Thursday, June 23, 2016

Notes: The China Tea Book

The China Tea Book Luo Jialin

Part 1 TEA

Overview 1
Green -energetic as the youth
Oolong -reserved and mature as a middle aged man
Black Tea - Maternal love
Pur-erh- incarnation of a wise old man with a lot of stories

Production of Tea
harvesting -plucking tender leaves. Most tea is from buds. Oolong is full leaf

withering - partial dehydration of fresh leaves (Green tea does not require withering or fermentation)

fermentation-  Using air to stimulate oxidation (oolong varying levels, black tea 100%)

fixation - using high temperature to kill leaf cells and terminate fermentation

rolling - rupturing cell walls and shaping leaves (green tea lightly rolled, black heavily rolled. Oolong any way)

drying- removing excess moisture via steaming - stabilizes the key properties such as flavor

scenting/ rolling - causing leaves to absorb a floral fragrance-properties of a flower

Roasting -using fire to dry roast the leaves - heavier , more mature -- rock tea (oolong) is heavily roasted

Tea & Your Health
Tea has 'tea polyphenols', which are catechin based substances.
alkaloid in tea leaves is caffeine
amino acids such as thiamine - 2-5%
water soluble vitamins vitamin c and b group. Also, fat soluble vitamins, such as A. (have to eat tea leaves for A)
minerals - potassium- osmotic pressure and blood balance, as well as renewal of cells
Manganese, selenium, zinc and calcium.
Lipopolysaccharides that improves that body's ability to manufacture blood, strengthen immunity and resist the effects of radiation. --C, B1, B2, B3, B5, B11 H

Storage of Tea- stored away from light. It should also be stored in airtight jar and stored away from moisture. -- Pu-erh ages and should be stored in bamboo, paper or cloth. Black tea is good for sachet.

Green Tea 2



It is good to brew in it a clear teapot because then you can see the green tea leaves unfold. Green tea likes to be boiled at a low temperature, 175F. If it is brewed at a higher temperature nutrients and minerals are lost. Also, the tea becomes bitter and loses vitality. Pick cups that can dissipate heat rapidly. - cup choice is important. 

Dragon Well Tea


From the time of Emperor Qianlong of the Qing Dynasty, the name comes from a well. This well did not dry up during long droughts. People believed that the dragon of the seas lived there. On the well near Hangzhous West Lake to Xishi. 

Green Spiral Tea

 Famous tea from Suzhou, it is cultivated within the east and west Dongting Mountains in Taihu Lake. Green Spiral Tea is grown with various fruit trees that protect the plants in shade and keep them from freezing over. 

Mount Meng Sweet Dew

From Sichuan, growing on mountain tops, is the Mount Meng Tea. It was the first tea to be cited on ancient documents and was given to the emperor. 

Bamboo Leaves Green Tea


This tea has lasted less than half a century and is grown on mount E'mei/ It was classified as an imperial tribute, during the Tang dynasty, It was christened by General Chen Yi. 

Oolong Tea 3 - the Mature Tea of a Middle Aged Man
Fermentation of oolong is based on Tea Tree variety and on cultural factors. The more fermented the tea, the redder it looks and the more challenging it is to identify the original flavors of the tea. Rock Tea must be roasted to produce it. Roasting reduces the lightness of the liquor. Water usIt is generally ahverested in spring and winter ed for Oolong should never exceed 195 degrees F. The more heavily fermented the tea, the hotter the water has to be. Red porcelin pots are typically picked for Oolong tea. It is generally harvested in spring and winter. White tip oolong the exception because of buds

Wuyi Rock Tea



It is from the Fujian Province and each tea bush takes root on rock cliffs. It was the cradle to the philosopher Zhu Xi's Neo-confucian philosophy. The primodial ancestors of the tea are four ancient tea trees on a Tianxin Cliff, where the words "Big Red Robe" have been written. Or it might be that the farmers blended a variety and claimed it was the orginal tea, beacause it is now extinct. Big Red Robe, Golden Water Turtle, White Cockscomb and Iron Arhat- High degree of fermentation and roasting. "Craggy Charm" - It is a recluse tea- not changing - Ming Emperor cured of illness draped the tea in red robes.

Iron Mercy Goddess 


Semi-fermented Oolong tea. It is cultivated in Anxi, Fujian Province.  Temperature should be no higher than 195F  or less. To taste good, when brewed, the leaves should unfold.

Frozen Summit Oolong 
Light fermentation and emphasis on Aroma. A Taiwanese tea. 

White Tip Oolong
It is only grown in Taiwan. Only variety of tea that uses buds. It is heavily withered and fermented. Harvested before the Qingming festival. Flavor is believed to be produced by the bites of a grasshopper. -Bitten Tea--Boast Tea- it is a rarity and historically expensive



Black Tea 4

In Chinese, black tea is 'red tea', which is the color of the drink after it has been brewed. Black tea is heavily fermented. Black Tea can be brewed in water exceeding 195 F and is made of buds and tender leaves.

Keemum and Dian Hong

During Tang Dynasty, Keemun was a known production place for tea. Though during the tang dynasty, green tea was produced not black. That changed with the Qing dynasty.  

