Beaver Creek (Missouri), Bradleyville (07054080)

StateMissouriLatestGood (434 cfs)
RiverBeaver CreekRatingObservedEstimated
Updated2026-06-19 16:15 (42 minutes ago)Flood - The river is flooding. Obstacles can be treacherous or deadly. The river should be avoided at this stage for casual trips and definitely for the inexperienced. Trips should be attempted only with protective gear and equipment.Flood(none)1610
Discharge434 cfs (median: 125 cfs)High - The river is high and potentially dangerous, especially for the young and / or inexperienced. Normal stream obstacles are sometimes difficult to navigate. Extended distances can be attempted, but canoe travel may not be advisable.High(none)727
Height3.85 feetGood - Conditions are ideal for a canoe or kayak. Boats typically will drag on fewer than one-quarter of riffles, if at all, and portages are unnecessary or rare. Normal float lengths can be attempted without a problem.Good200395
TrendFalling (falling over 24 hours)Low - River is low but can still be floated. Some riffles are okay but most come with significant dragging and might need a portage. Float lengths should be reduced to accommodate low flow, dragging, and portages.Low100154
USGSExternal icon USGS Site (External icon Duck Duck Go Maps)Poor - River is too low to float comfortably. Most or all riffles will drag or must be portaged and some obstacles (such as slick shelf rock) cause undue problems. Avoid the river at this stage for casual paddling trips.Poor5050

Trending Data

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Trips for Beaver Creek (Missouri), Bradleyville (07054080)

