues about how rocks had formed.
III. Metamorphic Rocks
A. Regional Metamorphism, where certain areas of the Earth's crust
undergo extreme heat and pressure form most metamorphic
rocks.
B. When shale undergoes metamorphism, it can form many new
minerals:
1. Slate - 1st rock formed when shale is metamorphosed.
2. Schists - Named for primary mineral in it. Larger crystals present.
3. Gneiss - Coarsest grained metamorphic rock. Minerals form in bands in the rock. Usually light vs. dark colored bands
C. Contact metamorphism occurs when hot magma melts the rocks
in contact with it. Chemicals can react with the rocks along with
the heat and pressure.
Monday, January 12, 2009
Global, living environment
(25 multiple choice questions)
One way passage
Gastrointestinal tract
Extracellular digestion
PERISTALSIS: rhythmic muscular contraction, moves food down digestive tract

One way passage
Gastrointestinal tract
Extracellular digestion
PERISTALSIS: rhythmic muscular contraction, moves food down digestive tract
Thursday, January 08, 2009
Interactive human body
Click the Mr. Bones to take you down the incredible path called the Human Body. You may have a test tomorrow or possibly Monday in LIVING ENVIRONMENT class on digestion and respiration.
Global: read "struggle for Equal Rights" & answer ques. for review 1-5
upcoming: Ancient Rome test on 1/21. (study your notes and File flips)
global MID TERM ON 1/27 (MULTIPLE CHOICE & dbq)
Click here for another tutorial about the human body systems.
Global: read "struggle for Equal Rights" & answer ques. for review 1-5
upcoming: Ancient Rome test on 1/21. (study your notes and File flips)
global MID TERM ON 1/27 (MULTIPLE CHOICE & dbq)
Click here for another tutorial about the human body systems.
Tuesday, January 06, 2009
Global & Living Environment
Global: create a new file flip with 24 vocab cards and 8 concept cards. Also, Complete packet on the geography of Italian Peninsula.
Living Environment: "quiz" on Respiration and Digestion Friday… might be postponed depending on tomorrow. (STUDY FOR THIS QUIZ, THE WEATHERMEN MAKE MISTAKES TOO)
Living Environment: "quiz" on Respiration and Digestion Friday… might be postponed depending on tomorrow. (STUDY FOR THIS QUIZ, THE WEATHERMEN MAKE MISTAKES TOO)
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