United States
Wasco County

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16 travelers at this place

  • Day16

    4 passes day

    September 23, 2019 in the United States ⋅ ⛅ 11 °C

    Today was quite exhausting. We took off from Hood River and cycled almost all day uphill (1789m in total) with nasty side and head winds. In the end, we made 4 passes (not that far apart though): Bennett Pass, Barlow Pass, Wapinitia Pass, and Blue Box Pass.
    Then, daily routine started: once it's about 4, we start looking for a campspot. Once found (ideally next to a river, creek or lake), we pitch the tent, wash ourselves, do some stretching for the legs, cook dinner, do the dishes, get ready for bed when it's dark at around 7:30pm and write our footprint for the (of course)!). Today, we found a good spot early, so we are in bed at 7 already ;)
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  • Day8

    Northward Bound

    June 14, 2019 in the United States ⋅ ☀️ 24 °C

    It was time to start heading home as we have a long drive ahead of us. We made a short stop at my favourite bargain-finding store, Ross. Hard to believe but this was the only shopping that we did and we purchased very little. We took a longer route northwest in order to go to Timberline Lodge in Mount Hood National Park. The Lodge is a National Historic Landmark and was part of a Federal Art Project in the 1930’s. Built during the Great Depression, it provided jobs for local artisans. The exterior of the hotel was used in the Steven King movie, The Shining. We were impressed.

    From here we continued north to Hood River that is a port along the Columbia River. It is also called the windsurfing capital of the world due to strong wind gusts and river currents. Along our route was an area known as the Fruit Loop with orchards and fruit stands. Unfortunately we were too late for apple blossoms and too early for fruit. We did a short walk along the waterfront park while waiting for a table at a nearby restaurant. After dinner we headed to The Dalles for the night, just another 35 km. We mistakenly took an exit that took us off the interstate and along a scenic route where the road was so curvy that the speed limit was only 50 kmh. As a result, we didn’t arrive at our hotel until nightfall!
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  • Day2

    The Gorge rock formations

    September 13, 2018 in the United States ⋅ ⛅ 21 °C

    as you travel along the river you pass into a drier climate and the sun comes out!

    you notice the change in vegetation from big conifers (doug firs, big leaf maples and hemlock) wet temperate rain forrest to the drier interior forests we see around Keremeous in BC. these forests are Ponderosa pine, bunchgrass forests (and some oregon white oak too quercus garryana according to wiki). This occurs around Hood River and The Dalles. Then you go into even drier territory with only the grassland and sage scrub......amazing such a transition in really such a short drive only around 100 miles. This is why it is so nice to vacation in Eastern Oregon. The temperature is always higher than Western Oregon and the sun tends to shine........However these days the down fall is there are way more fires and we saw lots and lots of evidence of brush fires that had burnt off the vegetation along the entire hillside on both sides of the river.

    On our route home we camped at Deschutes River State Park, where we have camped quite a few times before. Lovely spot on the river, nice bike trail along an old railway bed behind the campground that goes into the deschutes river canyon......this year it was black from the campground back. Apparently there had been a fire here july 2 2018 and it burned both sides of the canyon back 20 miles...... This river is a popular fishing river, but the fishing guides think the fish are ok as the grassland at the edges of the river did not get burnt. There were lots of fishermen in the campsite when we were there, so I hope the fishing is still good.

    You can see lots and lots of the Columnar Basaltic rocks all along the gorge. These are the columnar rocks created when thick magma cools. They are the same sort of rocks from the Giant Causway in Ireland. see here for a cool video of how basalt columns form: ( https://www.youtube.com/watch?v=cWGoiOFgpKI )

    This fellow Nick has a huge series of videos about geology. Very interesting if you want to delve into the Gorge's geology. You have the base rock of Columnar basalts and many lava floods over the years. (17.5 MYA) -Columbia river basalt group - This is why so many layers -these basalts formed from lava from cracks (fissures) in the continental crust that are now over in Wyoming, (yellowstone). But on top of that you have 2 huge Glacial Lakes. One called Lake Bonneville, that covered Utah and Idaho and today the remnant of this lake is the Great Salt Lake in Utah. It gave way 17000 yrs BP, one time only. And a 2nd glacial lake called Glacial lake Missoula in Montana, that gave way in the Pliestocene (glacial times 12,000 bp) over 100 times.