Lapsang Souchong

Like Rock Tea, Lapsand Souchong is grown in the wuyi mountains. This was one of the first varieties that was introduced to the western world. During the drying and withering process, a pine-scenting process is added. It is chopped up for international markets, but it is important to try to tea in its rolled form. 

Pu-erh Tea 5

It is believed to be good company when we want to lose ourselves in meditation or seeking inner peace. Pu-erh is a dark tea, and it is post fermented, meaning that its fermentation never fully stops. The tea changes with age. Pu-erh takes its name from its production in the Pu-erh county, yunnan province. It is a broad leaf tea that is compressed into cakes and bricks. --raw and ripened categories--wet piling. Pu-erh break down fats. It is believed to prevent cancer and help with cardiovascular disease. brewing methods enhance flourine content.




Part 2 TEA CULTURE 
To start we need to focus on the principle of tea culture. 
Principles 6

Time - two types of time-- the physical domain and the abstract/ sentimental. Green tea is best for morning. Oolong for midday. And roasted Ooolong, black tea and pu-erh for afternoon and evening.--More heavily fermented tea should be in the evening-- pur-erh last. 
-no man steps in the same river twice. 

Space -Tea settings space. A theme is a defining feature for a tea setting. Differentiate between decoration and function. The boundaries between these two may blend. Teahouses, mountains or gardens...Japanese culture tends to have tea houses. For drinkers in ancient china, one could not appreciate tea without drinking in the mountains or close to water. Tea houses in china fill the niche that cafe in western societies provide. Even strangers are expected to greet each other in a friendly way. Servers are almost intimate in their relationship to the customers. Operas are held in tea houses. 

Teaware-  Ingredients - dry leaves/ water, people who brew tea, tea utensils--teaware with time will survive throughout the ages. Sancia cup for green tea. -- nature themes utensils.  

Ambiance --Incense burning came into being in the spring and autmn period of the warring states period. Did not gain maturity til Sui and Tang Dynasties. Later, it was introduced to Japan. Long parties- you can show how incese is made.. shorter parties, you can just burn the incense. boned incese or boneless incense. Incesne should not interfer or distract from tea drinking. Flower arrangement- maturity during Sui and Tang dynasties. Pick flowers without a strong scent. Flowers should go with the theme. Musical playing can be at end of party or between servings. Traditional zither...selecting music is based on theme of the party. 

Ancient Chinese Tea Culture 7
Chinese art centered on calligraphy and painting- hanging scrolls or handscrolls. For a long time, poetry reigned over all other art forms. 

Poetry- Chinese Tang poet Jiao Ran makes the poem "drinking tea" that defines the tea ceremony/ experience. Li Bai wrote a poem exemplifying his gratitude for getting cactus tea.Tang Poet Yuan Zhen made a pyramid poem of the shape and color of tea leaves and what fun it is to drink tea in the moon light. Sang Dynasty, poetry became broader and rules and motif of tea came into discussion. --Cold food Festival and Qingming Festival. Chon'er prince and accidentally burning alive his servant tale. Song poem by Sui Sui speaks of homesickness and tea - "we can do nothing but seek joy admist sorrows'Song poet Huang Tingjian made a poem relating tea drinking to 'meeting up with an old friend after a long time" Ming and qing synasties focused on novels. In novel " A dream in Red Mountains" readers can find descriptions of tea. Tang and song dynasties, tea was in short supply and required a complicated process to brew it. 

Calligraphy- It evolved from the oracle bone script, drum script, great seal script, lesser seal script, clerical script to the cursive script, regular and running. The meaning and aesthetics of script are both important. Song dynasty Cai Xiang calligrapher made a treatise' notes on tea'--Su was also recognized for his experise on tea-- he documented how to take care of your teeth, using tea. Ming and Qing dyanasties Xu Wei made "seven procedure to brew tea"  

Painting -"scroll of Exemplary Women' by Gu Kaizhi in Jin Dynasty. Zhou Fang "playing Zither and Drinking Tea"Ming  Dynasty Ding Yupeng "Yuchuan brews tea" 


TEA and Zen 8
Tea associated with the meditative state of zen practice. This idea reached maturity during the Song Dynasty. --valued unexpected comprehension . Sage of Tea, Lu Yu was a buddist follower. In Tang and Song Dynasties, Two monks named Jianzhen and Eisai introduced tea to Japan. Real Tea lovers will make the best out of an imperfect cup of Tea. This is a type of Zen Thought. "Let it be" and ' All are equal" --Tea forethought and introspection are a microcosm of greater life. 

Dissemination 9
Tang Dynasty- Steaming Tea
Song Dynasty - Whisking the Tea
Ming Dynasty -Steeping
Japan- Matcha

Historically Tea was grown in South China.
Beijing known for scented tea
Assam black is made from original trees
Darjeeling Black was originally grown in china

Japanese Tea ceremony 

Senchado
Heian Era, the tea brewing method of the Tang Dynasty was introduced to Japan.
Momoyama Eras- Whisking method spread from Song to Japan.
Edo Era- steeping from Ming was introduced =, giving rise to various schools.
Japanese Tea Ceremony - Murata Juko, Takeno Joo and  Sen no Rikyu
Japanese saw it as form of spiritual expression
Japanese Tea ceremony has thought and performance about it
The book of tea by Okakura Tenshin   

Ancient Tea Route 
Central China and Tibet Route-created ancient Tea Route- Older than Silk Road and passes huge mountains - roof of the world. 







