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Busting out the comic and in to reality
the robots are coming . . .www.monoclothing.com
Nearly as tall as me , . . .Lord Breakfast
Mono Cliffs Provincial Park. It's not a big park but it tells of important geology along the Bruce Trail in Ontario.
I had a very pleasant hike here in cool fall weather. No bugs, no people, just me and my thoughts (and my camera).
Mono Cliffs Provincial Park. It's not a big park but it tells of important geology along the Bruce Trail in Ontario.
I had a very pleasant hike here in cool fall weather. No bugs, no people, just me and my thoughts (and my camera).
The Mono–Inyo Craters are a volcanic chain of craters, domes and lava flows in Mono County, Eastern California. The chain stretches 25 miles (40 km) from the northwest shore of Mono Lake to the south of Mammoth Mountain. The Mono Lake Volcanic Field forms the northernmost part of the chain and consists of two volcanic islands in the lake and one cinder cone volcano on its northwest shore. Most of the Mono Craters, which make up the bulk of the northern part of the Mono–Inyo chain, are phreatic (steam explosion) volcanoes that have since been either plugged or over-topped by rhyolite domes and lava flows. The Inyo Craters form much of the southern part of the chain and consist of phreatic explosion pits, and rhyolitic lava flows and domes. The southernmost part of the chain consists of fumaroles and explosion pits on Mammoth Mountain and a set of cinder cones south of the mountain; the latter are called the Red Cones.
Eruptions along the narrow fissure system under the chain began in the west moat of Long Valley Caldera 400,000 to 60,000 years ago. Mammoth Mountain was formed during this period. Multiple eruptions from 40,000 to 600 years ago created the Mono Craters and eruptions 5,000 to 500 years ago formed the Inyo Craters. Lava flows 5,000 years ago built the Red Cones, and explosion pits on Mammoth Mountain were excavated in the last 1,000 years. Uplift of Paoha Island in Mono Lake about 250 years ago is the most recent activity. These eruptions most likely originated from small magma bodies rather than from a single, large magma chamber like the one that produced the massive Long Valley Caldera eruption 760,000 years ago. During the past 3,000 years, eruptions have occurred every 250 to 700 years. In 1980, a series of earthquakes and uplift within and south of Long Valley Caldera indicated renewed activity in the area.
The region has been used by humans for centuries. Obsidian was collected by Mono Paiutes for making sharp tools and arrow points. Glassy rock continues to be removed in modern times for use as commercial scour and yard decoration. Mono Mills processed timber felled on or near the volcanoes for the nearby boomtown Bodie in the late 19th to early 20th centuries. Water diversions into the Los Angeles Aqueduct system from their natural outlets in Mono Lake started in 1941 after a water tunnel was cut under the Mono Craters. Mono Lake Volcanic Field and a large part of the Mono Craters gained some protection under Mono Basin National Forest Scenic Area in 1984. Resource use along all of the chain is managed by the United States Forest Service as part of Inyo National Forest. Various activities are possible along the chain, including hiking, bird watching, canoeing, skiing, and mountain biking.
Source: Wikipedia
Another from a nice evening at Mono Lake last week....I was drawn to the reflections on this calm night. The brightness (.9 GND) in the sky created enough of light in the reflections to give fill light to the shadow side of the Tufa's and the plant remnants in the foreground. According to the Mono Lake newsletter the lake level has risen 1.2 feet just since April of this year.....
As usual, best on Black
Mono Lake is an alkaline and hypersaline lake in California, United States that is a critical nesting habitat for several bird species and is one of the most productive ecosystems in North America.
Geology
Mono Craters are rhyolitic domes. The dark colored Negit Island is of volcanic origin and is somewhat less than 2000 years old. Paoha Island is the larger and lighter colored island in the lake and was formed 300 years ago from uplift caused by magma movement. Black Point is the remnant of a cinder cone volcano that erupted under water in prehistoric times, when Mono Lake was much larger (and referred to as Lake Russell).