    Lake Bonneville reached capacity when the Bear river from Wyoming changed direction and started flowing into lake Bonnevile rather than going into the Snake river. eventually the rock damming the lake at Red rock pass eroded and the lake gave way. It happened one time and took about 6 weeks to empty. The amount of water was twice that of Glacial lake Missoula, but the flow rate was less. it was constricted at Red Rock pass. It carried many large Basalt boulders with it, which it had carved from the canyon walls, and you can see these in the rock layers along the corridors where they are exposed in the Bonneville layer. Sediment mixed with large boulders. You also seen them in the Snake river canyon in Idaho, in the farmers fields they call them "Melon Gravel". Huge boulders of basalt that were dropped as the waters energy lessened.... We will see these later in our road trip as we basically follow the path of the Snake river and then the flood through Red Rock pass to get to the Great Salt lake in Utah

    For Glacial Lake Missoula, the ice dam broke, and a huge amount of water came flowing down the ancestral Columbia river.....it came down very quickly with a lot of force and a lot of water so carved out the channels deeper and deeper is my understanding. It also backed up at certain choke points - Wallula gap- and gave rise to other glacial lakes such as Lake Lewis in Eastern Washington. Lake Missoula emptied over 100 times in the pliestocene (glacial times) and took a day to empty.

    Bonnevile broke only once and took 6 weeks to flow out (1700 BP) , Missoula broke many times (1200 BP ) and reformed but gushed out in days.

    another cool u tube video regarding this from nick: (https://www.youtube.com/watch?v=i1BFb_uYlFQ )
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  • Day2

    more of the gorge rocks and burn

    September 13, 2018 in the United States ⋅ ⛅ 19 °C

    nice basaltic columns, and rock layers

    Deshcutes river park where you can see the burn and the yellow border. Below the yellow is the camping area.

    across the columbia river on the Washington side you see the many wind turbines. they are on the oregan side too, but you can't see them when you are down at river level.....eventually we will get to the top alone the plateau and you will see lots of them. It is very windy.Read more

  • Day2

    deschutes state park

    June 6, 2019 in the United States ⋅ ⛅ 18 °C

    walked along the river which was fairly high. Spring run off. Very windy still in the morning. No sites available to stay another night.

    Philadelphus lewesii was in blossom. heavenly scent as you walked down the path.

    there was a fire that went through the gorge last year and it was interesting to see what was burned and what was not... Very mosaic. Lots of greenery coming back where there was burn, but unfortunately i suspect a lot of it was the non native invasives.

    there was an outhouse previously and i am pretty sure that structure was burnt, but a bench maybe 50 feet from it was fine. it is interesting to see how fires in a smaller scale don't necessarily burn everything. The lecture we went to in the winter he said this was the normal pattern, a mosaic. We only have the big devastating fires these days because of our past suppression of fires. had we allowed them to go through on a more regular basis they would remain small. Patch works would not be touched and the burned areas would be reseeded from these unburnt areas. it will be interesting to see how this burn regeneration progresses over the next few years. there were quite a few large trees along the rivers edge that were burnt.
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You might also know this place by the following names:

Wasco County, مقاطعة واسكو, Уаско, ৱাসকো কাউন্টি, Condado de Wasco, Wasco maakond, Wasco konderria, شهرستان واسکو، اورگن, Comté de Wasco, Wasco megye, Ուասկո շրջան, Contea di Wasco, ワスコ郡, Wasco Comitatus, Wasco Kūn, Hrabstwo Wasco, Comitatul Wasco, Округ Воско, Васко, واسکو کاؤنٹی، اوریگون, Quận Wasco, Condado han Wasco, 沃斯科縣

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