Showing posts with label mountains. Show all posts
Showing posts with label mountains. Show all posts

Tuesday, August 26, 2025

Accurate naming

At the far end of Buttle Lake, I stopped to take a couple of photos. And then, at home, looked up the mountains on the map. As I do, usually.

Had to laugh at this one.

From Thelwood Creek Bridge, looking south.

And looking north, towards the lake.

So: most of Vancouver Island is a mass of mountains. The Golden Hinde, our tallest mountain, at 2195 metres, lies 18 kilometres from my viewpoint.

Here's a Google Maps terrain view; you get the idea:

The red star marks the snow-sprinkled mountain in the first photo above. The Golden Hinde is a little to the left at the level of the end of the lake.

And here's the map covering only what I could see from the bridge:

Big Interior Mountain, 1857 m. 11 km, bridge to BIM. View rotated; South to the left.

Big Interior Mountain? A name to distinguish it from the other hundreds of big interior mountains. Good job!

A Skywatch post.

~~~~~~~~~~~~~~~

En el extremo más al sur del Lago Buttle, me detuve para sacar fotos del paisaje. Y luego, en casa, busqué las montañas en el mapa, como acostumbro.

Una montaña me hizo reir.

  1. Vista desde el puente sobre el riachuelo Thelwood, mirando hacia el sur.
  2. Y mirando hacia el lago, al norte.
  3. La mayor parte de la isla de Vancouver se constituye de montañas. El Golden Hinde, nuestra montaña más alta, midiendo 2195 metros de altura, dista 18 kilómetros desde el puente de donde saqué estas fotos. Aquí está un mapa en relieve que lo demuestra. La estrella roja marca la montaña incluida en la primera foto; la que tiene algo de nieve en la cumbre. El Golden Hinde es un poco hacia el oeste desde el puente.
  4. Y un tramo del mapa, incluyendo solamente lo que se podría ver desde el puente. Con esa montaña con nieve, llamada "Montaña Grande Interior", que queda a 11 km. del puente. (El sur aquí es hacia la izquierda.)
¿Montaña Grande Interior? Un buen nombre que la distingue de las múltiples montañas grandes interiores, ¿no? ¡Bien hecho!

Un post para Skywatch.


Sunday, February 16, 2025

Disguised as mountains

 I am going to do something different today. Philosophizing, you might call it. Rambling about, spiralling in on something I've learned.

As a small child, I overheard my doctor talking to Mom. The walls were thin; this was not for my ears. He said, good old white-haired Doctor Gilchrist, dead and gone now these 60 years and more, he told Mom not to expect me to reach adulthood. He was mistaken, no blame to him; this was before the age of antibiotics. I'm now 82 years old, and I think I'm an adult.

I took this to heart. Not with despair, but with determination. I was going to remember. Everything. Because I was a child and still took literally all I had been told, and "knew" I would soon be facing heaven. And I didn't like what they said heaven was; gates and paved streets and gold, all shiny and hard. I was a child of the rainforest. The substrates I knew were water and wood, mossy rock and forest duff. No straight lines anywhere, nothing polished,  no stony walls. No gold. So I was going to store up memories of the world around me to hark back to for comfort once I was stuck in heaven. (I was a child, remember.)

I had plenty of time to stock up memories. I spent many hours looking out my window, or my hospital windows, watching, watching. The way water moved, the swaying of evergreen branches, the shapes of the mountains, the courses of raindrops on glass; I can still see them, could still paint the picture of the view out of my bedroom window.

When I was able, and released into the wild, I kept up the program of remembering. The scent of pine branches, the taste of fresh huckleberries, the business of crabs on the stony beach, the smell of wood smoke and the touch of salt spray on my face. I swam down under the dock to look at the sea urchins clustered there. I climbed the hill and lay on the moss in the afternoon sunlight. All filed away.

So nothing has changed. I still go out and look and remember. And after years in other climes, I'm back close to home, where I spent my first years. I'm once again in the rainforest. Looking at lichen and mushrooms, logs on the shore, gulls and crows, hermit crabs and bees and diving ducks ... And mountains.

And here's where what I'm seeing has changed for me. The mountains. The rocks. Glacial erratics on the shore; tall, forbidding rock faces where they've cut roads through the hills; slabs of sandstone forming the bed of a summer-slow creek. Rocks.

I am not a scientist. Science-oriented, yes, but not extensively science-trained. And geology has never been my strong suit; I know the basics, that's about it. But I've loved the mountains, even more so after some years in Bella Coola, in that deep valley hemmed in by white peaks. Nusatsum, the Saloompt, Noosgulch, Thunder Mountain; I can see their shapes in my dreams yet. And then, here in Campbell River, as I drive down the shore highway at low tide, I pass glacier-wrought beach decor; long scratches in flat slabs of sandstone and discarded rocks scattered about, glacial erratics, their lower surfaces colonized by barnacles. This island has been a busy place ever since it sprung out of the sea, so many millennia ago.

But there has always been a divide, to my mind: nature, with its horde of living things, and star stuff, the rocks Ma Nature lives on. And this was another mistake.

I don't know where, exactly, I started to realize it. Maybe reading about the fossils of crinoids found near Buttle Lake. Maybe earlier, splitting a stone from the clay hillside below my cabin in the Fraser Valley and finding inside it a fossilized leaf. But still, those were examples of life trapped in stone. I was reading about limestone when it finally clicked; the stone is as much part of living Nature as the snowdrops that sprung up beside my door last week and the cat that sits on my windowsill, tail twitching as she watches the sparrows in the plum tree, so tantalizingly out of reach.

See, limestone is made up of the shells of tiny marine animals. My rock book lists, "Reef forming animals, such as corals and algae, and shelled animals such as bivalves, gastropods, brachiopods, ammionites and echinoids  are all common and sometimes form the entire rock." Like the moon snail shell I found on the beach, like the weathered clam and mussel shells that make up much of the sand. Just older. Very much older; the crinoids at Buttle Lake were there, waving about underwater, collecting their food just as barnacles do today, but this was 290 to 260 million years ago.

That's the limestone. What about the igneous rocks, the basalt and granite? No telling what they were before they got crushed and melted down there in the deep earth, but there is one hint; by weight, their most common element is oxygen. The element that turned this globe from a barren waste to a growing, living, breathing thing.

The Bella Coola river runs green, a pale blue-green that tints the ocean water for 15 kilometres beyond the estuary. Glacier runoff, rock flour; the mountain rocks ground to a fine powder and borne out to sea to slowly sink to the bottom, there to provide trace minerals to swimming and creeping critters, or even to be converted to those super-hard snail teeth (made of goethite crystals). Given a few hundred millennia, if the sun still shines, these same snail's teeth will be rock again, ready to be stewed, squeezed, re-ground, delivered for re-use by a new generation of critters. Ma Nature recycles.

And life goes on. Even when it's disguised as mountains. The rocks from which life arose, back there in the cooling star stuff.

It's all of a piece. This world is a living entity. Maybe the stars are dead. Lifeless, anyhow. But now I wouldn't be so sure.

One more thing to remember.

Today's photos are ones I took years ago, in 2010: the mountains of the Bella Coola valley.

View from near the top of the Hill, the road dropping down into the valley, a 1500 metre drop.

Nusatsum, as seen from my window.