DateStartEndDistanceConditionDischargeHeightFishingDetails
Click for details2021-05-08 CR 437 Brownbranch Total trip distance: 4.5 miles4.5 High 679 4.60 Great LMB
RB
RSF
SMB
LMB, RB, RSF, SMB
Barton, Adam
Barton, Scott
Barton, Adam; Barton, Scott
We had the creek to ourselves on a Saturday due to rain falling in the morning. The water was up and flowing a little too fast for adequate fishing conditions, but we still caught tons of rock bass and smallmouth. There were a couple of tricky portages around some trees and rapids, but overall it turned into a beautiful afternoon on the water. I would recommend the area below Brownbranch for better fishing.We had the creek to ourselves on a Saturday due to rain falling in the morning. The water was up and flowing a little too fast for adequate fishing conditions, but we still caught tons of rock bass and smallmouth. There were a couple of tricky portages around some trees and rapids, but overall it turned into a beautiful afternoon on the water. I would recommend the area below Brownbranch for better fishing. USGS Gauge Data:
Bradleyville (07054080)
Discharge: 679
Height: 4.60
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 679<br />Height: 4.60
Source: BartonSource: Barton
Click for details2019-05-25 Jackson Mill CR 437 Total trip distance: 9.2 miles9.2 Good 629 4.43 Great GSF
RB
SMB
GSF, RB, SMB
Bartlett, Joe
Bartlett, Renee
Edmond, Brian
Edmond, Julian
Grindstaff, Brian
Grindstaff, Nathaniel
Hayes, Katie
Larsen, Lisa
Travers, Gina
Tuter, Kristin
Van Someren, Tom
Bartlett, Joe; Bartlett, Renee; Edmond, Brian; Edmond, Julian; Grindstaff, Brian; Grindstaff, Nathaniel; Hayes, Katie; Larsen, Lisa; Travers, Gina; Tuter, Kristin; Van Someren, Tom
The water level on this trip was nearly perfect. There is no access at MO 76 despite the guidebook information. We put in at Jackson Hollow instead. The takeout is now gated and the landowner there is not friendly to paddlers (as we were told by some locals).The water level on this trip was nearly perfect. There is no access at MO 76 despite the guidebook information. We put in at Jackson Hollow instead. The takeout is now gated and the landowner there is not friendly to paddlers (as we were told by some locals). USGS Gauge Data:
Bradleyville (07054080)
Discharge: 629
Height: 4.43
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 629<br />Height: 4.43
Source: EdmondSource: Edmond
Click for details2017-04-01 Brownbranch Bradleyville Total trip distance: 7.9 miles7.9 Good 532 4.01 Good LSF
SMB
LSF, SMB
Arnold, Al
Edmond, Brian
Edmond, Julian
Larsen, Chris
Larsen, Lisa
Turk, Scott
Van Someren, Tom
Arnold, Al; Edmond, Brian; Edmond, Julian; Larsen, Chris; Larsen, Lisa; Turk, Scott; Van Someren, Tom
The water was still high but coming down. It was relatively clear but still murky. At about 2/3 and 3/4, there were at least three tree obstacles that would have blocked us at a lower water level. Fortunately, there is an outfitter at Brownbranch that does some work clearing the river.The water was still high but coming down. It was relatively clear but still murky. At about 2/3 and 3/4, there were at least three tree obstacles that would have blocked us at a lower water level. Fortunately, there is an outfitter at Brownbranch that does some work clearing the river. USGS Gauge Data:
Bradleyville (07054080)
Discharge: 532
Height: 4.01
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 532<br />Height: 4.01
Source: EdmondSource: Edmond
Click for details2020-04-21 Bradleyville Sam Day Road Total trip distance: 4.5 miles4.5 Good 511 3.81 None NoneNone Bartlett, Renee
Jones, Marianne
Van Someren, Andrea
Van Someren, Tom
Bartlett, Renee; Jones, Marianne; Van Someren, Andrea; Van Someren, Tom
This is the float that will forever be known as the "Fuck the Beaver" float. It begins with a huge sinkhole full of mud near the put in requiring a portage of 50 yards or so to the water. (Note: walking thru the sinkhole may result in the loss of your shoes.) Just downriver from the put in, a downed tree makes a tricky obstacle. We ended up with two boats tipped over. Otherwise, this was a quick, pretty stretch of river with only one or two other minor obstacles, the last of which claimed my hat, sunglasses and lawn chair. Fishing is unknown since my new birthday pole was broken in 3 pieces on this float. This section was fairly busy with multiple groups of floaters. However, we did find a nice shaded gravel bar for a wonderful lunch. In addition, there were lots of long, low water level stretches that did not require portage at this level but that might make this section less than ideal at a lower level.This is the float that will forever be known as the USGS Gauge Data:
