Tuesday, April 26, 2011
artist statement
The best thing about dreams is that fleeting moment, when you are between unconcious sleep and concious awakeing, when you can't comprehend the difference between reality and fantasy, when for just that one moment you feel with your entire soul, that the dream is reality. Often in a dream state our perception of reality is shifted, caused by external stimuli represented upon our concious desires.
Dreams represents a language, a highly developed communication. This extra ordinary way of thinking, where the mind works overtime, ticking away, creating scenarios and illusions, which may or may not be there, to others, or at all.
Not only our memories, but the things we have forgotten are ‘housed’. Our soul is an adobe. And by remembering “houses” and “rooms” we learn to ‘abide’ within ourselves. Now everything becomes clear, the house images move in both directions: they are in us as much as we are in them.
My work is a silent expression of space, dreams, experiences; a hyper reality which I encounter. Dreams and experiences that throw me into turmoil –amplifying my thoughts and altering my perspective of what I see, what I feel and think.
The world is the space in my mind. The clouds are my thoughts. The depth and motions of clouds. The depth and motion of my thoughts.
Perhaps
Monday, March 7, 2011
Sunday, March 6, 2011
Clouds
From Wikipedia, the free encyclopedia
A cloud is a visible mass of water droplets or frozen ice crystals suspended in the Earth's atmosphere above the surface of the Earth or other planetary body. Clouds in the Earth's atmosphere are studied in the nephology or cloud physics branch of meteorology. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Generally, precipitation will fall to the surface; an exception is virga which evaporates before reaching the surface. Clouds can show convective development like cumulus, be in the form of layered sheets such as stratus, or appear in thin fibrous wisps as with cirrus. Prefixes are used in connection with clouds: strato for low cumulus-category clouds that show some stratiform characteristics, nimbo for low to middle stratiform clouds that can produce moderate to heavy precipitation, alto for middle clouds, and cirro for high clouds. Whether or not a cloud is low, middle, or high level depends on how far above the ground its base forms. Some cloud types can form in the low or middle ranges depending on the moisture content of the air. Clouds have Latin names due to the popular adaptation of Luke Howard's cloud categorization system, which began to spread in popularity during December 1802. Synoptic surface weather observations use code numbers for the types of tropospheric cloud visible at each scheduled observation time based on the height and physical appearance of the clouds. While a majority of clouds form in the Earth's troposphere, there are occasions where clouds in the stratosphere and mesosphere are observed. Clouds have been observed on other planets and moons within the Solar System, but due to their different temperature characteristics, they are composed of other substances such as methane, ammonia, or sulfuric acid.
A cloud is a visible mass of water droplets or frozen ice crystals suspended in the Earth's atmosphere above the surface of the Earth or other planetary body. Clouds in the Earth's atmosphere are studied in the nephology or cloud physics branch of meteorology. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Generally, precipitation will fall to the surface; an exception is virga which evaporates before reaching the surface. Clouds can show convective development like cumulus, be in the form of layered sheets such as stratus, or appear in thin fibrous wisps as with cirrus. Prefixes are used in connection with clouds: strato for low cumulus-category clouds that show some stratiform characteristics, nimbo for low to middle stratiform clouds that can produce moderate to heavy precipitation, alto for middle clouds, and cirro for high clouds. Whether or not a cloud is low, middle, or high level depends on how far above the ground its base forms. Some cloud types can form in the low or middle ranges depending on the moisture content of the air. Clouds have Latin names due to the popular adaptation of Luke Howard's cloud categorization system, which began to spread in popularity during December 1802. Synoptic surface weather observations use code numbers for the types of tropospheric cloud visible at each scheduled observation time based on the height and physical appearance of the clouds. While a majority of clouds form in the Earth's troposphere, there are occasions where clouds in the stratosphere and mesosphere are observed. Clouds have been observed on other planets and moons within the Solar System, but due to their different temperature characteristics, they are composed of other substances such as methane, ammonia, or sulfuric acid.
Tuesday, February 15, 2011
Saturday, February 5, 2011
the scientist
I was just guessin' at numbers and figures,
Pulling the puzzles apart.
Questions of science, science and progress
Do not speak as loud as my heart.
Pulling the puzzles apart.
Questions of science, science and progress
Do not speak as loud as my heart.
Monday, January 17, 2011
Thursday, November 25, 2010
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