~~~~~~~~~~
Hoy voy a hacer algo diferente. Un poco de historia personal, dando vueltas hasta llegar a algo que he aprendido.

De niña, escuché cuando mi doctor hablaba con Mamá en la cocina. Las paredes no llevaban aislamiento; no sabían que yo les oía. Dijo, el buen Doctor Gilchrist, ya pasado hace 60 años y más, le advertía a mi pobre madre, que no debería esperar a que yo llegara a adulta. Se equivocaba. No lo podía saber; esto era antes de la edad de los antibióticos. Ahora ando en los 80 años, y creo ser adulta.

Esta noticia la tomé muy en cuenta. No para desesperar; sino con el intento firme de prepararme. Iba a cometer todo a memoria. Todo. Porque era niña y todavía tomaba lo que me decían como verdad absoluta. Y "sabía" que pronto estaría en el cielo. Y no me gustaba la descripción de ese lugar; portones y calles pavimentadas, y oro; todo brilloso, todo duro, sólido. Yo era hija de los bosques pluviales. Los sustratos que conocía eran agua y madera, piedras acojinadas con musgos, tierras sueltas de bosque compuestas de hojas y piñas de abeto. En mi mundo no existían las lineas rectas, nada estaba pulido, no había paredes de piedra. No había oro. Y decidí archivar memorias del mundo que me rodeaba, para poder hallar consuelo recordándolas una vez encerrada en el cielo. (Era una niña, recuerden.)