List of Gardening Resources -On Going-- Edit

Kobuto Gardens - Next door - Volunteer on Tuesday Mornings
Dirt Corps -http://www.urbansystemsdesign.com/#!dirt-corps-program/cpt7
Seattle Tilth - http://www.seattletilth.org/

Drop in Parties
  • Rainier Beach Urban Farm and Wetlands (SE Seattle)
    5513 S. Cloverdale St; Seattle 98118
    Wetlands restoration and food forest work
    Fridays, 10 a.m.-12 p.m.
    Questions? Contact lizzystone@seattletilth.org
  • Good Shepherd Center Adult Learning Garden (Wallingford)
    4649 Sunnyside Ave N; Seattle 98103
    Garden is located on the southeast side of Meridian Park
    Fridays, 11 a.m.-1:30 p.m.
    RSVP appreciated 2-3 days in advance to suehartman@seattletilth.org
  • McAuliffe Park Learning Garden (Kirkland)
    10824 NE 116th St, Kirkland, WA 98034
    Help prepare the garden for a productive growing season
    Thursdays, 4-7 p.m.

Start Your Fall and Winter Garden

EmailPrint
Wetlands Steward


Bellevue Gardens 
Horticultural Assistance 
Work with Garden staff or interns to plant, prune, create and maintain paths, and detail the garden. Tuesday or Thursday mornings, 9:00 to 11:00 AM.
Work with a group of volunteers that concentrates its efforts in the Waterwise Garden, first and third Wednesdays of the month from 1:00–3:00 PM.


Work with the Northwest Perennial Alliance.The Alliance concentrates their efforts in the Garden's Perennial Border.
Work parties are most Thursdays from 10:00 AM–12:00 PM. Email the Alliance or visitwww.northwestperennialalliance.org

Garden d’Lights installation, creation and take-down: Join the team that creates, maintains and installs the lights displays.

http://www.bellevuebotanical.org/volunteer.html

South Seattle Community College Horticultural Program 

Seattle Japanese Garden http://seattlejapanesegarden.org/index.html
Moon Festival 

Northwestern Chapter of North American Rock Garden Society http://www.nargsnw.org/


List of Gardening Resources -On Going-- Edit

Kobuto Gardens - Next door - Volunteer on Tuesday Mornings
Dirt Corps -http://www.urbansystemsdesign.com/#!dirt-corps-program/cpt7
Seattle Tilth - http://www.seattletilth.org/

Drop in Parties
  • Rainier Beach Urban Farm and Wetlands (SE Seattle)
    5513 S. Cloverdale St; Seattle 98118
    Wetlands restoration and food forest work
    Fridays, 10 a.m.-12 p.m.
    Questions? Contact lizzystone@seattletilth.org
  • Good Shepherd Center Adult Learning Garden (Wallingford)
    4649 Sunnyside Ave N; Seattle 98103
    Garden is located on the southeast side of Meridian Park
    Fridays, 11 a.m.-1:30 p.m.
    RSVP appreciated 2-3 days in advance to suehartman@seattletilth.org
  • McAuliffe Park Learning Garden (Kirkland)
    10824 NE 116th St, Kirkland, WA 98034
    Help prepare the garden for a productive growing season
    Thursdays, 4-7 p.m.

Start Your Fall and Winter Garden

EmailPrint
Wetlands Steward


Bellevue Gardens 
Horticultural Assistance 
Work with Garden staff or interns to plant, prune, create and maintain paths, and detail the garden. Tuesday or Thursday mornings, 9:00 to 11:00 AM.
Work with a group of volunteers that concentrates its efforts in the Waterwise Garden, first and third Wednesdays of the month from 1:00–3:00 PM.


Work with the Northwest Perennial Alliance.The Alliance concentrates their efforts in the Garden's Perennial Border.
Work parties are most Thursdays from 10:00 AM–12:00 PM. Email the Alliance or visitwww.northwestperennialalliance.org

Garden d’Lights installation, creation and take-down: Join the team that creates, maintains and installs the lights displays.

http://www.bellevuebotanical.org/volunteer.html

South Seattle Community College Horticultural Program 

Seattle Japanese Garden http://seattlejapanesegarden.org/index.html


Wednesday, June 22, 2016

Washington Butterfly Association

http://wabutterflyassoc.org/

Hikes

https://www.theoutbound.com/scott_kranz/8-amazing-spring-hikes-near-seattle

Monday, June 20, 2016

Notes: Geology of PNW

Geology of The Pacific Northwest: Investigate How the Earth was Formed by Nomad Press

Chapter 1 - Plate Tectonics Shape Our Land and Sea
Plate Tectonics - theory that was developed in the 1960s

A peek inside the earth

Crust- thin layer of the earth
Mantle -layer below the crust. 
Lithosphere- the crust and mantle together and is broken up into plates.
Asthenosphere- is partially melted and is viscous. 
Core- Center of the earth 9000F or 5000C

The Lithosphere is broken up into 12 major plates. There are also a few smaller plates. The plates are always moving slowly. The asthenosphere is very hot and plates move because of convection. Plates can move 1 to 6 inches a year. At plate boundaries, Volcanoes form.
Divergent Plate Boundary - plates are moving against each other
Convergent  Plate Boundary- are where two plates collide. (Sometimes a oceanic plate collides with a continental plate, and since the oceanic plate is denser and thinner, it slides underneath- this is called subduction. 

