World Waterfall Database

Lazy Bear Falls

Skagit County, Washington, United States

Status: Cataloged
This waterfall has been surveyed by members of the World Waterfall Database.

Detailed Info

Lazy Bear Falls is a significant waterfall located near the mouth of Falls Creek, itself a tributary of Bacon Creek, a few miles outside the border of North Cascades National Park. Falls Creek drains from a high basin on the east flank of Diobsud and Electric Buttes, both an extension of the Bacon Peak massif. As it flows from elevations over 6,000 there is significant snow melt feeding into the creek as well as melt from several small glaciers. By the time the creek reaches the valley floor and plunges over the back-to-back 27 and 47 foot punchbowl drops which make up Lazy Bear Falls the volume of the creek is considerable. During the spring and early summer months when snow melt is at its peak, the falls upper tier thunders into its basin and then the creek splits into two segments as it plunges over the lower tier. By late summer and autumn the volume is reduced such that the lower tier of the falls is a single, very narrow punchbowl type plunge. At nearly any time of year the recess behind the falls can be traversed for an even more unique perspective.

Falls Creek has a drainage area of approximately 5-1/2 square miles, extending up to the summits of Diobsud and Electric Buttes, and running part way up the shoulder of Bacon Peak. A small glacier on Electric Butte provides the primary source of flow to the creek in the summer, but numerous permanent snow patches along the ridge also contribute. Because the basin features both high elevation and low elevation terrain, the flow of the creek remains quite consistent throughout the year, though reduced in the late summer and autumn months when there is no longer any active seasonal snow melt.

History and Naming

Lazy Bear Falls is the Proposed name of this waterfall.

Has also been known as:

  • Falls Creek Falls

This waterfall has for the most part been referred to simply as Falls Creek Falls, no colloquial names are known. The name Lazy Bear Falls was suggested by Burlington resident and waterfall hunter Aaron Young after a visit to the falls resulted in encountering a lethargic black bear scrounging in trash left in the parking area / campsite at the end of the road next to the falls. Falls Creek itself is thought to have been named for the presence of this waterfall.

Our Thoughts

Lazy Bear Falls is a bit difficult to access (as far as the drive goes) but it is well worth putting up with the unkempt road in order to visit. The falls are powerful, scenic, make a very good study for photographers and might even offer the chance to see some wildlife (just don't get too close if you do encounter the falls' namesake mascot).

Photo Tips

Spray off the base of the falls can be intense during the melt season and can drift all the way to the trail if it catches the wind right. The falls have a wide open easterly exposure and will see direct, even sunlight in the morning hours. By 3-4pm the sun will transit directly over the falls and can create severe backlighting problems.

Location & Directions

Coordinates:   48.63338, -121.42737
Elevation:   670 feet
USGS Map:   Damnation Peak 7 1/2"

Lazy Bear Falls is found south of the North Cascades National Park boundary in the Bacon Creek valley near Marblemount. Drive the North Cascades Highway (US 20) east from Marblemount for almost 5 miles. Just after crossing Bacon Creek, turn left onto Bacon Creek Road #1060. As of 2018 a rock slide has partially blocked the road around the 4.7 mile mark, and only high clearance vehicles can drive beyond it. It isn't clear whether the forest service will repair the road or not. After the slide the road becomes considerably rougher. Follow the main road at a fork at the 5.5 mile mark, and cross Bacon Creek on a bridge shortly after. Continue another mile to the next fork in the road at a tight switchback, and keep right (again the road heading right is heavily overgrown at this point). Follow the road to its end in another 8/10 mile. This final 8/10 mile of the road is water barred and heavily overgrown, and should be done on foot. At the end of the road, find an obvious trail at the downhill apex of the clearing (not near the creek) which will lead shortly and easily to good views of the falls.

View this location in Google Earth

Other Nearby Waterfalls

Additional Waterfalls which occur within 5 miles of Lazy Bear Falls
No additional waterfalls were found within 5 miles.