Tuve bastante tiempo en que guardar memorias. Pasé muchas horas mirando por mi ventana, por las ventanas del hospital, observando, observando. Como se movía el agua, como se mecían las ramas de los pinos y cedros, las formas de las montañas, los caminitos que hacían las gotas de lluvia en el vidrio; lo puedo ver todavía en memoria, podría hoy pintar la vista desde esa ventana de antaño.

Cuando me había recuperado suficientemente, cuando me dejaron salir al mundo salvaje, seguí con el programa. Memorizaba el aroma de ramas de abeto, el sabor de los arándanos rojos en la primavera, las actividades de los cangrejos entre las piedritas de la playa, el olor de humo de madera fresca, y la frescura de rocío del agua salada en mi cara. Bajé nadando bajo el muelle para mirar los erizos de mar que se amontonaban allí. Subí el cerro y me acosté sobre el musgo bajo el sol de la tarde. Todo lo cometí a memoria.

Pues nada ha cambiado. Todavía salgo y miro y guardo las memorias. Y después de años en tierras lejanas, estoy de regreso cerca de donde pasé esos primeros años. Estoy entre los bosques pluviales, observando los líquenes, los hongos, los troncos en la orilla del mar, las gaviotas y los cuervos, cangrejos ermitaños y patos buceadores ... Y las montañas.

Y aquí es donde como pienso de lo que veo ha cambiado, Las montañas. Las rocas. Los bloques erráticos en la playa; rocas gigantes, amenazantes, donde han cortado caminos en las laderas; planchas de piedra arenosa que forman la base de un rio que corre lentamente en el verano. Piedras.

No soy científica. Estudio y leo las ciencias, sí, pero no tuve gran educación formal en las ciencias. Y la geología nunca me ha sido muy accesible, conozco lo básico, y no mucho más. Pero siempre he amado las montañas, aun más después de algunos años en Bella Coola, en ese valle profundo, encerrado entre picos nevados. Nusatsum, Saloompt, Noosgulch, el monte de los Truenos; veo sus formas en mi sueños todavía. Y luego, aquí en Campbell River, pasando por la carretera costal, veo como los glaciares han deorado las playas; grietas largas en las planchas de piedra arenosa, piedras abandonadas regadas por doquier, los grandes bloques errráticos, con sus superficies inferiores colonizados por los bálanos. Esta isla ha sido un sitio activo desde que saltó del mar, hace tantas milenios.

Pero siempre ha habido una división a mi manera de pensar: de un lado, la naturaleza, con sus millares de seres vivientes, y al otro lado materia de estrellas, las piedras sobre las cuales la Madre Naturaleza forma su hogar. Y esto fue un error.

No sé exactamente donde empecé a darme cuenta. Tal vez fue al leer acerca de los fósiles de los crinoides que se encuentran en las piedras cerca del lago Buttle. Tal vez fue antes, al partir una piedra que sacamos, mi nieto y yo, de entre la arcilla del monte bajo mi cabañita en el valle del Fraser, y encontrar el fósil de una hoja entera. Pero no; esos eran ejemplos de la vida atrapada por las rocas. Leía acerca de la caliza cuando de repente, lo vi; la piedra es tanto parte de la naturaleza viva como lo son las flores de la nieve que brotaron al lado de mi puerta la semana pasada y de la gatita que se sienta en mi ventana, meneando la cola mientras mira los gorriones en el ciruelo, tan tentadores, tan fuera de su alcance.

Vean; la caliza se compone de las conchas de animales marinos miniaturos. Mi libro guía de rocas tiene la lista: —Animales que forman arrecifes, como los corales y las algas, y animales con concha como los bivalvos, los gastropodos, brachiopodos, las amonitas y los equinoides todos son comunes y a veces forman la roca entera. — Como la concha del caracol luna que hallé en la playa a marea baja, como las conchas rotas de almeja y mejillón que forman gran parte de la arena. Pero más viejas. Mucho más viejas; los crinoides del lago Buttle estaban allí, meciéndose bajo el agua, buscando su comida como lo hacen hoy en dia los bálanos, pero esto hace de 290 a 260 millones de años.