A subducting plate can cause a lot of heat and pressure. This causes the release of heat to the surface. Magma rises to the surface, creating volcanoes.  (Sometimes plates just slam into each other and create volcanoes. Sometimes, plates just grind each other, creating earthquakes)

Hotspots are small hot regions inside a plate (yellowstone is an example- magma is flowing to the top for some reason)

750 million years ago Rodinia broke apart, the rift was at the western edge of Idaho today. An ocean formed there. (Some of the oldest rocks in the pnw can be found there). Pangea formed 200 million years ago. Pangea broke apart and atlantic ocean formed. An rocky oceanic plate subducted under the north American plate. Sediments were scraped off to form Oregon and WA. 7 and 4 million years subduction became steeper and cause the edge to fold. The Olympic mountains are the crest of that fold. 

Alaska is complicated. It's filled with all sorts of crazy rocks from everywhere. 

Review of  Rodinia and Pangea - the big basin in montana --when  Rodinia broke apart it created a basin. Sediments rushed into the basin. These belt rocks are near Montana and Idaho in glacier national park.   





Currently the Juan de Fuca plate is subducting into the north American plate, creating the active cascade mountains.

Another plate is subducting in Alaska, that is forming the Aleutian Islands. Alaska coastal mountains.

Exercise; Cut Candy Bar and watch plate tectonics

3 Types of Rocks
Igneous Rocks- have formed from the cooling of molten rock - think basalt
Sedimentary Rock - when small sediments of rock are pressed tightly into rock
Metamorphic Rock- when heat and pressure forms into new rocks

The rockies were formed 90 million years ago. The rockies are a fold and thrust belt. The rocks on the top of the rockies are old - probably half a billion years older (western Montana and Idaho- glacier national park.

The Coast range mountains (Olympics, Oregon coast range and Klamath Mountains)- Lots of recycling of rock is happening.

Cascade Mountains - volcanoes
Denali is highest mountain in alaska. The brooks range- Artic National Wildlife Refuge
The Alaska range contains Denali
The coast mountains in Canada are highest mountains near a coast (some only 10 miles)

Mt Rainier- 14,411 feet - if it erupted, huge mudslides were cascade down the mountain. 26 glaciers and has a huge network of glacier caves, formed from volcanic gas.
Mt hood 11, 249 feet
Borah Peak 12,668 in Idaho

Things to tell if a glacier has been around- Grooves, U shaped Valley, Hanging Valley, Horns (mounatains), Cirques, Moraines

1986 Hubbard Glacier dam broke- huge and powerful flood.

Volcanoes
Shield Volcanoes-
Stratovolcanoes
Cinder Cones
Volcanic Domes

1989 a jet plane flew over active mount redoubt. It nearly destroyed the engines.
Mt St Helens -1980
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The Mating Game


Mariposa (En Havana)

by Si Se
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Lava Tubes in Lava Beds National Monument Park in North Eastern California

Crater Lake in Oregon is the Caldera of Mt Mazama. It is the ninth deepest -lake in the world.
Newberry Volcano- Shield volcano -geothermal energy
Mt Novarupta and Mt Katmai -statovolcanoes in Alaska -Ask Build up - The Valley of Ten Thousand Smokes is part of the Katumai NAtional Park and Preserve

Richter Scale is logarithmic.

1964- Great Alaskan Earthquake near Anchorage Alaska. It was a 9.2. 
1960 -9.5 earthquake in Chile 

Basins and Plateaus 
Basalt Columbia Intermontane-100,000 square miles across Washington, Oregon, Idaho and area of northern Neveda (259,000)- used to be a ocean of hot lava flows. Multomah Falls, oregon side of columbia gorge..An interesting feature of basalt is that when it cools, it can form vertical columns of 5, 6 or 7 sides. 
1783- eruption in Iceland that lasted 8 months and produces 3 cubic miles of lava. It killed 10,000 and starved half the countries livestock. 

It is not known why flood basalts' happen. There is the big plume theory, the delamination theory (lower part of lithosphere splits off and sinks into mantle), Theory of both

Mega Flood- 16,000 years ago near the end of the ice age. Channeled Scablands -Glacial Lake Missoula was a lake formed in montana. 2,000 feet deep and 200 miles long. Flood water raced at 65 mile per hour. 13 -70 flood occurred. 

Snake River Plain is flat 400 mile-long depression containing basalt rocks. Geologists believe that snake Inidan plain formed in the same plume of magma that caused the Columbia river basalt. The great rift zone (50 miles long)- contains craters of the moon national monument and preserve. It has volcanoes, ropy, basalt and lava tubes. 
Magma plumes experiment - oil and water to make lava lamp 
magma basalt columns - let cornstarch solution dry out in sun 

Climate - latitude, nearness to ocean, altitude, and Jet-streams
Seattle is cloudy because the jet stream carries air from the west, and lots of evaporated clouds.  Seattle has Mediterranean climate - Jet stream moves to Canada during the summer- that is why it is so dry. 