Ecology
In order to provide water for growing Los Angeles, water was diverted from the Owens River and then from the tributaries that fed Mono Lake (see California Water Wars). In 1941 the city of Los Angeles extended an aqueduct system into the Mono Basin, diverting water that would otherwise have entered Mono Lake.
Enough water was diverted that evaporation soon exceeded inflow and the lake level fell rapidly, exposing alkaline sands and once-submerged tufa towers, and turning Negit Island into a peninsula, exposing the nests of gulls to coyotes and forcing them to abandon the island.
In 1976 University of California, Davis graduate student David Gaines earned his master's degree studying the Mono Lake ecosystem and was instrumental in alerting the public of the effects of the lower water level. Gaines formed the Mono Lake Committee in 1978 and joined up with the Audubon Society to fight a now famous court battle to protect Mono Lake through state public trust laws. Despite these efforts, the lake is still lower than historic levels and exposed shorelines are a source of significant alkali dust during periods of high winds.
Owens Lake, which sustained a similar ecosystem, completely dried up because of water diversions. Mono Lake was spared the same fate on September 28, 1994, when the California State Water Resources Control Board issued an order to protect Mono Lake and its tributary streams. Since that time the lake level has steadily risen; in 1941 the lake level was at 6417 feet above sea level and as of 2004 it was at 6381 feet (1945 m). The goal is to have lake level rise to 6392 feet above sea level, a goal made more difficult by drought in the American West.
The lake contains approximately 280 million tons of dissolved salts, with the salinity varying on the amount of water in the lake at any given time. Before 1941, the salinity was approximately 50 grams per liter (g/l) (compared to a value of 31.5 g/l for the world's oceans). In 1982, when the lake reached its lowest level, the salinity had nearly doubled to 99 g/l. In 2002 it was measured at 78 g/l and is expected to stablize at an average 69 g/l as the lake replenishes over the next 20 years.
The hypersalinity and high alkalinity (pH=10 or equivalent to 2.5 grams of NaOH per liter of water[2]) of the lake, means that no fish are native to the lake. An attempt by the California Department of Fish and Game to stock the lake failed. The lake is famous for the Mono Lake brine shrimp, Artemia monica, a tiny species of brine shrimp, no bigger than a thumbnail, that are found nowhere else on earth. During the warmer summer months, an estimated 4-6 trillion brine shrimp inhabit the lake. The species has no food value for humans, but is a staple for birds of the region. Also an important food source, alkali flies ("Ephydra hians") live along the shores of the lake and walk underwater encased in small air bubbles to graze and to lay eggs. The whole food chain of the lake is based on the high population of single-celled algae present in the warm shallow waters.
Mono Lake is a vital resting and eating stop for migratory shorebirds and has been recognized as an International Reserve in the Western Hemisphere Reserve Network. Nearly 2,000,000 waterbirds, including 35 species of shorebirds, use Mono Lake to rest and eat for at least part of the year. Some shorebirds that depend on the resources of Mono Lake include American avocets, Killdeers, and sandpipers. Over 1.5 million eared grebes and phalaropes use Mono Lake during their long migrations.
Late every summer tens of thousands of Wilson's phalaropes and red-necked phalaropes arrive from their nesting grounds, and feed until they continue their migration to South America or the tropical oceans respectively.
In addition to migratory birds, a few species spend several months to nest at Mono Lake. Over 85% of the state population of California gulls nest at Mono Lake each year. After abandoning the landbridged Negit Island in the late 70s, California gulls have moved to some nearby islets and have established new, if less protected nesting sites. Cornell University and Point Reyes Bird Observatory have continued the study of nesting populations on Mono Lake that was begun over 20 years ago. Snowy Plovers also arrive at Mono Lake each spring to nest along the remote eastern shores.
In Mark Twain's Roughing It (1872), chapter 38 and chapter 39 provide a humorous but informative early description of Mono Lake in its natural condition in the 1860's.