Bradleyville (07054080)
Discharge: 511
Height: 3.81
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 511<br />Height: 3.81
Source: BartlettSource: Bartlett
Click for details2019-04-21 Brownbranch Bradleyville Total trip distance: 7.9 miles7.9 Good 496 3.96 Fair BLG
GSF
SMB
BLG, GSF, SMB
Bartlett, Joe
Bartlett, Renee
Dudenhoffer, Todd
Van Someren, Tom
Bartlett, Joe; Bartlett, Renee; Dudenhoffer, Todd; Van Someren, Tom
The water level was absolutely STELLAR, moving along great the entire length. No obstructions in the river, either. While the number of fish we caught placed us in the "fair" region we all judged the fishing as "poor". Note too: Beaver Creek Canoe Rental is charging floaters a $10 per boat "Access fee" to put in there.The water level was absolutely STELLAR, moving along great the entire length. No obstructions in the river, either. While the number of fish we caught placed us in the USGS Gauge Data:
Bradleyville (07054080)
Discharge: 496
Height: 3.96
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 496<br />Height: 3.96
Source: Van SomerenSource: Van Someren
Click for details2020-11-28 Brownbranch Bradleyville Total trip distance: 7.9 miles7.9 Good 442 4.02 Good SMBSMB Barton, Adam
Barton, Scott
Barton, Adam; Barton, Scott
No notes for this trip<i>No notes for this trip</i> USGS Gauge Data:
Bradleyville (07054080)
Discharge: 442
Height: 4.02
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 442<br />Height: 4.02
Source: BartonSource: Barton
Click for details2025-06-19 CR 437 Brownbranch Total trip distance: 4.5 miles4.5 Good 393 3.47 Great RB
SMB
RB, SMB
Barton, Adam
Barton, Scott
Barton, Adam; Barton, Scott
No notes for this trip<i>No notes for this trip</i> USGS Gauge Data:
Bradleyville (07054080)
Discharge: 393
Height: 3.47
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 393<br />Height: 3.47
Source: BartonSource: Barton
Click for details2022-09-04 Sam Day Road Hoot Owl Hollow (A) Total trip distance: 11.4 miles7.7 Good 368 3.86 None NoneNone Edmond, Alex
Edmond, Brian
Edmond, Joseph
Edmond, Julian
Edmond, Alex; Edmond, Brian; Edmond, Joseph; Edmond, Julian
This was an overnight trip with just the four of us. Water levels looked good for Beaver Creek and it was close so we decided to give it a try (the Northfork, our original destination, was flooding with the recent rain events). I was surprised to see the water murky, almost muddy. The shuttle to Long Creek Road was more than an hour as it was not direct. We stopped for an extended period at Brushy Creek which was a cool, clear stream that mixed with the muddy waters of Beaver Creek. We ate lunch and made our way to the camp site just above Hoot Owl Hollow. Dinner was burgers, mac and cheese, broccoli / sugar snap peas / mushrooms, and s'mores for dessert. Although the night was clear and fairly warm, we were tired and didn't stay up late. The water level on this day was not that high despite the murkiness of the water. It didn't warrant a "High" rating although it was really running down at Long Creek. I think we managed to get on the river as it was dropping rapidly (see the difference in water level between the two days). Alex and I ran the shuttle, Joseph and Julian stayed behind.This was an overnight trip with just the four of us. Water levels looked good for Beaver Creek and it was close so we decided to give it a try (the Northfork, our original destination, was flooding with the recent rain events). I was surprised to see the water murky, almost muddy. The shuttle to Long Creek Road was more than an hour as it was not direct. We stopped for an extended period at Brushy Creek which was a cool, clear stream that mixed with the muddy waters of Beaver Creek. We ate lunch and made our way to the camp site just above Hoot Owl Hollow. Dinner was burgers, mac and cheese, broccoli / sugar snap peas / mushrooms, and s'mores for dessert. Although the night was clear and fairly warm, we were tired and didn't stay up late. The water level on this day was not that high despite the murkiness of the water. It didn't warrant a USGS Gauge Data:
Bradleyville (07054080)
Discharge: 368
Height: 3.86
