Fault, by Betsy

I first encountered the word fault meaning a gap or rift in the earth’s crust–not in school or even at home under the tutelage of my parents–but when I was around the age of 50 years partnered with my current spouse and traveling in a geologist’s paradise, the state of Utah. I always thought I had had at least an average education and I did graduate from college. Yet I knew next to nothing about geology. Now whose fault is that?

I have no memory of geology being offered as a subject in high school and not even in college. Granted I attended a liberal arts college for women, and I guess geology was not considered to be of any interest to a 1950’s female student. It’s not that science courses were not offered. Biology101 was a required subject for freshmen. Plenty of courses were offered in chemistry, physics, and other sciences. But no geology or Earth science.

Part of the fault lies in the fact that it was not until the 1940‘s and 50‘s that geologists began to develop a new way of looking at the planet and how it works. Much that we now know about the history of our Earth has been very recently discovered. One of the few positive outcomes of the Second World War was that new technology used for searching for submarines could be developed and further used to study the ocean floor.

As a result scientists could now better understand the dynamics of the earth’s crust. Although the theory of continental drift had been around for decades, now there was an explanation for the movement of the Earth’s land masses which millions of years ago had been one large land mass called Pangea.

This theory of plate tectonics was in the development stage when I was in school. Makes me feel really old. The theory was still in its infancy and not completely developed and certainly not well established among geologists. No wonder it was not well known or understood among educators in 1950.

It seems that today the study of geology has become quite common. Most of my knowledge of the subject that I have now I have learned from my spouse in the last 20 years. Unlike myself, she studied geology in high school and college–and 10 years after I did. I have also gleaned a lot of knowledge from educational television programs about such topics as How the Earth was born, the early history of our planet, volcanoes, and global climate changes, and mass extinctions brought about by catastrophic geologic events. I find geology a fascinating subject, and I love learning new things. Geology does seem to be an excellent topic for educational TV, as the events which have made our earth what it is today are truly dramatic and lend themselves very well to television drama. No wonder. It is the fault of the earth’s faults that causes dramatic events such as tsunamis, earth quakes, volcanic eruptions–big, dramatic happenings.

Enough about the geologic fault. Another kind of fault with which I am quite familiar is the one that happens in tennis when the serve does not clear the net and drop inside the service box. In my ability and age level of tennis, the fault should be a rare happening. What a double fault amounts to is a gift for your opponents. It is a rare happening except when I am playing mixed doubles. In ladies’ senior doubles tennis, in my opinion, the serve is simply the first shot of the game and a way to put the ball in play. The point is rarely won on the serve.
I used to play some mixed doubles. I gave it up when I stopped playing on weekends and when I decided I did not want to routinely lose the game because of my partner serving double faults every time. Why is it that men serve faults so often and women hardly ever? I think it’s because men try to serve aces and women don’t. It’s very hard to serve an ace and it does not happen very often in my age group and ability level. An ace requires a great deal of spin and pace on the ball and perfect placement.

Neither I nor my team mates or our opponents are usually able to pull off such a serve. Better (and more fun) to place it well and play out the point. If I serve a fault, it’s no one’s fault but my own. And everyone knows it.

© 20 April 2015

About the Author

Betsy has been active in the GLBT community including PFLAG, the Denver Women’s Chorus, OLOC (Old Lesbians Organizing for Change), and the GLBT Community Center. She has been retired from the human services field for 20 years. Since her retirement, her major activities have included tennis, camping, traveling, teaching skiing as a volunteer instructor with the National Sports Center for the Disabled, reading, writing, and learning. Betsy came out as a lesbian after 25 years of marriage. She has a close relationship with her three children and four grandchildren. Betsy says her greatest and most meaningful enjoyment comes from sharing her life with her partner of 30 years, Gillian Edwards.