Eso es la caliza. ¿Y qué de las rocas ígnea, el basalto, el granito? No sé lo que eran antes de que fueron apresionadas y fundidas allá en el centro de la tierra, pero hay un indicio; tomando por peso, el elemento más común en estas rocas es el oxígeno. El elemento que fue el que transformó este globo terrestre de un desierto estéril en una cosa viva, creciendo, respirando.

El agua del rio Bella Coola es verde, un verde/azul pálido que tiñe el agua del mar por 15 kilómetros más allá del estuario. Es agua de glaciares, "harina de roca" lo llaman, las rocas de las montañas molidas hasta convertirlas en polvo finísimo; el rio las lleva al mar donde caen al fondo, y allí proveen de minerales esenciales a criaturas nadantes o rastreras, o se convierten en esos dientes extremadamente duros de los caracoles marinos (se hacen de cristales de goethita). En algunos cientos de milenios, si el Sol sigue brillando, estos mismos dientes de caracol se habrán convertido de nuevo en roca, lista para ser molida, presionada, cocida, y ofrecida para su nuevo uso por una nueva generación de criaturas. La Madre Naturaleza recicla.

Y la vida persiste. Aun cuando se disfraza de montañas. Las rocas de donde empezó la vida, en la materia de estrellas enfriándose en aquel entonces.

En fin, este mundo es una entidad viviente. Tal vez las estrellas estarán muertas. Sin vida. Pero ahora lo empiezo a dudar.

Una cosa más para guardar en la memoria.

Las fotos son de las montañas en el valle de Bella Coola, que menciona el texto, fotos que saqué en 2010. La primera es la vista desde cerca de la bajada al valle; el camino baja 1.500 metros desde el pasaje por el Chilcotin hasta llegar al rio.

La segunda foto es de la montaña Nusatsum, como la veía desde mi ventana en el valle.

Tuesday, November 23, 2021

The lakes, late fall

Lake views. There's frost on the side of the road now, snow and ice on the higher mountain peaks.

Upper Campbell Lake from the eastern end. Elkhorn, Golden Hinde and other peaks.

The tip of Buttle Lake, looking northeast.

Google maps view from the eastern end of Upper Campbell Lake, looking west. Buttle Lake winds off to the left. Summer view, with bare peaks.

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Un par de lagos en el centro de la isla. Ya hay escarcha al lado de la carretera, y en las montañas más altas, hay nieve nueva y hielo. (Mas que en la vista de Google, que enseña la situación a medio verano.)

Primera foto: el lago superior Campbell, mirando hacia el noroeste, con las montañas cubiertas de nieve fresca.

Segunda: el extremo interior del lago Buttle, mirando hacia el nordeste.

Y la tercera, una vista de las mapas Google; mirando desde el extremo del este del Lago Campbell Superior. El lago Buttle se extiende hacia el lado izquierdo.

Saturday, November 09, 2019

A cleft in the rocks

The road down the west bank of Buttle Lake (there is no road on the east bank) runs along a ledge cut out of almost vertical cliffs, sometimes almost at water's edge, mostly well above the tops of trees on the banks, with more rocks looming overhead.

Rugged rock

The lake lies, glacier-scraped, in a deep valley, fed by the constant trickles of water from the peaks above. 30 kilometres long, 1.5 wide at its widest point, it's more of a slow river than a lake, a drainage canal at the foot of the mountains.

I couldn't get back far enough to take in the full height of the cliff. Not without a boat to take me out into the lake.

Google map. The white areas are mountain peaks.Golden Hinde is the highest mountain on Vancouver Island, at 2197 metres.

Terrain view. From the lake surface, at 211 m above sea level, within 5 kilometres, the land has risen to 2000 metres, on both sides of the lake.

The road winds along the cliff face. When it comes out from behind trees, there's a view over the water. But parking along the roadside is not permitted, probably because of the danger from falling rocks, and the instability (or lack) of the lake-side shoulder, so at these viewpoints, there will be a sign: PULLOUT 500 M. Half a kilometre along, there's the pullout; a safe parking spot where the shoulder widens and looks firm. Usually, it's surrounded by bush; to see that viewpoint, you have to walk back those 500 metres, a kilometre round trip for a photo or two. I did this three times.