By The Numbers

The information presented in this table is meant to help identify and clarify the physical aspects of the waterfall for comparative purposes. While we try to ensure this information is as accurate as possible, sometimes it will prove necessary to either estimate or flat out guess at certain characteristics where either enough information isn't readily available, is not known, or we were not able to confirm a given trait upon surveying. This information may be changed at any given time to ensure accuracy.

Total Height

The Total Height listed for the waterfall represents the difference in elevation from the top of the uppermost drop, to the bottom of the lowermost drop of the waterfall, including all stretches of interstitial stream in between. Stream between two tiers of a waterfall is counted in its overall height regardless of whether or not that section of the stream would be legitimately considered a waterfall on its own right, were it to be isolated. Waterfalls with only one drop will of have the height of only the single drop listed here.

Tallest Drop

The Tallest Drop figure represents the height of the largest single drop within a multi-stepped waterfall. Waterfalls with only one drop will have the total height of the waterfall repeated here.

Num of Drops

The Number of Drops in a waterfall is a tally of the total number of distinct drops which make up the waterfall. Stretches of interstitial stream in between two or more distinct drops of a single waterfall are NOT considered to be distinct drops of the waterfall unless the section of stream in question would otherwise qualify as a waterfall were it to be isolated.

Avg Width

The Average Width of the waterfall represents the breadth of the waterfall from bank to bank under typical flow conditions, or if the waterfall has been Cataloged, under the conditions which it was most thoroughly surveyed. Often this number will be approximated because of a lack of approachability to many waterfalls. We often utilize Google Earth to measure the width (where imagery is of sufficient quality and resolution to allow it.

Maximum Width

Maximum Width represents a hypothetical measurement of roughly how wide a waterfall could get during peak streamflow or flood conditions. For smaller waterfalls, this figure will generally not differ much from the Average Width measurement, but for broader waterfalls - especially those that feature a crest that isn't constricted - this figure can at times be consideraby larger. Like the Average Width measurement, this measurement will take into account the difference in width at the top and bottom of the waterfall as much as possible, but will often be made based on the width of the crest of th falls alone.

Pitch

The Pitch of a waterfall is an estimated - often very roughly - measure of the average slope or steepness of a waterfall. The Pitch figure only takes into account sections of stream which are actively falling. Pools or stretches of level stream in between two or more successive drops of the falls will not factor in this figure. As an example, a waterfall which features two truly free-falling leaps separated by several dozen yards of flat stream will have a Pitch of 90 degrees. Similarly, a waterfall with two drops separated by a pool, one with a true free-falling drop, and one with a Horsetail type fall will average the two, so while the Plunging drop has a Pitch of 90 degrees, if the Horsetail drop has a Pitch of 45 degrees, the total Pitch will be roughly 67 degrees.

Run

The Run of a waterfall is a measurement representing the total linear distance on the ground between the top and bottom of a waterfall. This figure is not often easy to establish with a high degree of precision and as such will often be estimated. Waterfalls with a longer Run will usually either be less steep, often cascading type waterfalls, or will feature multiple steps separated by shorter stretches of a more gradual gradient streambed.

Form

The system of classification of waterfall forms we use is a heavily modified derivative of the classifications outlined by Greg Plumb in his "Waterfall Lover's Guide to the Pacific Northwest" books. While plumb uses eight distnct forms, we wanted further granularity and opted to break down the hierarchy twofold: first based on the overall pitch of the waterfall, and then based on what shape the fall takes as it makes its descent. There are five primary Categories of falls in this system: Plunge, Horsetail, Steep Cascades, Shallow Cascades, and Rapids. Additional deliniation is then applied depending on characteristics such as the breadth of the falls, whether it splits into two or more channels, whether it falls in multiple successive drops, etc. For more information on our waterfall form classifications, see the Help page.