Living on the Faultline, by Nicholas

          Late that
pleasant afternoon, after I’d finished classes, I walked across campus to do
some work in the library. On the third floor I found the book I needed and was
about to sit down at a table when things began to rumble. It was Oct. 17, 1989
and San Francisco was about to get a shaking like it hadn’t felt in decades.
Floors and walls trembled in the familiar motion of a California earthquake.
Fixtures rattled a little and swayed. Then the real shaking began. Ceiling
lights knocked around and flickered and then went out. Books were flung off
their shelves. Filing cabinets toppled over. People dove under tables and I
quickly placed my brief case over my head to protect against falling debris. I
had been through many earthquakes in San Francisco—felt the building sway,
heard the rattling, been waken up in a rippling bed, felt the floor jumping
around beneath my feet—but this time, for the first time, I was afraid. “God, I
could die here,” I thought.
          Then, it
stopped. Fifteen seconds that felt like 15 years. The lights were out but being
5 o’clock in the afternoon, there was enough light for us to thread our dazed
way down three flights of stairs and out of the building. There was no panic as
hundreds of students climbed over piles of books and papers and dust to leave.
Outside, people milled about the campus. I was in probably the worst building
in the worst spot for an earthquake. The San Francisco State University campus
sits almost exactly atop the San Andreas fault and the soil is mostly sand
which tends to magnify the waves of an earthquake. The building I was in was
built of concrete slabs, the kind that respond to shock waves by simply
collapsing. It’s called “pancaking” in which the floors just slide down onto
each other, crushing anything in between. I was glad to be outside.
          Since all
power in the city was out, no traffic lights worked, cars just stopped on the
street, dazed drivers wondering what to do next. No streetcars could run
either. The city just stopped.
          The first
reaction to a major earthquake is confusion. Buildings and the ground they’re
built on aren’t supposed to move like that. Disorientation is the first shock.
          The campus is
in the southwest corner of the city and with traffic totally snarled and no
public transit operating, I figured I might as well start walking home which
was close to the city center, probably 4-5 miles away. I started walking, heading
toward clouds of billowing black smoke. I hoped it wasn’t our house burning
down.
          The streets
were crowded with walkers and some people had transistor radios to get some
news. Remember, this was way before Internet, Facebook, cell phones. No such
thing as instant communication.
          One lady stood
in front of her house and announced to passersby that “That quake ran right in
front of my house.” Had the tremor run right in front in your house, I thought,
you wouldn’t be standing here now. The actual shift in tectonic plates was
probably miles deep in the earth.
          Somebody said
the Bay Bridge collapsed—a part of it, in fact, had. A freeway in Oakland had
collapsed, killing 60 people. The Marina District, built on landfill by the
bay, took the worst damage and was burning. All highways, bridges and trains
were unusable. If you couldn’t walk to where you needed to be, people were told
to just stay where they were. I kept walking, stepping around the occasional
pile of bricks and stucco that had fallen off buildings.
          Finally, I got
home. Everything was OK. We lived on a hill overlooking Golden Gate Park, the
most solid geology you could find in San Francisco (the hill, not the park
which is sand). Walls cracked and books had wobbled to the edges of shelves,
but nothing toppled or collapsed.
          Jamie got home
soon after I did. He’d been in a highrise office building downtown and had to
walk down ten flights of stairs but managed to drive home taking a circuitous
route through neighborhoods to avoid traffic jams. Some of the office towers
had actually banged against one another at the height of the shaking—or so we
heard.
          Shortly after
we arrived home, two friends showed up. They both worked in SF but lived in
Oakland and couldn’t get home so they hiked to our place and stayed with us.
There was no power in the house, so we built a fire outside in a little hibachi
grill and heated up some leftovers. The city was dark except for the glow to
the northeast where the Marina District kept burning. We felt oddly safe on our
bedrock hillside.
          We did
actually perform one rescue that dangerous night. The woman who lived in the
flat below ours was stranded in East Bay which meant her cat Darwin needed
feeding. He sat mewling at our back door until we invited him in and gave him
some food. Next day Darwin repaid the favor by leaving us a dead bird on our
doorstep.
          In the days
that followed, the city slowly got back to a new normal. Mail delivery was
cancelled for three days and many shops remained closed. The World Series
between SF and Oakland resumed. Buildings and freeways were inspected and some
condemned. BART resumed running trains the next day but the Bay Bridge was to
stay closed for at least a month until the collapsed section could be repaired.
Ferry boats started running across the bay—actually a nicer way to commute. We walked
through the Marina District over the rippled pavement and past the leaning or
burnt out flats. Everywhere you went you calculated how safe it was or wasn’t
until you realized there was no place safe but you went on anyway. Living on
the faultline. 
©
19 April 2015
 
About the Author 

Nicholas grew up in
Cleveland, then grew up in San Francisco, and is now growing up in Denver. He
retired from work with non-profits in 2009 and now bicycles, gardens, cooks,
does yoga, writes stories, and loves to go out for coffee.