View allAll Photos Tagged bedrock

Another shot from the two sunsets I enjoyed at Point Lobos this week.

en.wikipedia.org/wiki/Glacial_striation

 

Photomatix 5 ev -3 0 +3

onOne Enhance , decreased Sat

onOne Effects AG increased details upper part (the trees)

Hasselblad 501cm

80mm cb

ilford provia 400x (expired)

Patterns in the bedrock at Clam Harbour Beach. The image has been mirrored and copied twice to be symmetrical. The detail is best seen full screen.

I don't know what agate looks like before it's polished. Does anyone know if this might be agate? This is from bedrock at La Jolla, CA.

Model: Bree Swing

 

Photographer: Justin Bonaparte​

@justin.bonaparte.creative

www.modelmayhem.com/488132

 

Copyright 2019 by Justin Bonaparte. All Rights Reserved.

The BEST roadside attraction ever, and it's for sale

 

abcnews.go.com/Business/flintstones-bedrock-city-arizona-...

  

All rights reserved.

   

This image may not be copied, reproduced, distributed, republished, downloaded, displayed, posted or transmitted in any form or by any means, including electronic, mechanical, photocopying and recording without my written consent.

 

VWS0806 Copyright © VW Selburn 2021: Once upon a time, this was the bottom of a huge ocean.

thanks to ksuwildkat for the name

The Pre-Cambrian bedrock of the Lower Savage Islands, Nunavut, Canada, is among the oldest rock on the earth's surface dating back up to four billion years.

Multiple flash exposures BOC blended with ambient in PS CC

Certainly, the vast majority of visitors to Peggy's Cove go there to look at this lighthouse, which is probably one of the most photographed things in Nova Scotia. It is actually a pretty minimal structure made mostly of poured concrete, and is actually far from being the best looking lighthouse in Nova Scotia. There are many, many of them. I would say that the number of person visits to this area is likely phenomenal and may be counted occasionally. The cash register at this site is not the lighthouse. It has therefore been difficult to maintain it and renovation and painting has mostly been done by volunteers. There is something magical about the structure and view to those like me that photograph it over and over again in all weather, times and conditions. It is also a bit like a test pattern for those that like to try out their lenses and equipment. While this is not my best shot of it, I rarely go near the site without taking a few shots. This is basically it from the late evening of March 20, 2018. I saw about 15 or more people there, in various places. It is rarely without visitors. For this image, I used a basic DSLR camera. it was a very cold evening, with a clear sky and an icy breeze!

 

©2018 J.Gorman

Getting back to my hike in Joshua Tree from back in October.

 

Pushwalla Canyon

Josha Tree National Park

Mack Super-Liner 685 'Quin Dog' bulk tipping combination seen at Silverwater, NSW.

This 3+5 eight-axle outfit can gross at 59.5 tonnes

Bedrock City, Arizona, 2003. Pentax K1000. Agfa APX100 processed in Xtol.

This observation shows the northeastern wall of the relatively young Bonestell Crater located in the northern lowlands . The northern lowlands occupy most of the northern half of Mars. Bonestell is 42 kilometers (26 mi) in diameter and is 1,250 meters (4,101 feet) deep. HiRISE reveals details in the structure and color of these deep rocks that will help scientists decipher the origin and history of the northern lowlands.

 

Image is less than 5 km (3 mi) across and is 302 km (188 mi) above the surface. For full images including scale bars, visit the source link.

 

www.uahirise.org/PSP_010012_2225

NASA/JPL/UArizona

Part of the bedrock cut by the Potomac at Great Falls National Park in Potomac, Maryland

Native American Village Site. This rock circle served as the foundation of a dome-shaped dwelling built of branches and reeds by the ancestors of the modern Owens Valley Paiute. The site is located at the edge of what was a lake thousands of years ago fed by water from the melting of glaciers in the Sierra. Note the bedrock mortars in the floor of this dwelling area. Fish Slough area. BLM Volcanic Tablelands. Near Bishop, inyo Co., Calif.

These sand dunes in a crater south of Mawrth Vallis are being monitored to measure changes. However, active dunes also clear the dust off of the bedrock between the dunes, which may have diverse colors and compositions, as in the enhanced-color cutout.

 

date: 24 December 2019

altitude: 282 km

 

NASA/JPL/UArizona

uahirise.org/ESP_062863_1980

Crater formation is an intense phenomenon that sends shock waves into the surface that scours and displaces material to form a cavity. Larger craters are observed to possess a central structure formed as a result of bedrock uplifted from the subsurface. High pressures and temperatures experienced during impact cause irreversible changes to target-surface materials that contribute to the formation of rocks called “impactites.” These include impact melts which, as a consequence of melting and re-solidifying, are younger than the target-surface.

 

Identifying and studying well-preserved bedrock exposures associated with central uplifts may provide insights into subsurface composition and the geologic history of the target prior to impact.

Acquisition date

19 August 2009

 

Local Mars time

14:24

 

Latitude (centered)

-21.524°

 

Longitude (East)

44.736°

 

Spacecraft altitude

257.0 km (159.7 miles)

 

Original image scale range

26.7 cm/pixel (with 1 x 1 binning) so objects ~80 cm across are resolved

 

Source : www.uahirise.org/ESP_014361_1585

  

N303WS - Bombardier BD-100-1A10 Challenger 300 - Bedrock Air

at Hamilton International Airport (YHM)

 

c/n 20045 - built in 2005

 

Choose a style at Betty Rubble's Beauty Parlor at Bedrock Village.

 

Sadly no more...

University of Tasmania staircase to the basement of the Geology building.

18 Blythe a Day June 2022

Hall Creek slides down hundreds of feet of bedrock and leaves sheets of ice along the way. This is a shot of the the Hall Creek waterslide above the main waterfall.

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