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 368<br />Height: 3.86
Source: EdmondSource: Edmond
Click for details2025-06-20 Brownbranch Bradleyville Total trip distance: 7.9 miles7.9 Low 359 3.37 Great LSF
RB
SMB
LSF, RB, SMB
Barton, Adam Barton, ScottBarton, Adam
Barton, Scott On the water at 0815 and rolled into Bradleyville at about 1700. We stayed the night at the campground in Brownbranch after floating above the campground the day before, so there was no additional charge for us to access the creek. This section is noticeably wider and shallower in places after the May 2025 flood than it was last year when we floated in June. In many places along this stretch, there are dead trees and debris caked to the sides of the creek channel and in the riparian zones. Also, I lost count of the portages that are currently required to navigate this section due to the strainers and trees that are blocking the main creek channel. In my humble assessment, most of the quality smallmouth and Ozark bass habitat that was once prevalent in this section has been significantly altered or reduced to gravel fill. While a few quality fishing holes can be found on this stretch, I would prefer to float in the stretch above Brownbranch given the current state of the creek. We managed to grind out a solid day of fishing nonetheless, with dad catching our largest smallmouth of the trip (16.5”) and a plethora of 12” + smallmouth to go with it. The gravel mining operation above Bradleyville continues to alter the channel significantly, but our most productive hole of the day was right above the gravel mine. In that one hole, which spans about a 1/4 mile, we caught 10 smallmouth over 13” along with Dad's PB smallie of the trip (16.5"). Finally, the takeout at Bradleyville continues to degrade with each flood, so I am unsure how much longer it will serve as viable access to the creek. Also, the access road at the campground in Brownbranch is on its last leg as well, so I will be curious to see how the access issues on Beaver Creek are resolved after the next major flood event, which seems to happen annually anymore.On the water at 0815 and rolled into Bradleyville at about 1700. We stayed the night at the campground in Brownbranch after floating above the campground the day before, so there was no additional charge for us to access the creek. This section is noticeably wider and shallower in places after the May 2025 flood than it was last year when we floated in June. In many places along this stretch, there are dead trees and debris caked to the sides of the creek channel and in the riparian zones. Also, I lost count of the portages that are currently required to navigate this section due to the strainers and trees that are blocking the main creek channel. In my humble assessment, most of the quality smallmouth and Ozark bass habitat that was once prevalent in this section has been significantly altered or reduced to gravel fill. While a few quality fishing holes can be found on this stretch, I would prefer to float in the stretch above Brownbranch given the current state of the creek. We managed to grind out a solid day of fishing nonetheless, with dad catching our largest smallmouth of the trip (16.5”) and a plethora of 12” + smallmouth to go with it. The gravel mining operation above Bradleyville continues to alter the channel significantly, but our most productive hole of the day was right above the gravel mine. In that one hole, which spans about a 1/4 mile, we caught 10 smallmouth over 13” along with Dad's PB smallie of the trip (16.5 USGS Gauge Data:
Bradleyville (07054080)
Discharge: 359
Height: 3.37
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 359<br />Height: 3.37
Source: BartonSource: Barton
Click for details2016-07-16 Brownbranch Bradleyville Total trip distance: 7.9 miles7.9 Good 276 3.15 Excellent LSF
GSF
LMB
SMB
RB
LSF, GSF, LMB, SMB, RB
Amburn, Andrea
Amburn, Matt
Dudenhoeffer, Todd
Edmond, Brian
Eth, Joe
Van Someren, Tom
Amburn, Andrea; Amburn, Matt; Dudenhoeffer, Todd; Edmond, Brian; Eth, Joe; Van Someren, Tom
This was an excellent float trip. The water was nearly perfect (a little bit higher would have been nice but it was fantastic just like this). Joe caught more than 50 fish. I caught nearly 30 or more. Even when we didn't catch anything, we could feel fish hitting the lure.This was an excellent float trip. The water was nearly perfect (a little bit higher would have been nice but it was fantastic just like this). Joe caught more than 50 fish. I caught nearly 30 or more. Even when we didn't catch anything, we could feel fish hitting the lure. USGS Gauge Data:
Bradleyville (07054080)
Discharge: 276
Height: 3.15
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 276<br />Height: 3.15
Source: EdmondSource: Edmond
Click for details2019-06-14 Brownbranch Bradleyville Total trip distance: 7.9 miles7.9 Good 258 3.35 Fair GSF
LMB
LSF
SMB
GSF, LMB, LSF, SMB
Bartlett, Renee
Bullard, Loring
Jones, Marianne
Knowlton, Laurie
Siegfried, Beth
Bartlett, Renee; Bullard, Loring; Jones, Marianne; Knowlton, Laurie; Siegfried, Beth
The 2019 Flag Day Float had near perfect weather. Water levels were great. No major obstacles. Absolutely no crowds, didn't see another group all day. Fishing was fair. Was literally "spanked" by a fish.The 2019 Flag Day Float had near perfect weather. Water levels were great. No major obstacles. Absolutely no crowds, didn't see another group all day. Fishing was fair. Was literally USGS Gauge Data:
Bradleyville (07054080)
Discharge: 258
Height: 3.35
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 258<br />Height: 3.35
Source: BartlettSource: Bartlett
Click for details2024-06-19 Brownbranch Bradleyville Total trip distance: 7.9 miles7.9 Good 241 3.65 Excellent GSF
KSB
LMB
LSF
RB
SMB
GSF, KSB, LMB, LSF, RB, SMB
Barton, Adam
Barton, Scott
Barton, Adam; Barton, Scott
On the river at 0800 and off at 1730 with sunny skies and a high of 88 degrees. The cost to put in at Brownbranch is about $10, so budget accordingly. The water level was ideal for fishing and floating. There was a slight stain to the water, which was in part to the creek still coming down from a flood the week prior. A few new trees were down in the water from the recent flood, which made a few technical spots to paddle through. Also, if the water level is any lower than this, there are many riffles that would need to be waded, with slick rocks as a hazard. The final riffle into Bradleyville is a real doozy, so be careful when making that last descent. Most fish were caught using finesse patterns, targeting structure found in the deeper and shaded areas of the creek channel. We caught mostly 10"-12" smallies with a few over 14" and lots of Ozark bass. Overall between Dad and myself, we caught over 100 fish on the day. One of the best fishing floats in Ozarks.On the river at 0800 and off at 1730 with sunny skies and a high of 88 degrees. The cost to put in at Brownbranch is about $10, so budget accordingly. The water level was ideal for fishing and floating. There was a slight stain to the water, which was in part to the creek still coming down from a flood the week prior. A few new trees were down in the water from the recent flood, which made a few technical spots to paddle through. Also, if the water level is any lower than this, there are many riffles that would need to be waded, with slick rocks as a hazard. The final riffle into Bradleyville is a real doozy, so be careful when making that last descent. Most fish were caught using finesse patterns, targeting structure found in the deeper and shaded areas of the creek channel. We caught mostly 10 USGS Gauge Data:
Bradleyville (07054080)
Discharge: 241
Height: 3.65
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 241<br />Height: 3.65
Source: BartonSource: Barton
Click for details2015-04-21 Brownbranch Bradleyville Total trip distance: 7.9 miles7.9 Good 210 2.63 Good SMB
RB
SMB, RB
Coroleuski, Linda
Edmond, Brian
Ligon, Day
McKnight, Don
Coroleuski, Linda; Edmond, Brian; Ligon, Day; McKnight, Don
The river level was nearly perfect although there were a few places where the water level was a bit low. I wouldn't want to float this river any lower than this, except as a good fishing trip.The river level was nearly perfect although there were a few places where the water level was a bit low. I wouldn't want to float this river any lower than this, except as a good fishing trip. USGS Gauge Data:
Bradleyville (07054080)
Discharge: 210
Height: 2.63
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 210<br />Height: 2.63
Source: EdmondSource: Edmond
Click for details2022-09-05 Hoot Owl Hollow (A) Long Creek Road Total trip distance: 11.4 miles3.7 Good 169 3.43 None NoneNone Edmond, Alex
Edmond, Brian
Edmond, Joseph
Edmond, Julian
Edmond, Alex; Edmond, Brian; Edmond, Joseph; Edmond, Julian