It tends to rain on the mountains because the moist air rises to get over the mountains, but as it condenses in to cool air, it rains. Rain Shadow. Chinook Wind- a warm chinook wind can melt a foot of snow in a day. 1979, Loma, Montana - the temperature rose from -56 degrees to 49 degrees  F. Montana 1980 great falls 47 degree F in just 7 minutes.
Pineapple express - warm moist air. --polar night and midnight sun



Aurora borealis caused by solar wind with earth's upper atmosphere. Particles are attracted to south and north poles, due to magnetic attraction. 
Rain Gauge experiment
Fog experiment - match, ziplock bags, cup and icecubes
Cape disappointment is foggiest place in US. Warm air passes over colder ocean. 
Watershed- a land area that drains into a river or stream
Yukon, Columbia -Snake River system. Columbia river system is 4th largest river in US by water volume. Due to rapids (settlers had to portage) and large sandbars, 2,000 boats have sunk in Columbia river. 
Fish- Chinook (king), Chum, Coho, Pink and Sockeye - anadromous-- Hell Canyon is deepest canyon in US. 
Hydroelectric Dams- pressure can burst the swim bladders in fish, increase temperature in water. Largest salmon was caught in Kenai river in Alaska- it weighed 100 pounds. -Elwha Restoration
Yukon River - 1,982miles in Alaska interior- Barges are an efficient form of transportation  

Ecosystems Tundra- plain where soil below surface is frozen. Temperate rainforest- rainforest in temperate zone.  -epiphytes, mosses, ferns and lichens 39 - 54 degrees F. High level of biomass. Alaskan Rainforest has Fjords
Features of Olympic Forest - 8 species of fern, 500 year old trees that are over 200 feet tall (Douglas firs, hemlocks), Glacial flour of rivers - roosevelt elk, black bears, marmots, bats and river otters
birds - woodpeckers, marbled murrelets and spotted owls 
Bracket fungus- honey mushrooms in Malheur National Forest in Eastern Oregon is considered world biggest organism- 8,000 years old and cover 2,224 aces

Nurse Logs- 96% of big spruce and hemlock start on nurse logs. 1 in 10,000 becomes a tree. 
Tundra- permafrost -in summer tundra turns to marsh and pools water, Lichens are good food for caribou.--Artic tern Migrates between Arctic circle and antartica--experiences more sunlight then any other creature. 
Terrarium Experiment
The coast- ocean temperatures impact climate. Alaska is warmer because warmer water is hitting it from the south. Pacific Currents are colder. Upwelling- When colder, denser, nutrient rich water rises to the ocean surface. Colder water has more nutrients than warmer water - phytoplanton. half the world's fisheries happens where upwellings happen. 
Coastlines don't have distance because they are almost impossible to measure due to complexity. Reedsport Oregon - A wave energy park, using nuoys algal bloom - phytoplanton multiply out of control - Kelp are incredible underwater seaween forests. Kelp harvested for algin, alginic acid, nori or carageenan, Kelp love rocky surfaces and can grow a foot a day. Marine mammals - cetaceans (whales, dolphines and porpoises) 
pinnipeds (walruses, seals and sea lions)
Estuaries








Sunday, June 19, 2016

Notes - The Story of Earth

The book, The Plant Hunters: Two Hundred Years of Adventure and Discovery Around the World by Toby Musgrave, Chris Gardner, Will Musgrave, altered my perspective. While hiking, I am daydreaming about collecting seeds.

Currently, the maple trees are producing massive quantities of seeds ( the Maple's are stressed). I'd love to germinate a few trees.

I already have a small batch of maple seeds collected, and I am waiting for them to dry out. I want to try the process of stratification.
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Last weekend, I read the book The Story of Earth: The First 4.5 Billion Years, from Stardust to Living Planet by Robert M. Hazen.

Reading books in not enough, I think spending a little time to try to process the information is helpful. Since this book is written in clear chapters, I'm just going to review what was in the chapters again.



1. Birth - The Formation of the Earth
The book starts out like any typical story of the big bang, and then from big bang, Hazen talks bout the formation of the stars. He talks about the formation of the sun and the elements. How gravity sucks hydrogen together to make a star, and how the compression of hydrogen leas to fusion.

This compression lends itself to a fusion inspired dance. Gravity compresses, fusion of hydrogen creates helium. Helium fuses to create carbon. carbon to make neon. neon to oxygen. Then magneium, silicion sulfur and etc.... The last stage of a huge star last only a day, it makes lead, then a star explodes

He talks about how our solar system started out as a gaseous nebula and how an exploding star nearby triggered the formation of our solar system. 4.6 billion years ago, the presolar gasses spun faster and faster, making a centralized core and a flattened pattern of gasses.



