Type text, add images, blackout confidential details, add comments, highlights and more.
02. Sign it in a few clicks
Draw your signature, type it, upload its image, or use your mobile device as a signature pad.
03. Share your form with others
Send it via email, link, or fax. You can also download it, export it or print it out.
How to edit Topographic features of the taku glacier region online
Ease of Setup
DocHub User Ratings on G2
Ease of Use
DocHub User Ratings on G2
With DocHub, making changes to your paperwork takes just a few simple clicks. Follow these quick steps to edit the PDF Topographic features of the taku glacier region online free of charge:
Sign up and log in to your account. Sign in to the editor using your credentials or click on Create free account to evaluate the tool’s capabilities.
Add the Topographic features of the taku glacier region for editing. Click the New Document option above, then drag and drop the file to the upload area, import it from the cloud, or via a link.
Change your file. Make any changes needed: add text and photos to your Topographic features of the taku glacier region, underline important details, remove parts of content and replace them with new ones, and add icons, checkmarks, and areas for filling out.
Complete redacting the form. Save the updated document on your device, export it to the cloud, print it right from the editor, or share it with all the parties involved.
Our editor is super intuitive and efficient. Try it now!
Fill out topographic features of the taku glacier region online It's free
Taku GlacierTypeTidewater glacierCoordinates583542N 1341047WArea386 square miles (1000 square kilometers)Length58 km (36 miles)6 more rows
What is the width of the Taku Glacier?
The Taku Glacier terminus currently lies about 1.5 km (1 mi) across the Taku River from Taku Point.
Is the Norris Glacier advancing or retreating?
These are the Norris, Taku, Hole-in-the-Wall, Twin, and Tulsequah glaciers. Except for the Taku and its distributary, Hole-in-the-Wall, all the glaciers appear to be retreating.
What are some fun facts about the Taku Glacier?
Taku is extremely thick: In fact, it is one of the thickest known alpine glaciers in the world, measuring 4,860 feet (1,480 meters) from surface to bed. It is also the largest glacier in the Juneau Icefield.
Is the Taku Glacier advancing or retreating?
The Taku is a tidewater glacier that formerly calved, but is now advancing slowly over its outwash delta. The glacier had a dominantly positive mass balance from 1946-1988 and a slightly negative balance since 1988.
Hubbard Glacier is the largest of eight calving glaciers in Alaska that are currently increasing in total mass and advancing.
Why is the Taku Glacier advancing?
Due to the positive mass balance and the fact that it was no longer losing mass to icebergs, Taku Glacier has become insensitive to the warming that has impacted all other glaciers of the icefield. This has driven its advance.
How do you tell if a glacier is advancing or retreating?
The easiest way is to look a the glacier margins. If the ice is in contact with vegetation or rock covered in lichens or moss, it means it is most likely advancing. If you see a band of life-less rock in between the ice and the first plants/lichens/moss, it means it is retreating.
Related links
GEOL 101 Lab 6, Satellite Remote Sensing of Glaciers
Satellite remote sensing offers a new and very powerful way to study glaciers (as well as many other features of Earths surface). This lab will use satellite
by SP Anderson Most glaciers in this region are distributaries of the Stikine Icefield, which extends from north of the Stikine River to south of the Taku River. The Stikine
This site uses cookies to enhance site navigation and personalize your experience.
By using this site you agree to our use of cookies as described in our Privacy Notice.
You can modify your selections by visiting our Cookie and Advertising Notice.... Read more...Read less