From Wikipedia, the free encyclopedia
Mono Lake (/ˈmoʊnoʊ/ MOH-noh) is a large, shallow saline soda lake in Mono County, California, formed at least 760,000 years ago as a terminal lake in an endorheic basin. The lack of an outlet causes high levels of salts to accumulate in the lake. These salts also make the lake water alkaline.
This desert lake has an unusually productive ecosystem based on brine shrimp that thrive in its waters, and provides critical habitat for two million annual migratory birds that feed on the shrimp and alkali flies. Historically, the native Kutzadika'a people derived nutrition from the Ephydra hians pupae, which live in the shallow waters around the edge of the lake.
When the city of Los Angeles diverted water from the freshwater streams flowing into the lake, it lowered the lake level, which imperiled the migratory birds.
Mono Lake (/ˈmoʊnoʊ/ MOH-noh) is a large, shallow saline soda lake in Mono County, California, formed at least 760,000 years ago as a terminal lake in an endorheic basin. The lack of an outlet causes high levels of salts to accumulate in the lake. These salts also make the lake water alkaline.
This desert lake has an unusually productive ecosystem based on brine shrimp that thrive in its waters, and provides critical habitat for two million annual migratory birds that feed on the shrimp and alkali flies. Historically, the native Kutzadika'a people derived nutrition from the Ephydra hians pupae, which live in the shallow waters around the edge of the lake.
When the city of Los Angeles diverted water from the freshwater streams flowing into the lake, it lowered the lake level, which imperiled the migratory birds.
Dibujo con bolígrafo Bic negro, lápiz color naranja y acuarela blanca sobre papel amarillo
70 x 50 cm
Mono books, Money and Happiness, will be available at my degree show next month as a limited edition set. Be sure to drop me an email if your interested in getting your hands on a set, cause once they're gone they're gone!
Mono Cliffs Provincial Park. It's not a big park but it tells of important geology along the Bruce Trail in Ontario.
I had a very pleasant hike here in cool fall weather. No bugs, no people, just me and my thoughts (and my camera).
Mono Lake is an alkaline and hypersaline lake in California, United States that is a critical nesting habitat for several bird species and is one of the most productive ecosystems in North America.
Geology
Mono Craters are rhyolitic domes. The dark colored Negit Island is of volcanic origin and is somewhat less than 2000 years old. Paoha Island is the larger and lighter colored island in the lake and was formed 300 years ago from uplift caused by magma movement. Black Point is the remnant of a cinder cone volcano that erupted under water in prehistoric times, when Mono Lake was much larger (and referred to as Lake Russell).
Ecology
In order to provide water for growing Los Angeles, water was diverted from the Owens River and then from the tributaries that fed Mono Lake (see California Water Wars). In 1941 the city of Los Angeles extended an aqueduct system into the Mono Basin, diverting water that would otherwise have entered Mono Lake.
Enough water was diverted that evaporation soon exceeded inflow and the lake level fell rapidly, exposing alkaline sands and once-submerged tufa towers, and turning Negit Island into a peninsula, exposing the nests of gulls to coyotes and forcing them to abandon the island.
In 1976 University of California, Davis graduate student David Gaines earned his master's degree studying the Mono Lake ecosystem and was instrumental in alerting the public of the effects of the lower water level. Gaines formed the Mono Lake Committee in 1978 and joined up with the Audubon Society to fight a now famous court battle to protect Mono Lake through state public trust laws. Despite these efforts, the lake is still lower than historic levels and exposed shorelines are a source of significant alkali dust during periods of high winds.
Owens Lake, which sustained a similar ecosystem, completely dried up because of water diversions. Mono Lake was spared the same fate on September 28, 1994, when the California State Water Resources Control Board issued an order to protect Mono Lake and its tributary streams. Since that time the lake level has steadily risen; in 1941 the lake level was at 6417 feet above sea level and as of 2004 it was at 6381 feet (1945 m). The goal is to have lake level rise to 6392 feet above sea level, a goal made more difficult by drought in the American West.