For clues of this time period, there are meteorites. The 4.566-billion chondrites
When the sun first formed, an intense radiant energy broiled the nebula, creating rocky droplets, called chondrules. (After the ancient greek word for grain)

A younger group of rock is called the anchondrites..They have been melted a reworked.  
They represent a host of exotic meteorite types such as Howardites, eucrites, diogentites, ureilites, acapulcoites, lodranites ---most named for locality where they were found

Pallasite - snatch a core-mantle boundary --shiny metal mixed with cystals of olivine



 2. The Big Thwack- The Formation of the Moon

About 4.5 billion years ago, a proto earth and a smaller planet were in competition for the same space in the solar system.  The smaller planet is called Theia (Theia the titan goddess who gave birth to the moon) Theia was a 1/3 of the earth mass. Both of the planets collided and formed the earth and moon. At the Roche limit, the moon formed 15 miles up. Moon lacks volatiles because they were blasted away and it lacks an iron core becuase that core ended up with earth.

Currently, the moon is 239,000 miles away. It inches away 3.82 centimerers every year. In early eath, the moon was huge and volcanic. It would have been bright and would have blcoked out the stars in the sky. Total angular moment of the system hasn't changed that much. 4.5 million years ago, everything was spinning fast. It still took 8,766 hours to go around the sun, but days were only 5 hours long. the moon only took 84 hours to go around the earth. Monster volcanic tides were found on earth.

3. The Black Earth - The formation of the Basalt Crust
The earth cooled via conduction, Convection and radiation.
Olivine crystals started to form. Sinking into the magma depths.

Magmas became depleted in magneisium  and were more concentrated with calcium and alumnimum. 
On moon, a second cystal formed along olivinr, anorthite.

On earth, with greater pressures pyroxene appeared.

They formed in a hard rock called peridotite

Early  peridotite crust sank.

Basalt comes about. Two varieties are plagioclase and pyroxene.
As masses of peridotite formed and sank, they were reheated and half-melted. The repeated half melting of peridotite changed to the composition of the rock. 
Basalt does nt have many crystals. Diabase and gabbro. Earth had a basalt crust that floated above magma. 



4. Blue Earth - The Formation of the Oceans

For some reason, earth volatiles did not evaporate. This is not the case with other planets. It lost some water when it collided with Theia, but on a whole earth has kept a large percentage of its water. Earth probably has a vast resevior deep underground. Maybe it stayed because of earth's magnetic field (???)

In Western Australia, in the Jack Hills, Some of the oldest rocks are found. Zirconium seeks its own kind and forms tiny crystals. Zirconium crystals are impressively stable, they can get heated and recycled in rock and not lose their structure. Some of them are known to be 3 billion years old. Zirconium crystals can tell time because they can incorporated uranium, and uranium's decay is a useful clock. Two of every 3 atoms are oxygen, which gives clues about temperature formation ( Recall technique of Oxy-16 and Oxy-18) and temperature can be an indicator of water content. Because of findings from theste crystals, some scientists argue that 4.4 billion years ago, the earth was already cooling down.

The early earth ocean was hot and salty. Most salt today is landlocked in salt domes and evaporate deposits. There were no continents for the salt to get tied up into, and thus the early oceans might have been twice as salty as it is today. The early oceans were also very acidic. The hadean air had lots of co2 and co2 combines with water to form carbonic acid. ..hydrogen ions, hydronium ions plus bicarbonate. This acidic ocean weathered rocks faster. --At that time the sun was faint

5. Gray Earth - The Formation of Granite Crust

The unique melting of silicom rich basalt lead to the formation of Granite. Granite has four basic components. Crystals of quarts (silicon oxide), two kinds of feldspar -rich in potassium and sodium-- mica/ pyroxene/ amphibole...sometimes zircon.

After this, we have to appreciate Buoyancy. Granite floats on Basalt. It accumulates mountains on top of basalt. Plate tectonics; Granite floats and basalt sinks. This is the key to the origin of the continents. Basalt get recycled and reheated. Granite floats and forms continents.

Question: Has granite stopped forming? If it has, what stops it? If not, are we going to become one giant granite ball?


6. Living Earth - The Origins of Life
amino acids made by Harold Urey
Carbon experiements

There are quasi-living sytem of molecules
Citric acide cycle -It starts with acetic acid, reacts with Co2 to form pyruvic acid, then reacts with more co2 to make oxaloacetic acid..eventually the molecules get so big, that they break up into acetic acid again.

Self-replicating auto-catalytic network- they are complicated reactions that speed up the development of themselves but then go on to destroy their neighbors.

RNA molecule that made copies of itself. Some how these RNA polymers adapted to out compete their RNA Neighbors. Perhaps they bonded onto minerals.

Also think about the lipid communities.

Early microbes learned to take normal reactions, that had energy. They they developed some type of enzyme to accelerate the process. Early microbes reduced iron to form red mineral hematite. The geo-sphere and the biosphere co-evolved.

Then photosynthesis comes about. Hopanes survive after a photosynthetic cell dies out.

7. Red Earth - Photosynthesis and the Great Oxidation Event

Microbes have figures out quite a few ways how to harvest light and energy sources. A few photosynthetic pathways produce no light at all. Biochemist Robert Blackenship and arizona state university study these microbes. Microbes shuffle and swap light producing genes. Plants get their photosynthesis from two more primitive pathways - Photo system 1 and Photo system 2.

