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Larry the Light Fixture likes to wear disguises. When he dresses up like an electric fan, people stand under him during the Summer thinking they will get cooled off. All they get is a boisterous laugh from Larry!
Ballard, Washington 2018
Front view of the Insight H2X Typhoon 2 showing the LED, reflector, and lens. The light is attached with a Daniel Defense offset light mount.
This valley in Nectaris Fossae may have been offset by a strike slip fault. Nectaris Fossae is south of Valles Marineris, right between Thaumasia Planum and Noachis Terra.
NASA/JPL/University of Arizona
It doesn’t take much color in the sky to offset the blues. At least, not for me.
Monte Sano State Park, Huntsville, Alabama.
Nikon D7500 — Nikon 18-300mm F6.3 ED VR
100mm
F8@0.6 seconds
ISO 400
GND filter
Cropped
DSB_5038.JPG
©Don Brown 2026
A little offset study with 1/4, 1/2, 3/4 and 1 plate height differences. Could have been done a bit easier maybe, but it was just a 'digital table-scrap'.
My sempervivums have just started to throw out dozens of offsets, which means I'll soon have loads of new plants to propagate. At the moment though, they are just tiny strands coming off the main rosettes. This is about 2mm across, but you can see the familiar patterns of the sempervivum plant ready to go. Three shots stacked in Zerene Stacker.
Please give credit to my Facebook page if re-posting any image. www.facebook.com/CStarendaPhotography
Mural by Hoxxoh aka @hoxxoh, seen at 1594 Central Avenue in Dubuque, Iowa.
Drone photo by James aka Urbanmuralhunter on that other photo site.
Edit by Teee.
Someone on Reddit asked me to help them with a thatched roof design. This was an idea I had off the top of my head. Round studs going in both directions with the relief in between making space for the lip of the stud. Connects up with eyelet pieces.
Come join me on
Keep Dreaming in Bricks!
Trip to Alaska. Helicopter Tour. Mendenhall Glacier. Juneau. Jul/2016
Mendenhall Glacier is a glacier about 13.6 miles long located in Mendenhall Valley, about 12 miles (19 km) from downtownJuneau in the southeast area of the U.S. state of Alaska.[2] The glacier and surrounding landscape is protected as the 5,815-acre Mendenhall Glacier Recreation Area, a federally designated unit of the Tongass National Forest.[3]
The Juneau Icefield Research Program has monitored the outlet glaciers of the Juneau Icefield since 1942, including Mendenhall Glacier. The glacier has also retreated 1.75 miles (2.82 km) since 1958, when Mendenhall Lake was created, and over 2.5 miles (4.0 km) since 1500. The end of the glacier currently has a negative glacier mass balance and will continue to retreat in the foreseeable future.[4]
Given that average yearly temperatures are currently increasing, and the outlook is for this trend to continue, it is actually possible that the glacier might experience a period of stabilization or slight advance during its retreating march. This is because increasing amounts of warm, moist air will be carried up to the head of the icefield, where colder ambient temperatures will cause it to precipitate as snow. The increased amount of snow will feed the icefield, possibly enough to offset the continually increasing melting experienced at the glacier's terminus. However, this interesting phenomenon will fade away if temperatures continue to climb, since the head of the glacier will no longer have cold enough ambient temperatures to cause snow to precipitate.
Source: Wikipedia
O glaciar (ou Geleira) Mendenhall é um glaciar/geleira com aproximadamente 19 km de comprimento situado no vale de Mendenhall a aproximadamente 19 km de Juneau, Alasca, nos Estados Unidos.
Originalmente conhecido como Sitaantaagu ("o glaciar por detrás da vila") ou Aak'wtaaksit ("o glaciar por detrás do pequeno lago") pelos tlingits, o glaciar (ou geleira) foi baptizado glaciar Auke pelo naturalista John Muir em 1879. Foi rebaptizado em 1892 em honra de Thomas Corwin Mendenhall, superintendente do U.S. Coast and Geodetic Survey entre 1889 e 1894. Estende-se desde o campo de gelo de Juneau, a sua origem, até ao lago Mendenhall.
O Juneau Icefield Research Program estuda os glaciares (ou geleiras) de descarga do campo de gelo de Juneau desde 1946. Entre 1948 e 2005 o ponto terminal do glaciar (geleira), que flui através dos subúrbios de Juneau, recuou 580 metros. Desde 1910, ano da criação do lago Mendenhall, o glaciar recuou 2,8 km e recuou 4,0 km desde 1700. Actualmente apresenta balanço de massa negativo e deverá continuar a recuar no futuro próximo.
O glaciar (or geleira) Mendenhall está incluÃdo na Floresta Nacional de Tongass.
Fonte: Wilipedia