At a couple of pullouts, though, there were gaps in the trees. One gave me a view of Mount McBride, 5 km away down the Wolf River valley.

Mount McBride, 2081 m. high.The little yellow trees are cottonwoods on the east shore of the lake.

These signs were helpful. I wish there were more like them.

Looking along another helpful sign, to Marblerock Canyon.


Thursday, February 07, 2019

Turning points

Sunday afternoons, I often point the car north or west and let it go until sunset, not going anywhere in particular, just watching the sky and the hills, the roadside rocks and trees. Then I turn around and come home.

This was where I turned back east, at the first viewpoint over Upper Campbell Lake, with the setting sun making me and the camera squint.

Heading south from Woss; I was looking for snow, since it's winter. This was all the snow I found.

A Skywatch post.

Tuesday, December 27, 2016

Ice

I had gone to the top of the hill to look at distant snowy peaks, when I looked down at my feet instead.

Ice on construction site puddle

Puddle # 2

And the view I had been looking for. Mt. Washington, again.


Friday, December 16, 2016

White

The air has been clear the last few days, the clouds riding high, the early dawn* misleadingly warmed with orange light although the temperature is still below zero. From the highway, as I drove south to join the swan count Tuesday morning, the mountains of the mainland, usually a pale blue blur, stood tall, dazzling in their cloaks of new snow.

10 AM. From the parking lot at Salmon Point. I've been trying to identify these mountains on Google. Maybe the tall, pointed one might be Mt. Denman, 6532 ft (1991 m), going by the shape.

Update: It is Mt. Denman. Thanks, Paul!

Looking the other way, over Woodhus Slough, Mt. Washington.

Snow near roads gets grungy fast; even the logs bordering the parking lot were speckled with grey. But on the trail out to the slough, the ground was as white as the distant mountains.

Last fall's flowers.

Icy snow on a fence post.


Sky, rocks, logs, and our footprints. The trail was just more packed snow. 10:20. The clouds are settling down again, but there's still a hint of orange in the east.

The weather people are promising us two more days of cold weather, going down to 8 below zero (Celsius) this morning, before the rain comes back and the snow melts. Or turns to slush.

*Not really so early these days: sunrise this morning will be at 8:14.

A Skywatch post.

Saturday, August 06, 2016

Viewpoint

Rocks, green-clad hills, clouds, and a mini-lake.

From a high point on the road home (about 200 m. above sea level).

And the road meanders on, across the shoulder of the hill, heading up to Bull Lake.

More or less where we were.

While I've been gallivanting around the island (Campbell River and points west, east, north and south), my critters at home in the tank have been active. I'm working on a video of a hermit and her babies, which should be done by tomorrow.

And then there are all those other points (east, south, north) to look at. I will never catch up!



Sunday, March 20, 2016

Looking up

From above, on a map of the terrain, the mid-section of north Vancouver Island has the texture of crumpled paper or tinfoil, sharp-edged folds going every which way. We humans mostly crawl like insects along threads of road down in the valleys, wondering at the snowy peaks and rock faces so far above us.

Google map. Woss and Gold River marked in red. Campbell River is off the map, to the upper right.

Snow and cloud intermingle.

A light snow cover; it is spring, after all. The lower slope has been logged off; the next generation of trees is just starting out.

In those high valleys, the snow lies deep.

(I think this is Mount Abel, just over a mile high. Or it could be the Jagged Mountains; it's hard to confirm the shape from Google maps, because they travelled this road in the summer, when most of the snow was gone.)

While the sun shone in the valley below, it was warm enough this week to walk without a coat, but as soon as I stepped into the shadow of the trees, I was shivering. Old snow still lies in ditches and dark corners. There are signs on the highway warning of ice and frost; snow tires are still needed until next month.

Coming down the Sayward hill; I was warned not to attempt the climb when it's icy.

Red catkins on an alder tree. From a distance, in sunlight, they look almost pink.



Sunday, November 08, 2015

Almost full circle

In my earliest clear memory, I was standing on the dock in Tahsis, on the northwest coast of Vancouver Island. It was raining, just a drizzle. There was a boat; I think we had just landed. I was 4 years old.