The lake contains approximately 280 million tons of dissolved salts, with the salinity varying on the amount of water in the lake at any given time. Before 1941, the salinity was approximately 50 grams per liter (g/l) (compared to a value of 31.5 g/l for the world's oceans). In 1982, when the lake reached its lowest level, the salinity had nearly doubled to 99 g/l. In 2002 it was measured at 78 g/l and is expected to stablize at an average 69 g/l as the lake replenishes over the next 20 years.
The hypersalinity and high alkalinity (pH=10 or equivalent to 2.5 grams of NaOH per liter of water[2]) of the lake, means that no fish are native to the lake. An attempt by the California Department of Fish and Game to stock the lake failed. The lake is famous for the Mono Lake brine shrimp, Artemia monica, a tiny species of brine shrimp, no bigger than a thumbnail, that are found nowhere else on earth. During the warmer summer months, an estimated 4-6 trillion brine shrimp inhabit the lake. The species has no food value for humans, but is a staple for birds of the region. Also an important food source, alkali flies ("Ephydra hians") live along the shores of the lake and walk underwater encased in small air bubbles to graze and to lay eggs. The whole food chain of the lake is based on the high population of single-celled algae present in the warm shallow waters.
Mono Lake is a vital resting and eating stop for migratory shorebirds and has been recognized as an International Reserve in the Western Hemisphere Reserve Network. Nearly 2,000,000 waterbirds, including 35 species of shorebirds, use Mono Lake to rest and eat for at least part of the year. Some shorebirds that depend on the resources of Mono Lake include American avocets, Killdeers, and sandpipers. Over 1.5 million eared grebes and phalaropes use Mono Lake during their long migrations.
Late every summer tens of thousands of Wilson's phalaropes and red-necked phalaropes arrive from their nesting grounds, and feed until they continue their migration to South America or the tropical oceans respectively.
In addition to migratory birds, a few species spend several months to nest at Mono Lake. Over 85% of the state population of California gulls nest at Mono Lake each year. After abandoning the landbridged Negit Island in the late 70s, California gulls have moved to some nearby islets and have established new, if less protected nesting sites. Cornell University and Point Reyes Bird Observatory have continued the study of nesting populations on Mono Lake that was begun over 20 years ago. Snowy Plovers also arrive at Mono Lake each spring to nest along the remote eastern shores.
In Mark Twain's Roughing It (1872), chapter 38 and chapter 39 provide a humorous but informative early description of Mono Lake in its natural condition in the 1860's.
From Wikipedia, the free encyclopedia
20 years old and still looks good, still patrols the garden and scares off other cats, I wonder if it is because he is a cross breed Abyssinian and tabby
The amazing natural wonder that is Mono Lake 4.18.13
Nikon D700
Nikkor 24-120mm @ 44mm
ISO 200
1/50s @ f/16
Circular Polarizer
Mono Lake is a large, shallow saline soda lake in Mono County, California, formed at least 760,000 years ago as a terminal lake in a basin that has no outlet to the ocean. The lack of an outlet causes high levels of salts to accumulate in the lake. These salts also make the lake water alkaline.
This desert lake has an unusually productive ecosystem based on brine shrimp that thrive in its waters, and provides critical nesting habitat for two million annual migratory birds that feed on the shrimp.
The human history of Mono Lake is associated with its productive ecosystem. The native Kutzadika'a people derived nutrition from the larvae of the alkali flies that live in the lake. When the city of Los Angeles diverted water from flowing into the lake, it lowered the lake level, which imperiled the migratory birds. The Mono Lake Committee formed in response, winning a legal battle that forced Los Angeles to partially restore the lake level.
en.wikipedia.org/wiki/Mono_lake
en.wikipedia.org/wiki/Wikipedia:Text_of_Creative_Commons_...