Earth is always evaporating hydrogen. The heavier o3 just lumbers around with the pull of gravity.
NOX microbes and peroxide microbes.

The questionable field of Microbe fossils. They have been found in Black chert, black shale and stromatolites. Nora Noffke added a forth one Sandstone- she found evidence of microbial mats.

Along with life-forms came the mineralogical explosion. It may be that microbes add to the formation of minerals. An oxygen rich subsurface lead to the formation of minerals. Molybdenite -mineral of molybdenum. Oxygen from microbes transformed Riheium and Molydbdenum.



Life is linked with 45 hundred known chemical species. Some of the new minerals provided habitats for life. Life has continuously co-evolved with rocks and minerals.  


8. The 'boring' Billion - The mineral Revolution
The boring billion may refer to our ignorance of this time period. The cratons have a complex history. The boring billion saw he formation of two super continents. Rodina and Pangea .....there was also an intermediate ocean. The climate was surprisingly stable.


During this time, there was a mineral explosion. Magazine American Mineralogist. 
This time period was very smelly- a sulfide laden ocean. 

9. White Earth - The Snowball-Hothouse Cycle
From a time period of 2.5 billion to 542 million years ago, the climate of the earth altered radically. There are mechanisms that keep the earth's climate in check, and there also mechanisms that send extreme positive or negative feedback loops.

The earth glaciated at least 3 times. Sturtian glaciation peaked 750 million years ago. The Marinoan glaciation follow 650 million years. Gaskiers glaciation occurred at 580 million years ago.

Tillites are one type of evidence for glaciation.


This Chapter begins with the prospect that earth froze over completely. According to an article found in the magazine science 'A Neoproterozoic Snowball Earth' by Paul Hoffman at the University of Maryland, Earth completely froze over. Methane isotopologs- 1 in a million methane molecules holds a carbon 13 and a deuterium. Finding a good ratio of these molecules will indicate at what temperature the methane froze in the ocean. If formed below 200 degrees, them microbial help was involved. If batch froze above 1,000 degrees, then it's abiotic. No instrument can get out this ratio. The Deep Sea Carbon Observatory help to fiance a proto-type instrument.

An interesting fact is that there is frozen methane in the bottom of the ocean.


During the end of these cycles, there is growing evidence that microbial communities started colonizing land. According to the article ' The Inception of the Clay Minerol Factory' by Martin Kennedy of the University of California, Riverside, indicated that the rise of oxygen to the degree we know now was due to feeedback between microbes and clay minerals.  Clay led to the burial of carbon and the rise of oxygen.

Also there is ancient phosphorus strata- in some communities phosphorus was the missing element,

With this rise of oxygen, it led to the rise of animals. Margulis believes in endosymbiosis. She believes that traits are shared among different animals as a survival technique. Donald Williamson proposed that butterflies represent the merging of two very different organisms- the worm-like caterpillar and the winged butterfly. --This sharing of traits furthers evolution.
10. Green Earth. The rise of a Terrestrial Biosphere

You can break up green earth into three acts.

Act 1- The beginning of the Cambrian period, 542 million years ago. Rodinia was broken into many small pieces.

Act 2- 300 million years ago, Gondwana collided with Laurentia to produce Pangaea and the Appalachian mountains.

Act 3- The Opening up of the Atlantic Ocean 175 million years ago, when Pangaea fragmented.

530 million years ago, many types of animals learned to build their shells out of hard minerals- usually using calcium carbonate or silica.

Lifeforms began colonizing the land. 400 million years ago, lifeforms were strange. Prototaxites specimens--fossils--their biological markers--fossilized tube like structures-turned out to be fungal. Meaning that their was fungus the size of a tree.


The invention of leaves, took million of years more. 360 million years ago, forests emerged and the land became emerald green. Plants and fugal filaments co-evolved.

Then the first fist started walking on land 395 million years ago and turned into amphibians.

300 million years ago, earth forests did well and another oxidation event happened. This benefited animals, and some organisms grew larger. Giant insects happened. There were monster dragonflies with 2 foot wingspans. 

Then there are times of mass death. 
251 million years ago was the great dying. 96% of all marine species died and 70 percent of land species. --not sure what caused it--maybe several factors such as decreased oxygen, large scale volcanoes, collapse of ozone layer. 

Then the age of Dinosaurs, the mesozoic era! It saw the development of flowering plants. Then 65 million years ago, a giant asteroid that was 6 miles wide, caused another great dying event. 

The rise of humans started with that asteroid 65 million years ago. Little mammals became big. 2.5 million years ago, homo habilis came around.     



11. The Future - Scenarios of a Changing Planet.
I'm going to keep my notes on this chapter short. The future for earth is certain. It will get swallowed or baked by the sun. A very very very very long time from now, life will not exist on earth. Our short term future, that is in our hands.

General Notes: 
To study petrochemistry, it is important to understand what are the common elements an earth. Oxygen, Silicon, Iron, Calcium (donar 2 e), Magnesium (donor 2 e) and aluminium (donor 3e)..then sodium and potassium.