A few days ago, checking maps and distances, I realized that I'm almost back where I started. There's a road through to Tahsis now, and it's less than a 3-hour drive from here. And the road is paved all the way to the west coast, at Gold River; after that it's gravel, and may be snowy going over two summits; they advise carrying chains in the winter.

So yesterday afternoon I headed west. I dawdled, stopping to take photos and look for mushrooms in the bush, so I only made it to the border of Strathcona Provincial Park, with 40 kilometres to go to Gold River, before I had to turn back to get home before night.

Coastal mountains, from the edge of Strathcona P. Park

Upper Campbell Lake. About 300 metres (1000 ft.) above sea level.

Three large lakes line up along valleys across the top of Vancouver Island, looking on the map like three wide rivers. First is Campbell Lake, in the hills just above Campbell River. It flows through a narrow neck into Upper Campbell Lake; the road follows the south side of the lake to the entrance to Buttle Lake; here it crosses and heads up the north side to the head of the valley going down into Gold River. I turned back just after the crossing.

Nameless islet at the west end of Upper Campbell Lake.

Spar tree in a logged-off area, with the new growth at its feet.

I'll post photos of some of the mushrooms I found tomorrow.

Friday, September 25, 2015

Two peaks

In the Klinaklini River basin, taken from the car window:

Rolls of hay, winter fodder for cattle.

Stony mountain peak. I'm told it's called "The Finger".

Humans are rare on the Chilcotin Plateau. Driving the highway at the busiest part of the day, I have counted, repeatedly, an average of 4 minutes between cars. At night, I can drive for hours rarely seeing a light. I find the sense of space exhilarating; it's me and the stars and the empty land. I can breathe.

Coming past the town of Kleena Kleene (named after the river) in daylight, I see green fields, a few haystacks, a scattering of houses. About 20 people live here year round. A minute later, the road curves, and I'm alone again.

Kleena Kleene is one of the driest locations in British Columbia because of the rain shadow effect of Coast Mountains located directly to the west. The temperature is cooler than the other similarly dry locations in the province. (From Wikipedia)

In spite of the dryness, the bottom of the valley is green, because the river snakes along gently, winding and looping around the hayfields. The few houses, up on the slopes, sit on dry, baked dust.

Friday, February 21, 2014

A dusting of new snow

The North Shore mountains, seen from the southern end of the lower mainland, on a warm February afternoon:

Front to back: Boundary Bay, Surrey, Vancouver, North Vancouver, North Shore mountains, sky.

Zooming 'way in, to a couple of ski slopes. My landmarks when I'm sort of lost; that way's north.

More new snow, very welcome.
A Skywatch post


Tuesday, January 07, 2014

It's all a matter of time. And water.

Mountains; all massive, jagged rocks:

Tall, sharp peaks, to our south, in Washington State.

Mount Baker

Which will eventually crumble to this:

Beach rocks, with barnacles and brown rockweed. Boundary Bay.

And then be ground down and smoothed out, by water and critters, to this:

Sand, still being ground down, this time by worms and snails. And water. (Other tracks; human, dog, sandpiper.)

Just give it time.

Monday, July 23, 2012

Greendale afternoon

We were in Greendale for a family wedding at my daughter's wedding chapel. I kept myself busy between events, taking photos of the kids. Laurie wandered about, checking out the garden, watching the sun set. These are a few of his photos.

Crocosomia, shedding petals

A tangle of daisies

Hydrangea and rail fence

Busy napping

Sparrow on a wire

Light fading on the neighbour's farmhouse, pink on the clouds and mountain peaks.

More warm light

Mountains southeast of Chilliwack

Darkening clouds over the chapel bell tower.

And one of mine:

Cousins, collecting tiny flowers to refill the flower girl's basket. (After the ceremony.)

The bride was beautiful, the groom beaming, the parents proud. The weather behaved itself; not too hot, not too damp, not raining; we were able to eat dinner in the chapel gardens. But the mosquitoes -- ahh! the mosquitoes! -- they were plentiful, and bloodthirsty! It's been a bad year for them at that end of the Fraser Valley. And by the time I found the Off, both bottles were empty.


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