The Mono–Inyo Craters are a volcanic chain of craters, domes and lava flows in Mono County, Eastern California. The chain stretches 25 miles (40 km) from the northwest shore of Mono Lake to the south of Mammoth Mountain. The Mono Lake Volcanic Field forms the northernmost part of the chain and consists of two volcanic islands in the lake and one cinder cone volcano on its northwest shore. Most of the Mono Craters, which make up the bulk of the northern part of the Mono–Inyo chain, are phreatic (steam explosion) volcanoes that have since been either plugged or over-topped by rhyolite domes and lava flows. The Inyo Craters form much of the southern part of the chain and consist of phreatic explosion pits, and rhyolitic lava flows and domes. The southernmost part of the chain consists of fumaroles and explosion pits on Mammoth Mountain and a set of cinder cones south of the mountain; the latter are called the Red Cones.
Eruptions along the narrow fissure system under the chain began in the west moat of Long Valley Caldera 400,000 to 60,000 years ago. Mammoth Mountain was formed during this period. Multiple eruptions from 40,000 to 600 years ago created the Mono Craters and eruptions 5,000 to 500 years ago formed the Inyo Craters. Lava flows 5,000 years ago built the Red Cones, and explosion pits on Mammoth Mountain were excavated in the last 1,000 years. Uplift of Paoha Island in Mono Lake about 250 years ago is the most recent activity. These eruptions most likely originated from small magma bodies rather than from a single, large magma chamber like the one that produced the massive Long Valley Caldera eruption 760,000 years ago. During the past 3,000 years, eruptions have occurred every 250 to 700 years. In 1980, a series of earthquakes and uplift within and south of Long Valley Caldera indicated renewed activity in the area.
The region has been used by humans for centuries. Obsidian was collected by Mono Paiutes for making sharp tools and arrow points. Glassy rock continues to be removed in modern times for use as commercial scour and yard decoration. Mono Mills processed timber felled on or near the volcanoes for the nearby boomtown Bodie in the late 19th to early 20th centuries. Water diversions into the Los Angeles Aqueduct system from their natural outlets in Mono Lake started in 1941 after a water tunnel was cut under the Mono Craters. Mono Lake Volcanic Field and a large part of the Mono Craters gained some protection under Mono Basin National Forest Scenic Area in 1984. Resource use along all of the chain is managed by the United States Forest Service as part of Inyo National Forest. Various activities are possible along the chain, including hiking, bird watching, canoeing, skiing, and mountain biking.
Source: Wikipedia
is a large, shallow saline lake in Mono County, California, formed at least 760,000 years ago as a terminal lake in a basin that has no outlet to the ocean. Because it lacks an outlet, dissolved salts make the lake very alkaline and saline.
This desert lake has an unusually productive ecosystem based on brine shrimp that thrive in its waters, and provides critical nesting habitat for two million annual migratory birds that feed on the shrimp. Mono Lake is also notable for containing a rod-shaped extremophilic species of bacteria that may be capable of metabolizing the usually poisonous element arsenic.
The human history of Mono Lake is associated with its productive ecosystem. The native Kutzadika'a people derived nutrition from the larvae of the alkaline flies that live in the lake. When the city of Los Angeles diverted water from flowing into the lake, it lowered the lake level, which imperiled the migratory birds. The Mono Lake Committee formed in response, winning a legal battle that forced Los Angeles to partially restore the lake level.
I love the sense I get of struggle from this little shrub's remains (rabbitbrush?). Funny, another flickr photog, a contact of mine, just uploaded the exact same shrub with almost the same composition (prompting me to go find the one I processed but never uploaded). I wonder how many photographers have noticed and photographed it's skeleton when there's so much big landscape out there to see? I know one did--Justbelightful! ;-)
Mono Lake is a place of extremes. It's a natural inland high desert lake with no outlet. Water flows in, but it doesn't flow out. As a result, the water has a saline content 2-3 times higher than an ocean (depending on water level). The story of Mono's water chemistry isn't that simple, though. Sodium salts of chlorides, carbonates and sulfates (Mono Lake has a lot of salt and baking soda in it), boron, potassium, and even volcanic ash added to the chemical recipe from repeated volcanic eruptions. This ecology is deadly to plants and most animals, yet supports an extremely unique assemblage of species well adapted to living within and around it's waters.