Watershed

The watershed which a waterfall occurs within, if it is specified, will be based on the ultimate distributary watercourse to the ocean. For example, Washington's Palouse Falls occurs along the Palouse River - which is a tributary to the Snake River, which is itself a tributary to the Columbia River, which ultimately enters the Pacific Ocean, so Palouse Falls would then fall within the Columbia River watershed. Streams which empty directly into the ocean, or into a minor basin which then empties to the ocean will often have this field left blank.

Stream

The name of the watercourse which the waterfall occurs along. If the watercourse is not known to have an officially or colloquially recognized name, this field is left blank.

Avg Volume

The volume of water present in the stream at the location of the waterfall. This is often the most difficult figure to pin down because accurately measuring streamflow is not a simple process. We will rely on USGS data as much as possible, and attempt to take into account seasonal fluctuations in stream levels if possible. There is no guarantee that this figure will be accurate, and in cases where there is no USGS data to use, it may be a very, very rough estimate at best.

Source

If known, the primary source of the watercourse which produces the waterfall will be listed here. This is helpful in determining whether a waterfall may flow more consistently during certain periods of the year - streams which originate in Springs, Lakes, or Glaciers will often flow more consistently throughout the year than those fueled by simply Runoff. The source of the stream may also be either unknown or undetermined.

Flow Consistency

A rough estimation of how many months out of the year the stream which produces the waterfall will actually hold water. The vast majority of waterfalls featured on this website will technically be truly perennial waterfalls (those that flow all year long), but some may see their flow dwindle greatly in the late summer months. This figure will not take into account the winter months when the waterfall may freeze, because in such cases the waterfall will very often be inaccessible. Entries which specify a Flow Consistncy of 12 Months should in general have an acceptable flow at any time of year (but may be better during certain periods - see below).

Best Flow

A general estimate of the best period of the year during which time the falls will be considered at optimal conditions, or flowing at their best. There may be variance within the range specified where the flow will be better or worse, but visiting at any time in the range specified (if available) will generally present the waterfall in its best light.

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Key

Cataloged Icon
Cataloged
Waterfalls which are Cataloged we have visited and surveyed in person. Statistical information should be quite accurate (for the most part), and exact measurements will often be available (information is not guaranteed to always be up to date). Detailed information, directions, and photographs will almost always be available.
Confirmed Icon
Confirmed
Confirmed Waterfalls are known to exist, should be relatively accurately mapped and geotagged, and the statistical information available will often be dependable. If height information is presented, it may be estimated but should be accurate. Directions will not likely be available.
Unconfirmed Icon
Unconfirmed
Unconfirmed Waterfalls are often marked on a published map, but we have yet to confirm the exact location and / or whether or not its stature is significant enough to qualify for listing in the database. Statistical information may be estimated and may be inaccurate. No directions.
Unknown Icon
Unknown
Waterfalls marked as Unknown are either suspected to exist based on heresay or a hunch, or we have received unverified information suggesting a waterfall may exist near the location provided but cannot corroborate it in any way. Geodata may not be accurate, the location may not be known at all, and statistical information will be estimated and highly inaccurate.
Inundated Icon
Inundated
Inundated Waterfalls have been submerged beneath lakes or reservoirs, usually a result of impoundment of a river behind a dam, and most often no longer functionally exist (there may be rare exceptions). We maintain records for these features out of historical importance.
Subterranean Icon
Subterranean
Though not common, some waterfalls can be found entirely underground within cave systems. Access to subterranean waterfalls can vary from easy via developed walkways to requiring a high level of extremely technical spelunking skill, including familiarity with ropework and a distinct lack of claustrophobia.
Disqualified Icon
Disqualified
Waterfalls which have been marked as Disqualified do not have the necessary stature or features to qualify as a legitimate waterfall according to our criteria. We will maintain records for entries with this status where the feature is well known and / or may have been historically referred to as a waterfall at some point in time.
Posted Icon
Posted
Posted Waterfalls are known to exist, and we may have a large amount of information associated with them, but are located on private property and are not legally accessible to the general public. Accessing waterfalls with this status should not be attempted without first being explicitly granted permission of the property owner.
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