We packed up camp and left the gravel bar shortly before 1000 hours after a breakfast of sausage / egg / cheese English muffin sandwiches and chocolate chip muffins. We were running low on water so I thawed the frozen water bottles I had in the cooler. It worked fine since we had eaten most of the food that needed refrigeration and the freezer packs were holding out. The river water had cleared considerably but was still flowing well. Because the river ended up in several braided channels, we did have some difficulty with dragging at riffles in a few places. There were also some dangerous areas, including a riffle that would have been impossible to navigate successfully in even a kayak. We avoided these and nobody tipped over although I scraped past a root wad and ended up with a minor contusion on the top of my head and lost my paddle in the process. Luckily, Alex retrieved it for me. We stopped in a few places to get out and explore and swim. We were at the takeout by 1300 hours. Since everyone had to fit in the car, we packed the gear in an upright canoe and repacked at the put-in to have a good trip home. We arrived at home by 1700 hours after a stop at Andy's on South Campbell.We packed up camp and left the gravel bar shortly before 1000 hours after a breakfast of sausage / egg / cheese English muffin sandwiches and chocolate chip muffins. We were running low on water so I thawed the frozen water bottles I had in the cooler. It worked fine since we had eaten most of the food that needed refrigeration and the freezer packs were holding out. The river water had cleared considerably but was still flowing well. Because the river ended up in several braided channels, we did have some difficulty with dragging at riffles in a few places. There were also some dangerous areas, including a riffle that would have been impossible to navigate successfully in even a kayak. We avoided these and nobody tipped over although I scraped past a root wad and ended up with a minor contusion on the top of my head and lost my paddle in the process. Luckily, Alex retrieved it for me. We stopped in a few places to get out and explore and swim. We were at the takeout by 1300 hours. Since everyone had to fit in the car, we packed the gear in an upright canoe and repacked at the put-in to have a good trip home. We arrived at home by 1700 hours after a stop at Andy's on South Campbell. USGS Gauge Data:
Bradleyville (07054080)
Discharge: 169
Height: 3.43
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 169<br />Height: 3.43
Source: EdmondSource: Edmond
Click for details2018-09-02 Bradleyville Sam Day Road Total trip distance: 7.0 miles7.0 Good 153 2.86 None NoneNone Henderson, Barry
Kendall
Miller
Winslow
Henderson, Barry; Kendall; Miller; Winslow
Good water, tight sunken channel, not a lot of scraping. Some log jams, and tricky spots. Both accesses were pretty tight. Put in at Bradleyville, down Church Street, then left on gravel road behind house, through field, under bridge. Take out was just as tight, but few cars there.Good water, tight sunken channel, not a lot of scraping. Some log jams, and tricky spots. Both accesses were pretty tight. Put in at Bradleyville, down Church Street, then left on gravel road behind house, through field, under bridge. Take out was just as tight, but few cars there. USGS Gauge Data:
Bradleyville (07054080)
Discharge: 153
Height: 2.86
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 153<br />Height: 2.86
Source: HendersonSource: Henderson
Click for details2009-08-19 Brownbranch Bradleyville Total trip distance: 7.9 miles7.9 Low 77 1.81 Excellent SMB
RB
LSF
BLG
SMB, RB, LSF, BLG
Fillmore, Brian
Ligon, Day
Fillmore, Brian; Ligon, Day
No notes for this trip<i>No notes for this trip</i> USGS Gauge Data:
Bradleyville (07054080)
Discharge: 77
Height: 1.81
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 77<br />Height: 1.81
Source: FillmoreSource: Fillmore
Click for details2009-08-22 Brownbranch Bradleyville Total trip distance: 7.9 miles7.9 Poor 74 1.79 None NoneNone Bowe, Michelle
Edmond, Alex
Edmond, Brian
Edmond, Joseph
Bowe, Michelle; Edmond, Alex; Edmond, Brian; Edmond, Joseph
No notes for this trip<i>No notes for this trip</i> USGS Gauge Data:
Bradleyville (07054080)
Discharge: 74
Height: 1.79
<b>USGS Gauge Data:</b></br />Bradleyville (07054080)<br />Discharge: 74<br />Height: 1.79
Source: EdmondSource: Edmond

