Click on the video above to see a time lapse of the construction of this custom built home in Ojai
Ok – what makes us love one style and not another?
- Tradition ?
- Color ?
- Functionality ?
- Form follows function ?
- You grew up with it ?
- You just plain like it ?
This home belongs to my friend Brian – a cabinet maker – business man – father – husband – into radio controlled helicopters – mountain biker – to mention a few hobbies.
Custom home on Ojai’s East End
Traditional “Wallace Neff” Spanish style home
Green Building – Built with Rastra Block
With the roof, stucco and driveway complete, only the finish landscape is missing!
Stucco Brown Coat
Building in the City of Ojai is a fairly straightforward process. The town itself is quite small, only 4.4 miles, beyond those boundaries you are in the unincorporated area of Ventura County – a bit more challenging building process. Call us to help you navigate the building process.
Ojai is located at 34°26′57″N 119°14′48″W
The city is generally at 745 feet (227 m) above sea level.
According to the United States Census Bureau, the city has a total area of 4.4 square miles (11 km2), of which only 0.35% is water, and the rest is land.
Ojai is situated in a small east-west valley, north of Ventura and east of Santa Barbara. It is approximately 15 miles (24 km) inland from the Pacific Ocean coast.
Since Ojai is lined up with an east-west mountain range, it is one of few towns in the world to have a “Pink Moment” occur as the sun is setting. The fading sunlight creates a brilliant shade of pink for several minutes on the Topatopa Bluffs, over 6,000 feet (1,800 m) above sea level at the east end of the Ojai Valley. Nordhoff Ridge, the western extension of the Topatopa Mountains, towers over the north side of the town and valley at more than 5,000 feet (1,500 m). Sulphur Mountain creates the southern ranges bounding the Ojai Valley, a little under 3,000 feet (910 m) in elevation. The Sulphur and Topatopa Mountains are part of the Transverse Ranges system.
The Ventura River flows through the Ventura River Valley, draining the mountains surrounding Ojai to the north and east and emptying into the Pacific Ocean at the city of Ventura. The Ventura River was once known for its steelhead fishing before Matilija Dam and Lake Casitas were constructed, eliminating habitat for this trout species.
The climate of Ojai is Mediterranean, characterized by hot, dry summers, sometimes exceeding 100 °F (38 °C), and mild winters, with lows at night sometimes below freezing. As is typical for much of coastal southern California, most precipitation falls in the form of rain between the months of October and April, with intervening dry summers.
Guest Post from:
PETER T. ERDELYI & ASSOCIATES, INC. • Architectural Engineering & Structural Design since 1974
1975 Sawtelle Blvd Ste 175 • Los Angeles, CA 90025 www.erdelyi.com
Here’s the next serving of our bite-sized engineering stories as they happened at Peter T. Erdelyi & Associates.
SHAKING ALL OVER
In light of the recent earthquakes I thought that sharing a few lesser known facts will help to understand what earthquakes are actually all about.
The earthquakes of California are caused by the movement of huge blocks, or plates, of the earth’s crust – the Pacific and North American plates. The Pacific plate is moving northwest, scraping horizontally past the North American plate at a rate of about 2 inches per year, which is about the rate your fingernails grow. (This maybe explains why my wife has to go to the manicurist so many times a year.:)) You can compare this movement to when you snap your fingers. Before the snap, you push your fingers together and sideways. Because you are pushing them together, friction keeps them from moving to the side. When you push sideways hard enough to overcome this friction, your fingers move suddenly, releasing energy in the form of sound waves that set the air vibrating and travel from your hand to your ear, and you hear the snap. The same process goes on in an earthquake. Slow movements in the earth’s outer layer push the sides of the faults together. The friction across the surface of the fault holds the rocks together so they do not slip immediately when pushed sideways. Eventually enough stress builds up and the rocks slip suddenly, releasing energy in waves that travel through the rock to cause the shaking that we feel during an earthquake. Continue reading “Earthquakes in Southern California”