Oxygen is an electron acceptor, (of two e)
Silicon is a electron donor. (4 e)
Quartz- Sio2
Iron is versatile. (sometimes donor of 2e, produces greenish color, will donote 3e- red rust formed)
Iron is a donar of par excellence) --also metal


Friday, June 17, 2016

Getting Dirty & Butterfly Sex

Mt Washington 8.5 miles, roundtrip Gain: 3250 ft.
 Little Si 4.7 miles, roundtrip Gain: 1300 ft.
Mt Si 8.0 miles, roundtrip Gain: 3150 ft.
 East Peak Rattle Snake Ledge 8.6 miles, roundtrip Gain: 2500 ft.

Yesterday, I had a successful trip. I did not go up Mt Teneriffe..I ended up double summiting  Mt Si and Little Si for a total mileage of 12.7 miles and an elevation gain of 4450ft.

It was a hard day, but I loved every second of it.





I met two people on the trail. I met a woman named Coco and a man named John.

 Having company was a treat, and it made the day go faster.

Coco was my age and had a child. She is an athletic junkie, which means that working out is her life. Coco does a little bit of everything to keep herself in shape. She can run a 10k uphill and likes to cradle her fitbit. She berated me for only hiking every 3 days and not everyday. John was retirement age and spent his life working in the submarine tourism industry- I never knew there was such a industry!- and was recovering from an accident. As far as I could tell, he missed his wife, who was adventuring in the Olympics, and he was having trouble adapting to old age. I do hope I see these people on the trails again!

On Monday, I plan to go back to Mount Teneriffe. Maybe I'll text Coco and tell her my plans...who knows? She might want to hike with me.  .

Tomorrow, I hunt butterflies!
If everything goes right, I'll be hunting butterflies with the Mountaineers near Reecer Creek Canyon. Hopefully, it won't rain too much, driving us and the butterflies away.

If I'm lucky, I'm hoping to see some randy Butterfly sex because in the last butterfly workshop, that is what I learned about.

Tonight, I plan to go to a Cascade Grotto meeting, and when I am there, I hope I hear something about the White Nose Bat Syndrome...I've been hiking all over North Bend... I want as much information as I can get on this.

Also, I wanted to share some pictures of Mat fixing the CV axle in my Car.
Below is animation of a CV joint. A constant velocity joint is designed to transmit energy at a variable angle, without causing too much friction.

(Image Source
= https://upload.wikimedia.org/wikipedia/commons/3/3a/Simple_CV_Joint_animated.gif)

 Mostly, I read while Mat explored the underside of my car. 
Although when he needed a hand, I did get a little dirty. 

Wednesday, June 15, 2016

Butterfly Documentary BBC 2015 - BEST Wildlife Documentary Movies HD [NEW]

Rants

I feel depressed.

I'm listening to the song below, and I think I'm just going to be stuck on my blog today.
Later, I have a very serious butterfly workshop to attend..... It's very serious indeed....

Below is why I love Salsa.



What happened at Pulse is certainly depressing. I get a little distressed when I look at the details of that incident.

Tomorrow, I plan to climb Mt. Teneriffe. Though I feel so depressed and lazy now. ...Ugh.... I'll feel differently tomorrow.

Climbing mountains always cheers me up.

I have a new conditioning program that I'm trying to follow. I've been trying to climb a mountain every 3 days.  So far, I've climbed Mt. Washington (& hiked twin falls the same day), The East Side of Rattlesnake Ledge, and tomorrow, I plan to hike up Mt. Teneriffe. All of these have been conditioner hikes, but I haven't been timing my hikes because just getting my fat ass up the mountain is an accomplishment.

If I get down the mountain and feel like sleeping, it's been a successful trip. When snoozing is the goal, I can't complain about my athletic aspirations. Part of the whole experience is taking selfies and collecting pebbles. (I'm a really annoying hiker... A man saw me take a selfie at twin falls, and whenever I passed him, he averted his eyes..I feel that somehow that I embarrassed us both. )

Dangers that I foresee while hiking on the trail from most challenging to least: getting lost, dehydration, cold, animals, and scary weirdos.

Getting lost- I have to be careful of forks and unmarked trails.  Bring a flashlight in case it gets dark.

Dehydration- I need to bring plenty of water and should view dizziness with suspicion.

Cold- The cold will fucking kill you. Being aware of weather conditions and not wearing cotton. But my hope is just to be out for a day.

Animals- Man, running into a bear or cougar is my worst nightmare. They say you can bring a horn. Sometimes I bring my harmonica to scare of animals with my horrific playing.

Scary Weirdos- On a whole, I don't concern myself with running into weirdos. Why would anyone attack you on a trail? It's not an ideal place to rob people because hikers don't always carry money. Plus, you have to climb a fucking mountain! One woman confided that she was concerned about rapists on the trail. Personally, I refuse to believe that if you are a woman (even an attractive one), that everyone is out to rape you. I believe that rape does happen, but statistically, it does not warrant cowering in fear. If someone attacks you, you take your rusty knife and you gut them. We can't have a society that controls' women through fear. Plus, we can't perpetuate racism or something-ism with the flames of our fear. Society needs support strong women, and part of that, is punishing those who engage in violent crime (with an equal predetermined system)...easier said than done. But here is how I feel ...Strong Women (who are valued) = Better Society.  
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