A total of 17 rows are displayed.

Trip Summary for Beaver Creek (Missouri), Bradleyville (07054080)

Miles120.1
Trips16
People38
Dates17
Years11
Months7
Rows17
Sources6

Condition Descriptions

Fishing Conditions

Fish Species

Notes

Classic Trip List

The classic River Trips application is still available for use. It is updated with the new system using a data retrofit. It is no longer maintained. The original River Trips application is no longer updated (as of 1 Dec 2016) but can be checked for errors or for the condition of the data before it was converted to the new system.

Gauge Data Table

ObservationHeightDischargeMaximum
Discharge
Minimum
Discharge
Mean
Discharge
P05P10P20P25P50
(Median)
P75P80P90P95
2026-06-19 16:15 3.85 434 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 15:15 3.86 438 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 14:15 3.87 441 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 13:15 3.88 444 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 12:15 3.89 447 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 11:15 3.90 450 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 10:15 3.91 453 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 09:15 3.92 456 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 08:15 3.93 460 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 07:15 3.93 460 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 06:15 3.94 463 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 05:15 3.94 463 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 04:15 3.95 466 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 03:15 3.96 469 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 02:15 3.97 472 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 01:15 3.98 476 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-19 00:15 3.99 479 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-18 23:15 4.00 482 8100 (2015) 30 (2001) 407 32 58 86 92 125 222 249 324 3480
2026-06-18 22:15 4.00 482 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 21:15 4.01 485 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 20:15 4.02 489 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 19:15 4.03 492 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 18:15 4.04 495 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 17:15 4.05 499 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 16:15 4.05 499 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 15:15 4.06 502 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 14:15 4.08 509 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 13:15 4.09 512 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 12:15 4.10 515 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 11:15 4.11 519 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 10:15 4.13 526 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 09:15 4.14 529 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 08:15 4.15 533 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 07:15 4.16 536 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 06:15 4.17 540 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 05:15 4.18 543 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 04:15 4.20 550 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 03:15 4.20 550 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 02:15 4.22 557 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 01:15 4.22 557 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-18 00:15 4.23 561 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-17 23:15 4.24 565 1860 (2015) 31 (2001) 213 33 61 92 99 139 211 276 341 1010
2026-06-17 22:15 4.26 572 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 21:15 4.27 575 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 20:15 4.28 579 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 19:15 4.29 583 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 18:15 4.30 586 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 17:15 4.31 590 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 16:15 4.33 598 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 15:15 4.34 601 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 14:15 4.37 613 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 13:15 4.38 616 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 12:15 4.41 628 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 11:15 4.42 632 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 10:15 4.44 640 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 09:15 4.45 643 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 08:15 4.47 651 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 07:15 4.48 655 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 06:15 4.49 659 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 05:15 4.51 667 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 04:15 4.53 675 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 03:15 4.55 683 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 02:15 4.56 687 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 01:15 4.59 700 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-17 00:15 4.60 704 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-16 23:15 4.61 708 728 (2015) 34 (2001) 188 35 62 88 97 142 226 272 450 592
2026-06-16 22:15 4.64 721 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 21:15 4.65 725 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 20:15 4.66 729 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 19:15 4.69 742 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 18:15 4.71 750 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 17:15 4.72 755 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 16:15 4.75 768 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 15:15 4.78 781 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 14:15 4.80 790 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 13:15 4.82 799 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 12:15 4.84 808 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 11:15 4.86 817 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 10:15 4.90 835 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 09:15 4.92 844 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 08:15 4.93 849 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 07:15 4.97 868 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 06:15 5.00 882 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 05:15 5.01 887 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 04:15 5.05 906 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 03:15 5.08 921 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 02:15 5.11 936 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 01:15 5.14 951 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-16 00:15 5.17 966 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-15 23:15 5.21 986 631 (2025) 30 (2000) 183 34 44 80 90 149 221 245 408 524
2026-06-15 22:15 5.25 1010 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 21:15 5.27 1020 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 20:15 5.32 1040 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 19:15 5.35 1060 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 18:15 5.40 1090 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 17:15 5.44 1110 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 16:15 5.48 1130 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 15:15 5.54 1160 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 14:15 5.58 1190 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 13:15 5.63 1220 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 12:15 5.66 1230 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 11:15 5.73 1280 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 10:15 5.78 1310 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 09:15 5.84 1340 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 08:15 5.89 1370 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 07:15 5.95 1410 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 06:15 6.04 1470 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 05:15 6.10 1510 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 04:15 6.18 1570 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 03:15 6.27 1630 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 02:15 6.35 1680 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 01:15 6.44 1750 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-15 00:15 6.57 1850 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-14 23:15 6.70 1960 522 (1995) 33 (2000) 194 36 51 80 92 159 273 297 449 499
2026-06-14 22:15 6.85 2080 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 21:15 7.02 2230 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 20:15 7.21 2410 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 19:15 7.46 2650 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 18:15 7.77 2970 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 17:15 8.28 3550 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 16:15 9.41 5070 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 15:15 11.21 7720 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 14:15 12.10 9270 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 13:15 11.89 8890 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 12:15 11.28 7840 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 11:15 10.59 6740 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 10:15 9.80 5590 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 09:15 8.66 4030 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 08:15 7.50 2690 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 07:15 7.49 2680 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 06:15 6.95 2170 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 05:15 5.44 1110 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 04:15 5.43 1100 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 03:15 5.50 1140 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 02:15 5.61 1200 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 01:15 5.76 1290 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-14 00:15 5.99 1440 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-13 23:15 6.26 1620 640 (1995) 30 (2000) 213 32 45 84 101 147 287 368 454 574
2026-06-13 22:15 6.33 1670 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 21:15 3.37 240 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 20:15 3.34 226 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 19:15 3.34 226 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 18:15 3.33 221 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 17:15 3.34 226 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 16:15 3.31 212 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 15:15 3.30 207 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 14:15 3.29 203 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 13:15 3.30 207 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 12:15 3.29 203 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 11:15 3.29 203 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 10:15 3.31 212 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 09:15 3.31 212 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 08:15 3.31 212 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 07:15 3.31 212 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 06:15 3.32 216 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 05:15 3.32 216 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 04:15 3.33 221 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 03:15 3.34 226 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 02:15 3.34 226 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 01:15 3.34 226 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-13 00:15 3.35 231 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-12 23:15 3.35 231 779 (1995) 26 (2000) 250 30 50 95 110 153 327 444 613 750
2026-06-12 22:15 3.36 236 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 21:15 3.37 240 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 19:15 3.37 240 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 18:15 3.38 245 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 17:15 3.39 250 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 16:15 3.39 250 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 15:15 3.40 255 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 14:15 3.42 264 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 13:15 3.42 264 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 12:15 3.43 268 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 11:15 3.45 278 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 10:15 3.46 282 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 09:15 3.46 282 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 08:15 3.47 287 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 07:15 3.49 296 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 06:15 3.48 292 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 05:15 3.50 301 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 04:15 3.51 305 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 03:15 3.51 305 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 02:15 3.52 309 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 01:15 3.53 313 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-12 00:15 3.54 318 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000
2026-06-11 23:15 3.54 318 1110 (1995) 27 (2000) 262 32 59 85 103 166 343 399 658 1000

A total of 185 rows are displayed for years 1995 through 2025.